Made in 1916 by British born, German trained, Melbourne stained glass artist William Montgomery, the William Major Olive Memorial Window features Saint Alban.

 

St Alban is venerated as the first recorded British Christian martyr. He is traditionally believed to have been beheaded in the Roman city of Verulamium (modern St Albans) sometime during the 3rd or 4th century, and his cult has been celebrated there since ancient times.

 

The vignette at the base of the memorial window features the following inscription; "In memory of William Major Olive a member chorister of this church killed on active service in France Easter Day 1916". The subject of Saint Alban, England's first martyr saint, may have been chosen to commemorate Lieutenant Olive's service to his country.

 

The window was ordered by the Reverend A. J. Drewett, and was unveiled by the Dean of Melbourne in a dedication ceremony on the 17th of April 1917, almost a year after Lieutenant Olive was killed. The service included the choir singing "Blessed are the Dead", a tribute to a former member of the choir.

 

The window, a large fully-painted single light cost £70.00. It was the third window by Melbourne's leading stained glass artist, William Montgomery, to be installed in the north nave, the others being St. Mark (1913) and St. Stephen (1915).

 

William Major Olive was born on 25 August 1890 to Henry Thomas and Ella Ada Olive at "Surbiton" in Studley Park, Kew. After an excellent studentship at Scotch College where he was a prefect and Senior Cadet, William Olive completed an equally successful bachelor's degree in civil engineering but joined up before the conferring ceremony. He was one of four men whose loss was noted at the Commencement Day ceremony 1917: William Olive; Edward Courtney Thomas MA; Eric Craven Jowett BE; Walter Alan Leckie BE. William Olive joined the 5th Field Company Australian Engineers and proceeded to Alexandria in November 1915, then went on to Marseilles, disembarking on 23 March 1916. Precisely one month later Lieutenant Olive was killed by a shell explosion at Bois Grenier at midday on 23 April. He was buried at Erquinhem Communal Cemetery Extension, France.

 

Built amid workers' cottages and terrace houses of shopkeepers, St. Mark the Evangelist Church of England sits atop an undulating rise in the inner Melbourne suburb of Fitzroy. Nestled behind a thick bank of agapanthus beyond its original cast-iron palisade fence, it would not look out of place in an English country village with its neat buttresses, bluestone masonry and simple, unadorned belfry.

 

St. Mark the Evangelist was the first church to be built outside of the original Melbourne grid as Fitzroy developed into the city's first suburb. A working-class suburb, the majority of its residents were Church of England and from 1849 a Mission Church and school served as a centre for religious, educational and recreational facilities. The school was one of a number of denominational schools established by the Church of England and was partly funded by the Denominational School Board.

 

St. Mark the Evangelist Church of England was designed by architect James Blackburn and built in Early English Gothic style. Richard Grice, Victorian pastoralist and philanthropist, generously contributed almost all the cost of its construction. Work commenced in 1853 to accommodate the growing Church of England congregation of Fitzroy. On July 1st, 1853, the first stone of St. Mark the Evangelist was laid by the first Bishop of Melbourne, The Right Rev. Charles Perry.

Unfortunately, Blackburn did not live to see its completion, dying the following year in 1854 of typhoid. This left St. Mark the Evangelist without an architect to oversee the project, and a series of other notable Melbourne architects helped finish the church including Lloyd Tayler, Leonard Terry and Charles Webb. Even then when St. Mark the Evangelist opened its doors on Sunday, January 21st, 1855, the church was never fully completed with an east tower and spire never realised. The exterior of the church is very plain, constructed of largely unadorned bluestone, with simple buttresses marking structural bays and tall lancet windows. The church's belfry is similarly unadorned, yet features beautiful masonry work. It has a square tower and broach spire.

 

Inside St. Mark the Evangelist Church of England it is peaceful and serves as a quiet sanctuary from the noisy world outside. I visited it on a hot day, and its enveloping coolness was a welcome relief. Walking across the old, highly polished hardwood floors you cannot help but note the gentle scent of the incense used during mass. The church has an ornately carved timber Gothic narthex screen which you walk through to enter the nave. Once there you can see the unusual two storey arcaded gallery designed by Leonard Terry that runs the entire length of the east side of building. Often spoken of as “The Architect’s Folly” Terry's gallery was a divisive point in the Fritzroy congregation. Some thought it added much beauty to the interior with its massive square pillars and seven arches supporting the principals of the roof. Yet it was generally agreed that the gallery was of little effective use, and came with a costly price tag of £3,000.00! To this day, it has never been fully utlised by the church. St. Mark the Evangelist has been fortunate to have a series of organs installed over its history; in 1854 a modest organ of unknown origin: in 1855 an 1853 Foster and Andrews, Hull, organ which was taken from the Athenaeum Theatre in Melbourne's Collins Street: in 1877 an organ built by Melbourne organ maker William Anderson: and finally in 1999 as part of major renovation works a 1938 Harrison and Harrison, Durham, organ taken from St. Luke's Church of England in Cowley, Oxfordshire. The church has gone through many renovations over the ensuing years, yet the original marble font and pews have survived these changes and remain in situ to this day. Blackwood reredos in the chancel, dating from 1939, feature a mosaic of the last supper by stained glass and church outfitters Brooks, Robinson and Company. A similar one can be found at St. Matthew's Church of England in High Street in Prahran. The fine lancet stained glass windows on the west side of St. Mark the Evangelist feature the work of the stained glass firms Brooks, Robinson and Company. and William Montgomery. Many of the windows were installed in the late Nineteenth Century.

 

The St. Mark the Evangelist Parish Hall and verger's cottage were added in 1889 to designs by architects Hyndman and Bates. The hall is arranged as a nave with clerestorey windows and side aisles with buttresses. In 1891 the same architects designed the Choir Vestry and Infants Sunday School on Hodgson Street, to replace the earlier school of 1849 which had been located in the forecourt of the church.

 

The present St. Mark the Evangelist's vicarage, a two-storey brick structure with cast-iron lacework verandahs, was erected in 1910.

 

I am very grateful to the staff of Anglicare who run the busy adjoining St. Mark's Community Centre for allowing me to have free range of the inside of St. Mark the Evangelist for a few hours to photograph it so extensively.

 

James Blackburn (1803 - 1854) was an English civil engineer, surveyor and architect. Born in Upton, West Ham, Essex, James was the third of four sons and one daughter born to his parents. His father was a scalemaker, a trade all his brothers took. At the age of 23, James was employed by the Commissioners of Sewers for Holborn and Finsbury and later became an inspector of sewers. However, his life took a dramatic turn in 1833, when suffering economic hardship, he forged a cheque. He was caught and his penalty was transportation to Van Diemen’s Land (modern day Tasmania). As a convicted prisoner, yet also listed as a civil engineer, James was assigned to the Roads Department under the management of Roderic O’Connor, a wealthy Irishman who was the Inspector of Roads and Bridges at the time. On 3 May 1841 James was pardoned, whereupon he entered private practice with James Thomson, another a former convict. In April 1849, James sailed from Tasmania aboard the "Shamrock" with his wife and ten children to start a new life in Melbourne. Once there he formed a company to sell filtered and purified water to the public, and carried out some minor architectural commissions including St. Mark the Evangelist in Fitzroy. On 24 October he was appointed city surveyor, and between 1850 and 1851 he produced his greatest non-architectural work, the basic design and fundamental conception of the Melbourne water supply from the Yan Yean reservoir via the Plenty River. He was injured in a fall from a horse in January 1852 and died on 3 March 1854 at Brunswick Street, Collingwood, of typhoid. He was buried as a member of St. Mark The Evangelist Church of England. James is best known in Tasmania for his ecclesiastical architectural work including; St Mark's Church of England, Pontville, Tasmania (1839-1841), Holy Trinity Church, Hobart, Tasmania (1841-1848): St. George's Church of England, Battery Point, Tasmania, (1841-1847).

 

Leonard Terry (1825 - 1884) was an architect born at Scarborough, Yorkshire, England. Son of Leonard Terry, a timber merchant, and his wife Margaret, he arrived in Melbourne in 1853 and after six months was employed by architect C. Laing. By the end of 1856 he had his own practice in Collins Street West (Terry and Oakden). After Mr. Laing's death next year Leonard succeeded him as the principal designer of banks in Victoria and of buildings for the Anglican Church, of which he was appointed diocesan architect in 1860. In addition to the many banks and churches that he designed, Leonard is also known for his design of The Melbourne Club on Collins Street (1858 - 1859) "Braemar" in East Melbourne (1865), "Greenwich House" Toorak (1869) and the Campbell residence on the corner of Collins and Spring Streets (1877). Leonard was first married, at 30, on 26 June 1855 to Theodosia Mary Welch (d.1861), by whom he had six children including Marmaduke, who trained as a surveyor and entered his father's firm in 1880. Terry's second marriage, at 41, on 29 December 1866 was to Esther Hardwick Aspinall, who bore him three children and survived him when on 23 June 1884, at the age of 59, he died of a thoracic tumor in his last home, Campbellfield Lodge, Alexandra Parade, in Collingwood.

 

Lloyd Tayler (1830 - 1900) was an architect born on 26 October 1830 in London, youngest son of tailor William Tayler, and his wife Priscilla. Educated at Mill Hill Grammar School, Hendon, and King's College, London, he is said to have been a student at the Sorbonne. In June 1851 he left England to join his brother on the land near Albury, New South Wales. He ended up on the Mount Alexander goldfields before setting up an architectural practice with Lewis Vieusseux, a civil engineer in 1854. By 1856 he had his own architectural practice where he designed premises for the Colonial Bank of Australasia. In the 1860s and 1870s he was lauded for his designs for the National Bank of Australasia, including those in the Melbourne suburbs of Richmond and North Fitzroy, and further afield in country Victoria at Warrnambool and Coleraine. His major design for the bank was the Melbourne head office in 1867. With Edmund Wright in 1874 William won the competition for the design of the South Australian Houses of Parliament, which began construction in 1881. The pair also designed the Bank of Australia in Adelaide in 1875. He also designed the Australian Club in Melbourne's William Street and the Melbourne Exchange in Collins Street in 1878. Lloyd's examples of domestic architecture include the mansion "Kamesburgh", Brighton, commissioned by W. K. Thomson in 1872. Other houses include: "Thyra", Brighton (1883): "Leighswood", Toorak, for C. E. Bright: "Roxcraddock", Caulfield: "Cherry Chase", Brighton: and "Blair Athol", Brighton. In addition to his work on St. Mark the Evangelist in Fitzroy, Lloyd also designed St. Mary's Church of England, Hotham (1860); St Philip's, Collingwood, and the Presbyterian Church, Punt Road, South Yarra (1865); and Trinity Church, Bacchus Marsh (1869). The high point of Lloyd's career was the design for the Melbourne head office of the Commercial Bank of Australia. His last important design was the Metropolitan Fire Brigade Headquarters Station, Eastern Hill in 1892. Lloyd was also a judge in 1900 of the competition plans for the new Flinders Street railway station. Lloyd was married to Sarah Toller, daughter of a Congregational minister. They established a comfortable residence, Pen-y-Bryn, in Brighton, and it was from here that he died of cancer of the liver on the 17th of August 1900 survived by his wife, four daughters and a son.

 

Charles Webb (1821 - 1898) was an architect. Born on 26 November 1821 at Sudbury, Suffolk, England, he was the youngest of nine children of builder William Webb and his wife Elizabeth. He attended Sudbury Academy and was later apprenticed to a London architect. His brother James had migrated to Van Diemen's Land in 1830, married in 1833, gone to Melbourne in 1839 where he set up as a builder in and in 1848 he bought Brighton Park, Brighton. Charles decided to join James and lived with James at Brighton. They went into partnership as architects and surveyors. The commission that established them was in 1850 for St Paul's Church, Swanston Street. It was here that Charles married Emma Bridges, daughter of the chief cashier at the Bank of England. Charles and James built many warehouses, shops and private homes and even a synagogue in the city. After his borther's return to England, Charles designed St. Andrew's Church, Brighton, and receiving an important commission for Melbourne Church of England Grammar School in 1855. In 1857 he added a tower and a slender spire to Scots Church, which James had built in 1841. He designed Wesley College in 1864, the Alfred Hospital and the Royal Arcade in 1869, the South Melbourne Town Hall and the Melbourne Orphan Asylum in 1878 and the Grand Hotel (now the Windsor) in 1884. In 1865 he had designed his own home, "Farleigh", in Park Street, Brighton, where he died on 23 January 1898 of heat exhaustion. Predeceased by Emma in 1893 and survived by five sons and three daughters, he was buried in Brighton cemetery.

 

William Montgomery (1850 - 1927) was an artist who specialised in stained glass painting and design. He was born in England in 1850, and studied at the School of Art in Newcastle-on-Tyne. In his final year William was awarded one of only three National Art Scholarships that year to study at South Kensington School of Art (now the Royal College of Art). He was employed by the leading London stained glass firm, Clayton and Bell, before joining Franz Mayer and Company in Munich, Germany. Over the next seven years he not only designed windows he also trained others in the English style of glass painting. William arrived in Melbourne, Australia, in 1886 during the Boom Period provided by the Gold Rush. Melbourne was at the time one of the wealthiest cities in the world, and was in the throes of a building boom. He quickly set up his studio at 164 Flinders Street in the heart of Melbourne, bringing with him the latest in European style and design and achieving instant success amongst wealthy patrons. He worked equally for Catholic and Protestant denominations, his windows being found in many churches as well as in mansions, houses and other commercial buildings around the city. This extended to the country beyond as his reputation grew. A painter as well as stained glass window designer William was a founding member of the Victorian Art Society in Albert Street, Eastern Hill. William became President of its Council in 1912, a position he held until 1916. He was a trustee of the National Gallery of Victoria. His commissions included; stained glass windows at Christ Church, Hawthorn: St. John's, Heidelberg, St. Ignatius', Richmond: Christ Church, St Kilda: Geelong Grammar School: the Bathurst Cathedral and private houses "Tay Creggan", Hawthorn (now Strathcona Baptist Girls Grammar), and "Earlsbrae Hall", Essendon (now Lowther Hall Anglican Grammar School). The success of William Montgomery made Melbourne the leading centre of stained glass in the Southern Hemisphere. William Montgomery died in 1927.

This informal indoor portrait features three people arranged in a layered composition, with a young blond, blue-eyed child occupying the foreground and two adults seated behind.

 

The child, wearing bright coral-red overalls over a navy-and-white striped shirt, looks directly into the camera with an unusually serious, inquisitive expression. The large blue eyes, slightly parted lips, and attentive gaze create an immediate connection with the viewer.

 

Behind the child, a woman with brown hair, wearing a green top, leans toward the center of the frame with a gentle smile. On the right, a man with glasses, short hair, and a salt-and-pepper beard wears a purple polo shirt. His relaxed posture and understated expression complement the woman's warmer expression.

 

A hand resting against the child's torso provides a visual suggestion of support and intimacy.

 

Discussion

 

Composition and visual relationships

 

The photograph uses a triangular arrangement, with the child positioned prominently in front of the adults. The three faces form a visual structure that conveys togetherness while maintaining each person's individuality.

 

The most compelling feature is the contrast in expressions:

 

- Child: Serious, observant, and intensely engaged with the camera.

 

- Woman: Relaxed, smiling, and looking toward the photographer.

 

- Man: Calm, reserved, and looking directly at the camera.

 

The child becomes the unmistakable focal point, while the adults provide context and a sense of familial connection. Their precise relationships cannot be established from the photograph alone.

 

Photographic technique

The image demonstrates effective use of selective focus.

 

The child's eyes are sharply defined, revealing fine detail in the irises and eyelashes. The adults are progressively softer, although their faces remain recognizable.

 

This creates visual depth without sacrificing the narrative importance of the background figures.

 

The technique corresponds to the use of shallow depth of field in environmental portraiture, where selective sharpness directs attention to the primary subject.

 

The lighting is soft and predominantly natural-looking, apparently entering from the left. Skin tones are warm, and the absence of harsh shadows contributes to the informal atmosphere.

 

Color relationships

The photograph benefits from three distinct clothing colors:

- Coral-red in the foreground

- Green on the left

- Purple on the right

 

The saturated red immediately attracts attention, reinforcing the child's position as the principal subject.

 

The comparatively subdued background prevents environmental details from competing with the people.

 

Artistic assessment

 

The photograph's principal strength is its psychological contrast.

The adults appear comfortable and accustomed to the camera, while the child's expression is more searching and ambiguous.

 

This contrast gives the image greater narrative interest than a conventional group portrait in which everyone smiles.

 

The tight framing contributes to the sense of physical closeness. The principal limitation is the partial cropping of the figures and the slightly distracting dark doorway behind the woman, although neither seriously diminishes the portrait.

 

The image functions as both a family document and an expressive environmental portrait. Its value lies in the individuality of the three expressions rather than in formal posing.

 

  

Features

 

24MP APS-C Exmor™ CMOS sensor

BIONZ X™ engine for superb detail and noise reduction

A-mount interchangeable lens system

Dedicated AF sensor with 79 AF points, 15 cross points

Translucent Mirror Technology for 8fps shooting

  

List Price: unavailable

...

 

epfilms.tv/sony-a68-newest-camera-beat-2016/

This image features the nearly spherical globular star cluster Caldwell 84. It is a composite of observations taken in visible and ultraviolet light by two of Hubble’s science instruments, the Advanced Camera for Surveys and the Wide Field Camera 3. These observations helped astronomers better understand the motions and chemical abundances of stars within the cluster. A relatively bright star, likely closer to us than the cluster is, appears to the upper left of the cluster’s center in Hubble’s image.

 

Astronomers have hypothesized that this globular cluster is a member of the “Gaia Sausage” — the remnants of a dwarf galaxy that is thought to have collided with the Milky Way between 8 million and 10 million years ago. As the dwarf galaxy merged with our galaxy, it was torn apart by the gravitational interaction, leaving behind several globular clusters and millions of stars with unusual orbits. Thanks to these unusual orbits, an elongated, sausage-like shape emerges when the velocities of these stars are plotted on a chart. Because globular clusters like Caldwell 84 generally form in larger galaxies, astronomers believe the dwarf galaxy that collided with the Milky Way was one of the largest of the Milky Way’s early satellite galaxies.

 

Also known as NGC 5286, Caldwell 84 was discovered in 1826 by the Scottish astronomer James Dunlop while he was observing in Australia. Located in the constellation Centaurus and boasting an apparent magnitude of 7.6, this globular cluster can be seen with a small telescope. However, scattered light from the nearby 4.6-magnitude star M Centauri can interfere with observing the cluster. It is most easily spotted during the Southern Hemisphere’s autumn. (Those located near the equator in the Northern Hemisphere can look for it in the late spring.) Caldwell 84 lies roughly 35,000 light-years from Earth and is among the oldest globular clusters in our Milky Way galaxy.

 

Credit: NASA, ESA, A. Sarajedini (Florida Atlantic University), and G. Piotto (Università degli Studi di Padova); Processing: Gladys Kober (NASA/Catholic University of America)

 

For Hubble's Caldwell catalog website and information on how to find these objects in the night sky, visit:

 

www.nasa.gov/content/goddard/hubble-s-caldwell-catalog

 

Venice is a neighborhood of the City of Los Angeles within the Westside region of Los Angeles County, California, United States.

 

Venice was founded by Abbot Kinney in 1905 as a seaside resort town. It was an independent city until 1926, when it was annexed by Los Angeles. Venice is known for its canals, a beach, and Ocean Front Walk, a 2.5-mile (4 km) pedestrian promenade that features performers, fortune-tellers, and vendors.

 

In 1839, a region called La Ballona that included the southern parts of Venice, was granted by the Mexican government to Ygnacio and Augustin Machado and Felipe and Tomas Talamantes, giving them title to Rancho La Ballona. Later this became part of Port Ballona.

 

Venice, originally called "Venice of America", was founded by wealthy developer Abbot Kinney in 1905 as a beach resort town, 14 miles (23 km) west of Los Angeles. He and his partner Francis Ryan had bought 2 miles (3 km) of ocean-front property south of Santa Monica in 1891. They built a resort town on the north end of the property, called Ocean Park, which was soon annexed to Santa Monica. After Ryan died, Kinney and his new partners continued building south of Navy Street. After the partnership dissolved in 1904, Kinney, who had won the marshy land on the south end of the property in a coin flip with his former partners, began to build a seaside resort like the namesake Italian city. 

 

When Venice of America opened on July 4, 1905, Kinney had dug several miles of canals to drain the marshes for his residential area, built a 1,200-foot-long (370 m) pier with an auditorium, ship restaurant, and dance hall, constructed a hot salt-water plunge, and built a block-long arcaded business street with Venetian architecture. Kinney hired artist Felix Peano to design the columns of the buildings.  Included in the capitals are several faces, modeled after Kinney and a woman named Nettie Bouck.

 

Tourists, mostly arriving on the "Red Cars" of the Pacific Electric Railway from Los Angeles and Santa Monica, then rode the Venice Miniature Railway and gondolas to tour the town. The biggest attraction was Venice's 1-mile-long (1.6 km) gently-sloping beach. Cottages and housekeeping tents were available for rent.

 

The population (3,119 residents in 1910) soon exceeded 10,000; the town drew 50,000 to 150,000 tourists on weekends.

 

For the amusement of the public, Kinney hired aviators to do aerial stunts over the beach. One of them, movie aviator and Venice airport owner B. H. DeLay, implemented the first lighted airport in the United States on DeLay Field (previously known as Ince Field). After a marine rescue attempt was thwarted, he organized the first aerial police force in the nation. DeLay performed many of the world's first aerial stunts for motion pictures in Venice.

 

Attractions on the Kinney Pier became more amusement-oriented by 1910, when a Venice Miniature Railway, Aquarium, Virginia Reel, Whip, Racing Derby, and other rides and game booths were added. Since the business district was allotted only three one-block-long streets, and the City Hall was more than a mile away, other competing business districts developed. Unfortunately, this created a fractious political climate. Kinney, however, governed with an iron hand and kept things in check. When he died in November 1920, Venice became harder to govern. With the amusement pier burning six weeks later in December 1920, and Prohibition (which had begun the previous January), the town's tax revenue was severely affected.

 

The Kinney family rebuilt their amusement pier quickly to compete with Ocean Park's Pickering Pleasure Pier and the new Sunset Pier. When it opened it had two roller coasters, a new Racing Derby, a Noah's Ark, a Mill Chutes, and many other rides. By 1925, with the addition of a third coaster, a tall Dragon Slide, Fun House, and Flying Circus aerial ride, it was the finest amusement pier on the West Coast. Several hundred thousand tourists visited on weekends. In 1923, Charles Lick built the Lick Pier at Navy Street in Venice, adjacent to the Ocean Park Pier at Pier Avenue in Ocean Park. Another pier was planned for Venice in 1925 at Leona Street (now Washington Street).

 

By 1925, Venice's politics had become unmanageable because its roads, water and sewage systems badly needed repair and expansion to keep up with its growing population. When it was proposed that Venice consolidate with Los Angeles, the board of trustees voted to hold an election. Consolidation was approved at the election in November 1925, and Venice was merged with Los Angeles in 1926. 

 

Many streets were paved in 1929, following a three-year court battle led by canal residents. Afterward, the Department of Recreation and Parks intended to close three amusement piers, but had to wait until the first of the tidelands leases expired in 1946.

 

In 1929, oil was discovered south of Washington Street on the Venice Peninsula, now known as the Marina Peninsula neighborhood of Los Angeles. Within two years, 450 oil wells covered the area, and drilling waste clogged the remaining waterways. The short-lived boom provided needed income to the community, which otherwise suffered during the Great Depression. Most of the wells had been capped by the 1970s, and the last wells, near the Venice Pavilion, were capped in 1991.

 

After annexation, the city of Los Angeles showed little interest in maintaining the unusual neighborhood. Most of the canals were filled in and paved over, and the former lagoon became a traffic circle. The neighborhood lacked the automobile-centric, homogeneous character that the city sought to cultivate in the post-World War II era, and was perceived as a dated, obsolete remnant of earlier decades' land speculation.

 

Los Angeles had neglected Venice so long that, by the 1950s the neglect had led to the area being labeled the "Slum by the Sea". With the exception of new police and fire stations in 1930, the city spent little on improvements after annexation. The city did not pave Trolleyway (Pacific Avenue) until 1954 when county and state funds became available. Low rents for run-down bungalows attracted predominantly European immigrants (including a substantial number of Holocaust survivors) and young counterculture artists, poets, and writers. The Beat Generation hung out at the Gas House on Ocean Front Walk and at Venice West Cafe on Dudley.

 

The Venice Shoreline Crips and the Latino Venice 13 (V-13) were the two main gangs active in Venice. V13 dates back to the 1950s, while the Shoreline Crips were founded in the early 1970s, making them one of the first Crip sets in Los Angeles.[citation needed] In the early 1990s, V-13 and the Shoreline Crips were involved in a fierce battle over crack cocaine sales territories.

 

By 2002, the numbers of gang members in Venice were reduced due to gentrification and increased police presence. According to a Los Angeles City Beat article, by 2003, many Los Angeles Westside gang members had resettled in the city of Inglewood.

 

Venice Beach is one of the most difficult places in the United States to build new housing due to stringent zoning regulations. Between 2007 and 2022, the number of available housing units actually decreased, despite a massive increase in property values and construction activity over the same period. The neighborhood was developed early in the history of Los Angeles, and as such much of the housing stock predates the current system of zoning regulations by decades. In the areas along Pacific avenue, many early 1900's multifamily buildings still exist, some housing as many as 30 units on a single lot with no parking. Current regulations mandate lower housing densities (most commonly 1 unit per 1,500 square feet of lot area).

 

As per a 2020 count, there were nearly 2,000 homeless people in Venice, up from 175 in 2014. Many of them take up residence in tents and tent cities. An LAPD official said that the increased homeless population has contributed to a spike in crimes in Venice in 2021. In February 2020, the city opened a 154-bed transitional housing shelter at a former Metro bus yard.

 

According to the City of Los Angeles, Venice is bounded on the north by the City of Santa Monica (Marine and Dewey Streets). On the west, it is bounded by the Pacific Ocean and on the east by Walgrove Avenue from the Santa Monica border to Venice Boulevard, Beethoven Street from Venice Boulevard to Zanja Street (including Venice High) and Del Rey Avenue from Zanja Street to Maxella Avenue. On the south, the boundary runs along Lincoln Boulevard to Admiralty Way, then south to Ballona Creek – including the Marina Peninsula community but excluding Marina del Rey. Venice borders the Palms, Mar Vista, and Del Rey neighborhoods, parts of Culver City and Marina del Rey.

 

According to the Venice Neighborhood Council, Venice consists of the eight existing neighborhoods listed in the Venice Specific Plan – Silver Strand, Oxford Triangle, Marina Peninsula, Silver Triangle, North Venice, South Venice, Presidents Row, Venice Canals, Oakwood, North OFW (Ocean Front Walk), NoRo (North of Rose Avenue) and Penmar – plus the additional neighborhood of East of Venice.

 

Venice Beach, which receives millions of visitors a year, has been labeled as "a cultural hub known for its eccentricities" as well as a "global tourist destination". It includes the promenade that runs parallel to the beach, the Venice Beach Boardwalk, Muscle Beach, and the Venice Beach Recreation Center with handball courts, paddle tennis courts, a skate dancing plaza, and numerous beach volleyball courts. It also includes a bike trail and many businesses on Ocean Front Walk.

 

The basketball courts in Venice are renowned across the country for their high level of streetball; numerous professional basketball players developed their games or have been recruited on these courts.

 

Venice Beach will host skateboarding and 3x3 basketball during the 2028 Summer Olympics.

 

Along the southern portion of the beach, at the end of Washington Boulevard, is the Venice Fishing Pier. A 1,310-foot (400 m) concrete structure, it first opened in 1964, was closed in 1983 due to El Niño storm damage, and re-opened in the mid-1990s. On December 21, 2005, the pier again suffered damage when waves from a large northern swell caused part of it to fall into the ocean.[51] The pier remained closed until May 25, 2006, when it was re-opened after an engineering study concluded that it was structurally sound.

 

The Venice Breakwater is an acclaimed local surf spot in Venice. It is located north of the Venice Pier and lifeguard headquarters and south of the Santa Monica Pier. This spot is sheltered on the north by an artificial barrier, the breakwater, consisting of an extending sand bar, piping, and large rocks at its end.

 

In late 2010, the Los Angeles County Board of Supervisors conducted a $1.6 million replacement of 30,000 cubic yards of sand at Venice Beach eroded by rainstorms in recent years. Although Venice Beach is located in the city of Los Angeles, the county is responsible for maintaining the beach under an agreement reached between the two governments in 1975.

 

The Venice Art Walls are murals along the Venice Boardwalk in Venice, Los Angeles, in the U.S. state of California.

 

According to David J. Del Grande of the Arizona Daily Star, "Venice Art Walls offers graffiti writers a place to paint and tag, with their creations curated by local graffiti production company Setting the Pace. The Setting the Pace foundation began managing the Venice Art Walls in 2012, and the group has since organized mural workshops for students and young artists."

 

According to Paste, artists with "prearranged permits can legally tag and create". The site has been mentioned as an example of a deterrent for graffiti elsewhere.

 

A street artist spray painting the wall in 2022

In 2019, Thrillist's Lizbeth Scordo said the "ever-changing" walls between Windward and Market "actually date back to the '60s (though painting them only became technically legal in the last 20 years), and you can watch artists add to the colorful history on weekends".

 

The Venice Beach Recreation Center comprises a number of facilities. The installation has basketball courts (unlighted/outdoor), several children play areas with a gymnastics apparatus, chess tables, handball courts (unlighted), paddle tennis courts (unlighted), and volleyball courts (unlighted). At the south end of the area is the muscle beach outdoor gymnasium. In March 2009, the city opened a sophisticated $2 million skate park, the Venice Beach Skate Park, on the sand towards the north. The Graffiti Walls are on the beach side of the bike path in the same vicinity.

 

The Oakwood Recreation Center, which also acts as a Los Angeles Police Department stop-in center, includes an auditorium, an unlighted baseball diamond, lighted indoor basketball courts, unlighted outdoor basketball courts, a children's play area, a community room, a lighted American football field, an indoor gymnasium without weights, picnic tables, and an unlighted soccer field.

 

Venice Beach is the headquarters of the Los Angeles County Lifeguards of the Los Angeles County Fire Department. It is located at 2300 Ocean Front Walk. It is the nation's largest ocean lifeguard organization with over 200 full-time and 700 part-time or seasonal lifeguards. The headquarters building used to be the City of Los Angeles Lifeguard Headquarters until Los Angeles City and Santa Monica Lifeguards were merged into the County in 1975.

 

The Los Angeles County Lifeguards safeguard 31 miles (50 km) of beach and 70 miles (110 km) of coastline, from San Pedro in the south, to Malibu in the north. Lifeguards also provide paramedic and rescue boat services to Catalina Island, with operations out of Avalon and the Isthmus.

 

Lifeguard Division employs 120 full-time and 600 seasonal lifeguards, operating out of three sectional headquarters, Hermosa, Santa Monica, and Zuma beach. Each of these headquarters staffs a 24-hour EMT-D response unit and are part of the 911 system. In addition to providing for beach safety, Los Angeles County Lifeguards have specialized training for Baywatch rescue boat operations, underwater rescue and recovery, swiftwater rescue, cliff rescue, marine mammal rescue and marine firefighting.

 

California is a state in the Western United States, located along the Pacific Coast. With nearly 39.2 million residents across a total area of approximately 163,696 square miles (423,970 km2), it is the most populous U.S. state and the 3rd largest by area. It is also the most populated subnational entity in North America and the 34th most populous in the world. The Greater Los Angeles area and the San Francisco Bay Area are the nation's second and fifth most populous urban regions respectively, with the former having more than 18.7 million residents and the latter having over 9.6 million. Sacramento is the state's capital, while Los Angeles is the most populous city in the state and the second most populous city in the country. San Francisco is the second most densely populated major city in the country. Los Angeles County is the country's most populous, while San Bernardino County is the largest county by area in the country. California borders Oregon to the north, Nevada and Arizona to the east, the Mexican state of Baja California to the south; and has a coastline along the Pacific Ocean to the west.

 

The economy of the state of California is the largest in the United States, with a $3.4 trillion gross state product (GSP) as of 2022. It is the largest sub-national economy in the world. If California were a sovereign nation, it would rank as the world's fifth-largest economy as of 2022, behind Germany and ahead of India, as well as the 37th most populous. The Greater Los Angeles area and the San Francisco Bay Area are the nation's second- and third-largest urban economies ($1.0 trillion and $0.5 trillion respectively as of 2020). The San Francisco Bay Area Combined Statistical Area had the nation's highest gross domestic product per capita ($106,757) among large primary statistical areas in 2018, and is home to five of the world's ten largest companies by market capitalization and four of the world's ten richest people.

 

Prior to European colonization, California was one of the most culturally and linguistically diverse areas in pre-Columbian North America and contained the highest Native American population density north of what is now Mexico. European exploration in the 16th and 17th centuries led to the colonization of California by the Spanish Empire. In 1804, it was included in Alta California province within the Viceroyalty of New Spain. The area became a part of Mexico in 1821, following its successful war for independence, but was ceded to the United States in 1848 after the Mexican–American War. The California Gold Rush started in 1848 and led to dramatic social and demographic changes, including large-scale immigration into California, a worldwide economic boom, and the California genocide of indigenous people. The western portion of Alta California was then organized and admitted as the 31st state on September 9, 1850, following the Compromise of 1850.

 

Notable contributions to popular culture, for example in entertainment and sports, have their origins in California. The state also has made noteworthy contributions in the fields of communication, information, innovation, environmentalism, economics, and politics. It is the home of Hollywood, the oldest and one of the largest film industries in the world, which has had a profound influence upon global entertainment. It is considered the origin of the hippie counterculture, beach and car culture, and the personal computer, among other innovations. The San Francisco Bay Area and the Greater Los Angeles Area are widely seen as the centers of the global technology and film industries, respectively. California's economy is very diverse: 58% of it is based on finance, government, real estate services, technology, and professional, scientific, and technical business services. Although it accounts for only 1.5% of the state's economy, California's agriculture industry has the highest output of any U.S. state. California's ports and harbors handle about a third of all U.S. imports, most originating in Pacific Rim international trade.

 

The state's extremely diverse geography ranges from the Pacific Coast and metropolitan areas in the west to the Sierra Nevada mountains in the east, and from the redwood and Douglas fir forests in the northwest to the Mojave Desert in the southeast. The Central Valley, a major agricultural area, dominates the state's center. California is well known for its warm Mediterranean climate and monsoon seasonal weather. The large size of the state results in climates that vary from moist temperate rainforest in the north to arid desert in the interior, as well as snowy alpine in the mountains.

 

Settled by successive waves of arrivals during at least the last 13,000 years, California was one of the most culturally and linguistically diverse areas in pre-Columbian North America. Various estimates of the native population have ranged from 100,000 to 300,000. The indigenous peoples of California included more than 70 distinct ethnic groups, inhabiting environments from mountains and deserts to islands and redwood forests. These groups were also diverse in their political organization, with bands, tribes, villages, and on the resource-rich coasts, large chiefdoms, such as the Chumash, Pomo and Salinan. Trade, intermarriage and military alliances fostered social and economic relationships between many groups.

 

The first Europeans to explore the coast of California were the members of a Spanish maritime expedition led by Portuguese captain Juan Rodríguez Cabrillo in 1542. Cabrillo was commissioned by Antonio de Mendoza, the Viceroy of New Spain, to lead an expedition up the Pacific coast in search of trade opportunities; they entered San Diego Bay on September 28, 1542, and reached at least as far north as San Miguel Island. Privateer and explorer Francis Drake explored and claimed an undefined portion of the California coast in 1579, landing north of the future city of San Francisco. Sebastián Vizcaíno explored and mapped the coast of California in 1602 for New Spain, putting ashore in Monterey. Despite the on-the-ground explorations of California in the 16th century, Rodríguez's idea of California as an island persisted. Such depictions appeared on many European maps well into the 18th century.

 

The Portolá expedition of 1769-70 was a pivotal event in the Spanish colonization of California, resulting in the establishment of numerous missions, presidios, and pueblos. The military and civil contingent of the expedition was led by Gaspar de Portolá, who traveled over land from Sonora into California, while the religious component was headed by Junípero Serra, who came by sea from Baja California. In 1769, Portolá and Serra established Mission San Diego de Alcalá and the Presidio of San Diego, the first religious and military settlements founded by the Spanish in California. By the end of the expedition in 1770, they would establish the Presidio of Monterey and Mission San Carlos Borromeo de Carmelo on Monterey Bay.

 

After the Portolà expedition, Spanish missionaries led by Father-President Serra set out to establish 21 Spanish missions of California along El Camino Real ("The Royal Road") and along the Californian coast, 16 sites of which having been chosen during the Portolá expedition. Numerous major cities in California grew out of missions, including San Francisco (Mission San Francisco de Asís), San Diego (Mission San Diego de Alcalá), Ventura (Mission San Buenaventura), or Santa Barbara (Mission Santa Barbara), among others.

 

Juan Bautista de Anza led a similarly important expedition throughout California in 1775–76, which would extend deeper into the interior and north of California. The Anza expedition selected numerous sites for missions, presidios, and pueblos, which subsequently would be established by settlers. Gabriel Moraga, a member of the expedition, would also christen many of California's prominent rivers with their names in 1775–1776, such as the Sacramento River and the San Joaquin River. After the expedition, Gabriel's son, José Joaquín Moraga, would found the pueblo of San Jose in 1777, making it the first civilian-established city in California.

  

The Spanish founded Mission San Juan Capistrano in 1776, the third to be established of the Californian missions.

During this same period, sailors from the Russian Empire explored along the northern coast of California. In 1812, the Russian-American Company established a trading post and small fortification at Fort Ross on the North Coast. Fort Ross was primarily used to supply Russia's Alaskan colonies with food supplies. The settlement did not meet much success, failing to attract settlers or establish long term trade viability, and was abandoned by 1841.

 

During the War of Mexican Independence, Alta California was largely unaffected and uninvolved in the revolution, though many Californios supported independence from Spain, which many believed had neglected California and limited its development. Spain's trade monopoly on California had limited the trade prospects of Californians. Following Mexican independence, Californian ports were freely able to trade with foreign merchants. Governor Pablo Vicente de Solá presided over the transition from Spanish colonial rule to independent.

 

In 1821, the Mexican War of Independence gave the Mexican Empire (which included California) independence from Spain. For the next 25 years, Alta California remained a remote, sparsely populated, northwestern administrative district of the newly independent country of Mexico, which shortly after independence became a republic. The missions, which controlled most of the best land in the state, were secularized by 1834 and became the property of the Mexican government. The governor granted many square leagues of land to others with political influence. These huge ranchos or cattle ranches emerged as the dominant institutions of Mexican California. The ranchos developed under ownership by Californios (Hispanics native of California) who traded cowhides and tallow with Boston merchants. Beef did not become a commodity until the 1849 California Gold Rush.

 

From the 1820s, trappers and settlers from the United States and Canada began to arrive in Northern California. These new arrivals used the Siskiyou Trail, California Trail, Oregon Trail and Old Spanish Trail to cross the rugged mountains and harsh deserts in and surrounding California. The early government of the newly independent Mexico was highly unstable, and in a reflection of this, from 1831 onwards, California also experienced a series of armed disputes, both internal and with the central Mexican government. During this tumultuous political period Juan Bautista Alvarado was able to secure the governorship during 1836–1842. The military action which first brought Alvarado to power had momentarily declared California to be an independent state, and had been aided by Anglo-American residents of California, including Isaac Graham. In 1840, one hundred of those residents who did not have passports were arrested, leading to the Graham Affair, which was resolved in part with the intercession of Royal Navy officials.

 

One of the largest ranchers in California was John Marsh. After failing to obtain justice against squatters on his land from the Mexican courts, he determined that California should become part of the United States. Marsh conducted a letter-writing campaign espousing the California climate, the soil, and other reasons to settle there, as well as the best route to follow, which became known as "Marsh's route". His letters were read, reread, passed around, and printed in newspapers throughout the country, and started the first wagon trains rolling to California. He invited immigrants to stay on his ranch until they could get settled, and assisted in their obtaining passports.

 

After ushering in the period of organized emigration to California, Marsh became involved in a military battle between the much-hated Mexican general, Manuel Micheltorena and the California governor he had replaced, Juan Bautista Alvarado. The armies of each met at the Battle of Providencia near Los Angeles. Marsh had been forced against his will to join Micheltorena's army. Ignoring his superiors, during the battle, he signaled the other side for a parley. There were many settlers from the United States fighting on both sides. He convinced these men that they had no reason to be fighting each other. As a result of Marsh's actions, they abandoned the fight, Micheltorena was defeated, and California-born Pio Pico was returned to the governorship. This paved the way to California's ultimate acquisition by the United States.

 

In 1846, a group of American settlers in and around Sonoma rebelled against Mexican rule during the Bear Flag Revolt. Afterward, rebels raised the Bear Flag (featuring a bear, a star, a red stripe and the words "California Republic") at Sonoma. The Republic's only president was William B. Ide,[65] who played a pivotal role during the Bear Flag Revolt. This revolt by American settlers served as a prelude to the later American military invasion of California and was closely coordinated with nearby American military commanders.

 

The California Republic was short-lived; the same year marked the outbreak of the Mexican–American War (1846–48).

 

Commodore John D. Sloat of the United States Navy sailed into Monterey Bay in 1846 and began the U.S. military invasion of California, with Northern California capitulating in less than a month to the United States forces. In Southern California, Californios continued to resist American forces. Notable military engagements of the conquest include the Battle of San Pasqual and the Battle of Dominguez Rancho in Southern California, as well as the Battle of Olómpali and the Battle of Santa Clara in Northern California. After a series of defensive battles in the south, the Treaty of Cahuenga was signed by the Californios on January 13, 1847, securing a censure and establishing de facto American control in California.

 

Following the Treaty of Guadalupe Hidalgo (February 2, 1848) that ended the war, the westernmost portion of the annexed Mexican territory of Alta California soon became the American state of California, and the remainder of the old territory was then subdivided into the new American Territories of Arizona, Nevada, Colorado and Utah. The even more lightly populated and arid lower region of old Baja California remained as a part of Mexico. In 1846, the total settler population of the western part of the old Alta California had been estimated to be no more than 8,000, plus about 100,000 Native Americans, down from about 300,000 before Hispanic settlement in 1769.

 

In 1848, only one week before the official American annexation of the area, gold was discovered in California, this being an event which was to forever alter both the state's demographics and its finances. Soon afterward, a massive influx of immigration into the area resulted, as prospectors and miners arrived by the thousands. The population burgeoned with United States citizens, Europeans, Chinese and other immigrants during the great California Gold Rush. By the time of California's application for statehood in 1850, the settler population of California had multiplied to 100,000. By 1854, more than 300,000 settlers had come. Between 1847 and 1870, the population of San Francisco increased from 500 to 150,000.

 

The seat of government for California under Spanish and later Mexican rule had been located in Monterey from 1777 until 1845. Pio Pico, the last Mexican governor of Alta California, had briefly moved the capital to Los Angeles in 1845. The United States consulate had also been located in Monterey, under consul Thomas O. Larkin.

 

In 1849, a state Constitutional Convention was first held in Monterey. Among the first tasks of the convention was a decision on a location for the new state capital. The first full legislative sessions were held in San Jose (1850–1851). Subsequent locations included Vallejo (1852–1853), and nearby Benicia (1853–1854); these locations eventually proved to be inadequate as well. The capital has been located in Sacramento since 1854 with only a short break in 1862 when legislative sessions were held in San Francisco due to flooding in Sacramento. Once the state's Constitutional Convention had finalized its state constitution, it applied to the U.S. Congress for admission to statehood. On September 9, 1850, as part of the Compromise of 1850, California became a free state and September 9 a state holiday.

 

During the American Civil War (1861–1865), California sent gold shipments eastward to Washington in support of the Union. However, due to the existence of a large contingent of pro-South sympathizers within the state, the state was not able to muster any full military regiments to send eastwards to officially serve in the Union war effort. Still, several smaller military units within the Union army were unofficially associated with the state of California, such as the "California 100 Company", due to a majority of their members being from California.

 

At the time of California's admission into the Union, travel between California and the rest of the continental United States had been a time-consuming and dangerous feat. Nineteen years later, and seven years after it was greenlighted by President Lincoln, the First transcontinental railroad was completed in 1869. California was then reachable from the eastern States in a week's time.

 

Much of the state was extremely well suited to fruit cultivation and agriculture in general. Vast expanses of wheat, other cereal crops, vegetable crops, cotton, and nut and fruit trees were grown (including oranges in Southern California), and the foundation was laid for the state's prodigious agricultural production in the Central Valley and elsewhere.

 

In the nineteenth century, a large number of migrants from China traveled to the state as part of the Gold Rush or to seek work. Even though the Chinese proved indispensable in building the transcontinental railroad from California to Utah, perceived job competition with the Chinese led to anti-Chinese riots in the state, and eventually the US ended migration from China partially as a response to pressure from California with the 1882 Chinese Exclusion Act.

 

Under earlier Spanish and Mexican rule, California's original native population had precipitously declined, above all, from Eurasian diseases to which the indigenous people of California had not yet developed a natural immunity. Under its new American administration, California's harsh governmental policies towards its own indigenous people did not improve. As in other American states, many of the native inhabitants were soon forcibly removed from their lands by incoming American settlers such as miners, ranchers, and farmers. Although California had entered the American union as a free state, the "loitering or orphaned Indians" were de facto enslaved by their new Anglo-American masters under the 1853 Act for the Government and Protection of Indians. There were also massacres in which hundreds of indigenous people were killed.

 

Between 1850 and 1860, the California state government paid around 1.5 million dollars (some 250,000 of which was reimbursed by the federal government) to hire militias whose purpose was to protect settlers from the indigenous populations. In later decades, the native population was placed in reservations and rancherias, which were often small and isolated and without enough natural resources or funding from the government to sustain the populations living on them. As a result, the rise of California was a calamity for the native inhabitants. Several scholars and Native American activists, including Benjamin Madley and Ed Castillo, have described the actions of the California government as a genocide.

 

In the twentieth century, thousands of Japanese people migrated to the US and California specifically to attempt to purchase and own land in the state. However, the state in 1913 passed the Alien Land Act, excluding Asian immigrants from owning land. During World War II, Japanese Americans in California were interned in concentration camps such as at Tule Lake and Manzanar. In 2020, California officially apologized for this internment.

 

Migration to California accelerated during the early 20th century with the completion of major transcontinental highways like the Lincoln Highway and Route 66. In the period from 1900 to 1965, the population grew from fewer than one million to the greatest in the Union. In 1940, the Census Bureau reported California's population as 6.0% Hispanic, 2.4% Asian, and 89.5% non-Hispanic white.

 

To meet the population's needs, major engineering feats like the California and Los Angeles Aqueducts; the Oroville and Shasta Dams; and the Bay and Golden Gate Bridges were built across the state. The state government also adopted the California Master Plan for Higher Education in 1960 to develop a highly efficient system of public education.

 

Meanwhile, attracted to the mild Mediterranean climate, cheap land, and the state's wide variety of geography, filmmakers established the studio system in Hollywood in the 1920s. California manufactured 8.7 percent of total United States military armaments produced during World War II, ranking third (behind New York and Michigan) among the 48 states. California however easily ranked first in production of military ships during the war (transport, cargo, [merchant ships] such as Liberty ships, Victory ships, and warships) at drydock facilities in San Diego, Los Angeles, and the San Francisco Bay Area. After World War II, California's economy greatly expanded due to strong aerospace and defense industries, whose size decreased following the end of the Cold War. Stanford University and its Dean of Engineering Frederick Terman began encouraging faculty and graduates to stay in California instead of leaving the state, and develop a high-tech region in the area now known as Silicon Valley. As a result of these efforts, California is regarded as a world center of the entertainment and music industries, of technology, engineering, and the aerospace industry, and as the United States center of agricultural production. Just before the Dot Com Bust, California had the fifth-largest economy in the world among nations.

 

In the mid and late twentieth century, a number of race-related incidents occurred in the state. Tensions between police and African Americans, combined with unemployment and poverty in inner cities, led to violent riots, such as the 1965 Watts riots and 1992 Rodney King riots. California was also the hub of the Black Panther Party, a group known for arming African Americans to defend against racial injustice and for organizing free breakfast programs for schoolchildren. Additionally, Mexican, Filipino, and other migrant farm workers rallied in the state around Cesar Chavez for better pay in the 1960s and 1970s.

 

During the 20th century, two great disasters happened in California. The 1906 San Francisco earthquake and 1928 St. Francis Dam flood remain the deadliest in U.S. history.

 

Although air pollution problems have been reduced, health problems associated with pollution have continued. The brown haze known as "smog" has been substantially abated after the passage of federal and state restrictions on automobile exhaust.

 

An energy crisis in 2001 led to rolling blackouts, soaring power rates, and the importation of electricity from neighboring states. Southern California Edison and Pacific Gas and Electric Company came under heavy criticism.

 

Housing prices in urban areas continued to increase; a modest home which in the 1960s cost $25,000 would cost half a million dollars or more in urban areas by 2005. More people commuted longer hours to afford a home in more rural areas while earning larger salaries in the urban areas. Speculators bought houses they never intended to live in, expecting to make a huge profit in a matter of months, then rolling it over by buying more properties. Mortgage companies were compliant, as everyone assumed the prices would keep rising. The bubble burst in 2007–8 as housing prices began to crash and the boom years ended. Hundreds of billions in property values vanished and foreclosures soared as many financial institutions and investors were badly hurt.

 

In the twenty-first century, droughts and frequent wildfires attributed to climate change have occurred in the state. From 2011 to 2017, a persistent drought was the worst in its recorded history. The 2018 wildfire season was the state's deadliest and most destructive, most notably Camp Fire.

 

Although air pollution problems have been reduced, health problems associated with pollution have continued. The brown haze that is known as "smog" has been substantially abated thanks to federal and state restrictions on automobile exhaust.

 

One of the first confirmed COVID-19 cases in the United States that occurred in California was first of which was confirmed on January 26, 2020. Meaning, all of the early confirmed cases were persons who had recently travelled to China in Asia, as testing was restricted to this group. On this January 29, 2020, as disease containment protocols were still being developed, the U.S. Department of State evacuated 195 persons from Wuhan, China aboard a chartered flight to March Air Reserve Base in Riverside County, and in this process, it may have granted and conferred to escalated within the land and the US at cosmic. On February 5, 2020, the U.S. evacuated 345 more citizens from Hubei Province to two military bases in California, Travis Air Force Base in Solano County and Marine Corps Air Station Miramar, San Diego, where they were quarantined for 14 days. A state of emergency was largely declared in this state of the nation on March 4, 2020, and as of February 24, 2021, remains in effect. A mandatory statewide stay-at-home order was issued on March 19, 2020, due to increase, which was ended on January 25, 2021, allowing citizens to return to normal life. On April 6, 2021, the state announced plans to fully reopen the economy by June 15, 2021.

  

One of the main features of the Italian Gardens of the Forest Glade Gardens is a magnificent Italian Rococo three tier fountain with horses at its base. It is surrounded by curcular paving which is decorated with two splendid cast-iron urns and four cherub statues representing the four seasons.

 

The Forest Glade Gardens are well established European inspired landscaped gardens of six hectares that are to be found on the Mount Macedon Road in the hill station town of Mount Macedon.

 

The Forest Glade Gardens are just shy of one hundred years old. The gardens were originally two adjoining properties that comprised orchards and lush grazing paddocks. In 1941 local family the Newtons purchased and extended the property and set about creating one of Mount Macedon's most stunning gardens.

 

In 1971 the Forest Glade Gardens were acquired by Melbourne property developer Mr. Cyril Stokes who together with his partner Trevor Neil Bell, developed the gardens even further. Cyril was a great collector of European antiques, and his love of European antiquity is reflected in the gardens, particularly in the many classical marble and bronze statues dotted about the grounds.

 

Unfortunately the Forest Glade Gardens were partly destroyed by the tragic Ash Wednesday bushfires of 1983. However, after many years of hard labour put in by Cyril and Trevor, The Forest Glade Gardens were reborn from the ashes. The gardens are built on a sloping block and consist of a range of terraces all of which offer wonderful vistas. A garden designed to give pleasure all year round, the Forest Glad Gardens contain several heritage listed trees and are made up of smaller themed gardens including; the Italian Garden, the Japanese Garden, the Daffodil Meadow, the Peony Walk, Hydrangea Hill, the Topiary Gardens, the Bluebell Meadow, the Fern Gully and the Laburnum Arch.

 

In 2011 the property was gifted to a registered charity - The Stokes Collection Limited - with the intention of keeping the Forest Glade Gardens maintained and open to the public.

 

I spent a delightful Saturday with the Famous Flickr Five+ Group in Mount Macedon, where I have never been before. Now I have, I would very much like to go back to such a picturesque place again.

 

The Mount Macedon township is located east of the Mount Macedon summit, which is approximately 60 km north-west of Melbourne.

 

The name of Mount Macedon is apparently derived from Philip II, who ruled Macedon between 359 and 336BC. The mountain was named by Thomas Mitchell, the New South Wales Surveyor General.

 

Settled in the 1850s by gold miners and timber cutters, the railway arrived at the Mount Macedon township in 1861, providing a vital connection to Melbourne, and sealing the town's future as a 'hill station' resort for wealthy Melburnians escaping the summer heat in the 1870s. With the land deforested, large blocks were sold and beautiful and extensive gardens were planted around the newly built homes. The rich soil and good rainfall also made the area suitable for large orchards and plant nurseries who could send fruit and flowers back to Melbourne. Newspaper owner, David Syme, built a house, "Rosenheim" in 1869. It was acquired in 1886 for Victorian Governors to use as a country retreat, making Mount Macedon an attractive destination for the well heeled of Melbourne society. A primary school was built in Mount Macedon in 1874, and as the decades progressed, hotels, guest houses, shops, a Presbyterian Church and Church of England were built. In 1983, Mount Macedon was devastated by the Ash Wednesday Bush Fires. A large portion of the town was raised, and a number of lives were lost. However, like a phoenix from the ashes, Mount Macedon has risen and rebuilt. Today it is still a popular holiday destination, particularly during spring time when the well established gardens flourish with flowers and in autumn when the exotic trees explode in a riot of reds and yellows.

  

Longwood Gardens prominently features poinsettias in their Christmas displays – in fact, according to their blog, they grew 4,400 of the iconic Christmas flower including 14 different cultivars for this year's Christmas display.

 

In honor of the day, I’ll begin the Longwood tour (lol ;-) in the Conservatory’s Rose House, with its ‘living tree’ crafted of red speckled poinsettias (Euphorbia pulcherrima 'LAZZPOSUGI' Superba™ New Glitter’) and Artemisia ‘Silverado.’

 

See more photos of the Rose House and the poinsettia tree below Please do click for a larger look, and don’t worry about commenting ;-)

 

If you want to read more about the Mexican-native poinsettia and its history (and ties to Philadelphia and California), check out Longwood’s blog post: longwoodgardens.org/blog/2020-12-09/poinsettia-evolving-t...

TOKYO, JAPAN - JUNE 08: Matias "Saadhak" Delipetro of LOUD at VALORANT Masters Tokyo Features Day on June 8, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

Looking north to the church - This view features the southwest transept (Resurrection Window), the nave, tower and spire.

 

-———

Links for background information ...

 

Australian Capital Territory Heritage (Decision about Registration of St Andrew’s Church Precinct, Forrest) Notice 2014 - Notifiable Instrument NI2014–43

www.legislation.act.gov.au/ni/2014-43/current/pdf/2014-43...

 

Church Tour

www.standrewscanberra.com/churchlife/church-tour/

 

My thanks to the staff and volunteers for granting access to the church and for their kindness in making me feel so very welcome.

 

-———

 

[ Location - Forrest, Australian Capital Territory, Australia ]

 

Photography notes ...

The photograph was taken using the following hardware configuration ...

(Year of manufacture indicated in braces where known.)

- Hasselblad 501CM Body (Chrome) - S/N 10SH26953 (2002).

- Hasselblad CFV-50c Digital Back for Hasselblad V mount camera.

- Hasselblad Focusing Screen for the CFV-50c digital back, with focussing prism and crop markings.

- Hasselblad 45 Degree Viewfinder PME-45 42297 (2001).

- Hasselblad Carl Zeiss lens - Distagon 50mm f/4 CF FLE T* (1991).

- FotodioX B60 Lens Hood for Select Hasselblad Wide-Angle CF Lenses - MFR # HASSY-HD-6050.

 

- Really Right Stuff (RRS) TFC-14 Series 1 Carbon Fiber Tripod - MFR # 13996.

- Really Right Stuff (RRS) BH-30 Ball Head with Mini Screw-Knob Clamp - MFR # BH-30 PRO.

- Hasselblad HATQCH (3043326) Tripod Quick Coupling.

- Arca-Swiss ARUCP38 Universal Camera Plate 3/8”.

- Nikon AR-3 Shutter Release Cable.

- Artisan & Artist ACAM-302 Silk Cord for Hassleblad Cameras (Black).

 

I acquired a total of 4 photographs (8272 x 6200 pixels, 2 rows and 2 columns, landscape format) with an ISO of 100. I did not record the exposure time nor the aperture.

 

Post-processing ...

Finder - Removed the CF card from the camera digital back and placed it in a Lexar 25-in-1 USB card reader. Then used Finder on my MacBook Air to download the raw image file (3FR extension) from the card.

Lightroom - Imported the images. Applied a standard metadata preset (20161110 Import 001) during the import process.

Lightroom - Used the Map module to add the location details to the EXIF header.

Lightroom - Exported the images as 16-bit TIFF files.

AutoPanoGiga - Opened the TIFF files and compiled the panorama with a Spherical projection (Kolor stitching | 4 pictures | Size: 11504 x 8527 | Lens: Standard | RMS: 3.09 | FOV: 63.92 x 47.38 ~ 14.58 | Projection: Spherical | Color: LDR )

AutoPanoGiga - Rendered the cropped panorama as a JPEG image using the “Maximum” quality option.

Lightroom - Imported the image. Applied a standard metadata preset (20161110 Import 001) during the import process.

Lightroom - Used the Spot Removal tool (Clone and Heal modes) to attenuate a number of sensor dust spots.

Lightroom - Made various lighting and color adjustments to the image.

Lightroom - Straightened the image.

Lightroom - Applied a crop with a 4:3 aspect ratio.

Lightroom - Saved the Develop module settings as a preset.

Lightroom - Output the image as a JPEG image using the “Maximum” quality option (11276 x 8457 pixels).

PhotoSync - Copied the JPEG file to my iPad Mini for any final processing, review, enjoyment, and posting to social media.

 

@MomentsForZen #MomentsForZen #MFZ #Hasselblad #501CM #CFV50c #Lightroom #AutoPanoGiga #WideAngleLens #Church #PresbyterianChurch #StAndrews #StAndrewsChurch #Exterior #Nave #Tower #Spire #Gothic #GothicArchitecture #Panorama

Designed in post-war Art Deco style by stained glass artist Napier Waller, Saint Aidan is the last of three windows installed in the porch of Saint John the Apostle and Evangelist Church of England, to the left of the narthex. Created in rich greens and blue, with a touch of pink, orange and yellow, the Saint Aidan window features the name of the saint in a scroll above his haloed head and an inscription across the bottom which comes from Psalm 18:10 "He did fly upon the wings of the wind". Saint Aidan is depicted upon one knee dressed in the greenish grey robes of a monk with glowing wings appearing behind him in an implicated style. Saint Aidan was an Irish monk and missionary credited for restoring Christianity to Northumbria. He founded a monastic cathedral on the island of Lindisfarne, known as the Lindisfarne Priory. Saint Aidan is often known as Saint Aidan of Lindisfarne.

 

Built on Burke Road on a rise between the busy shopping strips that make up the Camberwell Junction and the grand catholic Our Lady of Victories Basilica, stands the striking Saint John the Apostle and Evangelist Church of England.

 

Almost since the beginning of 1863, Church of England Services have taken place on the site where Saint John the Apostle and Evangelist Church of England stands. In 1863, Camberwell was not the affluent and well established inner city Melbournian suburb that it is today; rather it was a small rural outpost of Melbourne. Therefore the first church, known simply as the Church of England at Camberwell, was little more than a small Victorian Gothic church of brick and stone. However Camberwell, like most of Melbourne, grew as a result of the Gold Rushes and by 1869 an additional chancel had been completed to make allowances for a congregation of around 200 people. As Camberwell's citizenry swelled in number and wealth, so too did their places of worship, and by 1887 Saint John the Apostle and Evangelist Church of England was enlarged and added to. There was no shortage of money, as by this time Camberwell was the home of wealthy industrialists, businessmen and pastoralists as well as a backbone of respectable middle class white collar workers, so the church's windows were filled with elegant and costly stained glass from companies like Mathieson and Gibson, Brooks, Robinson and Company and artists like William Montgomery. Further additions were made on the cusp of the Great War in 1914, and finally a towering spire was added after the War in 1924. In 1930 three stained glass windows by Australian husband and wife artists Christian and Napier Waller featuring the Apotheosis of David were added.

 

By the outbreak of the Second World War, Saint John the Apostle and Evangelist Church of England was an enormous brick an sandstone Victorian Gothic edifice, recognised as a local landmark, and a source of great pride for its wealthy and respectable congregation. Seating over 800 people, it continued to be a place of worship and many happy occasions until the night of the 18th of March 1955, when as a result of an arson attack, the grand building was destroyed by fire. Only the bell tower and spire survived, standing defiantly against the odds, pointing to the heavens.

 

Devastated by the arson attack, the congregation of the church rallied and engaged successful ecclesiastical architect Louis Williams to design a new Saint John the Apostle and Evangelist Church of England. The foundation stone for the new church was laid by the then Archbishop of Melbourne, The Most Reverend J. J. Booth on the Feast of Saint Michael and All Angels on the 29th of September 1956. Rising like a phoenix from the ashes, the new Saint John the Apostle and Evangelist Church of England was completed within two years, finished in November 1957. Sadly, it was discovered several years after its completion, that the belfry and tower of the old Saint John the Apostle and Evangelist Church of England were seriously damaged by the heat of the 1955 fire. Constructionally compromised and therefore a danger not only to the congregation, but any passerby on busy Burke Road should the tower and spire fall into the thoroughfare, the remnants of the old church had to be demolished.

 

The current Saint John the Apostle and Evangelist Church of England building is architecturally very striking. The vast red brick facade rises vertically towards the sky with very little external decoration and is a fine example of Post-War Ecclesiastical architecture. In the wake of the Second World War, faced with austerity and building material shortages as well as the decimation of a workforce skilled enough to architecturally enhance revivalist buildings, architects had to re-think their designs to please their conservative clients who did not want the flat-roofed, glass encrusted boxes that were in vogue in architecturally avant-garde post-war America. Their answer was that between 1940 and 1960, they designed simplified versions of medieval churches. This link back to the more peaceful past, whilst managing the current difficulties of labour and building supplies worked beautifully. Saint John the Apostle and Evangelist Church of England is an ultra-stripped back, simplified version of a Romanesque church. It maintains a traditional rectangular shape, features a traditional pyramidal roof and has aisles that flank the central nave. Its front facade has a post-war Art Deco feel, particularly around the front porch which has elegant brick detailing and a very stylised Art Deco sandstone eagle - an attribute of Saint John the Apostle and Evangelist - above the door. This link to the past is enhanced by the two Old English Gothic style wrought iron lamps that flank the portico's outer doors. A traditional Gothic window with simplified sandstone tracery appears on the facade and is imbedded into a rounded arch which is more shallow than pre-war examples. The church's slender lancet windows have semicircular heads and feature for the most part, latticed plain glass. This allows the church's interior to be flooded with natural light even on a cloudy afternoon, such as the one when I visited Saint John the Apostle and Evangelist Church of England. Some describe the building as elegant, others austere, but the general consensus is that it is one of Louis William's finest architectural works from his very large output of work.

 

Inside the light filled church, the use of stained glass is at a minimum, yet there are three examples which are a throwback to Saint John the Apostle and Evangelist Church of England's glorious stained glass past. When the arsonist attack in 1955 raised the church, so many magnificent, historical and valuable stained glass windows were lost to the conflagration including the three stained glass windows by Australian husband and wife artists Christian and Napier Waller of the Apotheosis of David (shepherd, king and builder) installed in 1930. As part of the church's re-building, Napier Waller (Christian had died by 1955) was commissioned to create three new stained glass windows in memory of those from Saint John the Apostle and Evangelist Church of England who served in the two World Wars. Saint Columba, Saint Alban and Saint Aidan were unveiled in 1961. Installed to the left of the narthex, the three windows are set into their own bay with Saint Columbia on the left, Saint Alban in the middle and Saint Aidan on the right. Designed in post-war Art Deco style, Saint Columbia has an inscription which comes from Psalm 107:23 "They do business in the great waters", Saint Alban has an inscription from Psalm 76:8 "The earth trembled and was still" and Saint Aidan has an inscription from Psalm 18:10 "He did fly upon the wings of the wind".

 

Louis Reginald Williams (1890 – 1980) was born in Hobart, Tasmania and attended school at Queen’s College. His father was a furniture manufacturer, and the family was very religious. Louis’ interest in churches guided him into choosing a career in architecture. He was trained by architect Alexander North, with whom Louis eventually formed a joint partnership when they moved to mainland Australia and set up an architectural firm, Williams and North, in Little Collins Street in Melbourne. Although Louis was commissioned to design commercial buildings and houses, it is for his ecclesiastical buildings that he is best known. He worked mostly in either traditional Gothic or Arts and Crafts styles. Not only was he concerned about the exteriors of his churches, but the interiors as well, and he maintained a group of skilled craftsmen whom he trusted to create his designs for furniture and fittings to harmonise with the buildings he created. He also advised on stained glass, lighting and even mosaic tiling, and no detail was too small for Louis. He designed churches throughout Australia for the Church of England, Presbyterians, Lutherans, Methodists and the Christian Scientists. His career lasted for nearly sixty-five years until he was in his mid eighties.

 

Mervyn Napier Waller (1893 – 1972) was an Australian artist. Born in Penshurst, Victoria, Napier was the son of William Waller, contractor, and his wife Sarah, née Napier. Educated locally until aged 14, he then worked on his father's farm. In 1913 he began studies at the National Gallery schools, Melbourne, and first exhibited water-colours and drawings at the Victorian Artists' Society in 1915. On 31 August of that year he enlisted in the Australian Imperial Force, and on 21 October at the manse of St Andrew's Presbyterian Church, Carlton, married Christian Yandell, a fellow student and artist from Castlemaine. Serving in France from the end of 1916, Waller was seriously wounded in action, and his right arm had to be amputated at the shoulder. Whilst convalescing in France and England Napier learned to write and draw with his left hand. After coming home to Australia he exhibited a series of war sketches in Melbourne, Sydney, Adelaide and Hobart between 1918 and 1919 which helped to establish his reputation as a talented artist. Napier continued to paint in water-colour, taking his subjects from mythology and classical legend, but exhibited a group of linocuts in 1923. In 1927 Napier completed his first major mural for the Menzies Hotel, Melbourne. Next year his mural 'Peace after Victory' was installed in the State Library of Victoria. Visiting England and Europe in 1929 to study stained glass, the Wallers travelled in Italy where Napier was deeply impressed by the mosaics in Ravenna and studied mosaic in Venice. He returned to Melbourne in March 1930 and began to work almost exclusively in stained glass and mosaic. In 1931 he completed a great monumental mosaic for the University of Western Australia; two important commissions in Melbourne followed: the mosaic façade for Newspaper House (completed 1933) and murals for the dining hall in the Myer Emporium (completed 1935). During this time he also worked on a number of stained-glass commissions, some in collaboration with his wife, Christian. Between 1939 and 1945 he worked as an illustrator and undertook no major commissions. In 1946 he finished a three-lancet window commemorating the New Guinea martyrs for St Peter's Church, Eastern Hill. In 1952-58 he designed and completed the mosaics and stained glass for the Hall of Memory at the Australian War Memorial, Canberra. On 25 January 1958 in a civil ceremony in Melbourne Waller had married Lorna Marion Reyburn, a New Zealand-born artist who had long been his assistant in stained glass.

 

Breastfeeding features tutorials !! LIVE feeding my baby and breast milk for ALL SUBSCRIBE : www.youtube.com/channel/UCJY3x4scMGYDyMLDo9rp1Wg breastfeeding. It's a natural thing that shouldnt be considered taboo or judged by others.. These breastfeeding demonstrations contains me feeding my child with my breast, if this offends or you are not allowed to watch please do not watch. I want to encourage moms to breastfeed whenever/wherever this is the natural way to feed a baby. GO MY BREASTFEEDING SOCIAL MEDIA TO FOLLOW REDDIT: ift.tt/2cTI8lR TWITTER:http://ift.tt/2cTI8lR TUMBLR:http://ift.tt/2di9tBk MEDIUM: ift.tt/2cTKd0M GOOGLE+: ift.tt/2di95Tz VK: ift.tt/2cTHQLL FB PAGE: ift.tt/2di8UI0 BLOGGER: ift.tt/2cTIIjg THANKS FOR WATCHING THIS VIDEO TO MORE SEE PLEASE SUBSCRIBE MY CHANNEL YOUTUBE: www.youtube.com/channel/UCJY3x4scMGYDyMLDo9rp1Wg PINTAREST: ift.tt/2dia3PQ LINKEDIN: ift.tt/2cTIxoa INSTAGRAM: ift.tt/2di9THV 500px: ift.tt/2darP6P flickr: ift.tt/2dAsBZ9 TO CONTRAC: ARARSHUVO@ GMAIL.COM SO STAY ENJOY. THANK YOU.

SAO PAULO, BRAZIL - FEBRUARY 19: Zhang "Smoggy" Zhao of EDward Gaming poses during the VALORANT Champions Tour 2023: LOCK//IN features day on February 19, 2023 in Sao Paulo, Brazil. (Photo by Lance Skundrich/Riot Games)

This NASA/ESA Hubble Space Telescope image features the galaxy LEDA 857074, located in the constellation Eridanus. LEDA 857074 is a barred spiral galaxy, with partially broken spiral arms. The image also captured a supernova, named SN 2022ADQZ, shining brightly on the right side of the galaxy’s bar.

 

Several evolutionary paths can lead to a supernova explosion. One is the death of a supermassive star. When a supermassive star runs out of its hydrogen fuel, it begins a stage where it fuses the remaining elements to heavier and heavier ones. These final fusion reactions generate less and less outward force (radiation pressure) to balance the star’s gravitational tug inward. As heavier elements form in the star’s core, the core itself begins to fully collapse under its own gravity, and the star’s outer layers blast away in a supernova explosion. Depending on the star’s original mass, its core may collapse to nothing but neutrons, leaving behind a neutron star, or its gravity may be so great that it collapses to a black hole.

 

Astronomers detected supernova SN 2022ADQZ with an automated survey in late 2022. This discovery led them to look at the supernova’s host galaxy, LEDA 857074, with Hubble in early 2023.

 

Hubble's sharp vision means that it can see supernovae that are billions of light years away and difficult for other telescopes to study. A supernova image from the ground usually blends in with the image of its host galaxy, but Hubble can distinguish a supernova’s light from its host galaxy’s, measuring the supernova directly.

 

Astronomers detect thousands of supernovae annually, but the chance that they spot one in any particular galaxy of the millions that are cataloged is slim. Thanks to this supernova, LEDA 857074 joins the ranks of other celestial objects with its own Hubble image.

 

For more information: science.nasa.gov/missions/hubble/hubble-spotlights-a-supe...

 

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East-German postcard by VEB Progress Filmvertrieb, Berlin, no. 237/70. Photo: publicity still for Columna/Trajan's Column (Mircea Dragan, 1968) .

 

Last Saturday, 6 June 2015, British stage and screen actor and producer Richard Johnson has died, aged 87. He conferred his dark, handsome, saturnine features, assertive jaw, emphatic eyebrows and air of intelligence on scores of classic parts in the theatre, and on a wide range of film and television roles. Johnson was considered for the role of James Bond in the first Bond film, Dr. No. He declined the part down as he did not favour a lengthy contract.

 

Richard Keith Johnson was born at Upminster, Essex, in 1927, the son of Frances Louisa Olive (née Tweed) and Keith Holcombe Johnson. He was educated at Parkfield School and Felsted School before training for the stage at Rada. He claimed to have started acting as a child and then became a professional actor because it made him feel alive, and less aware of his ‘insufficiencies’. During the Second World War he served in the Royal Navy. His career began with a walk-on part in John Gielgud’s 1944 production of Hamlet in Manchester. He moved to the West End as part of a classical repertoire at the Haymarket where he took small parts in Love for Love, The Circle, and The Duchess of Malfi. Before and after his National Service in the Navy from 1945 to 1948 he was in repertory at Perth. After a season of old melodrama in Camden Town, he was in two West End productions, The Madwoman of Chaillot and After My Fashion, as well as open-air Shakespeare in Regent’s Park, before a season with the Bristol Old Vic company in 1953. He spent the next season in broadcasting, but in 1955 he got his first real break in Jean Anouilh’s version of the Joan of Arc story, The Lark, playing Warwick, one of his favourite parts, to Dorothy Tutin’s Joan. A few months later he was cast as Laertes in Peter Brook’s production of Hamlet, starring Paul Scofield (1955). After two more West End productions, playing Jack Absolute in The Rivals and Lord Plynlimmon in Plaintiff in a Pretty Hat, he joined the Shakespeare Memorial Theatre at Stratford-upon-Avon. Among his roles were Orlando in As You Like It, Mark Antony in Julius Caesar, Leonatus in Cymbeline and Ferdinand in The Tempest, which transferred to Drury Lane in 1957. The following season he played Romeo and Sir Andrew Aguecheek as well as the title role in Pericles and Don John in Much Ado About Nothing, visiting Moscow and Leningrad as Romeo and Aguecheek. During the 1960s Johnson became involved with Sir Peter Hall’s production of Cymbeline, leading to Hall inviting him to join him in the Royal Shakespeare Company. There, in 1961, he acted Hans in Jean Giraudoux’s Ondine. He also gave one of his finest performances as Urbaine in John Whiting’s The Devils, a study of 17th-century witchcraft directed by Peter Brook.

 

In 1959, Richard Johnson made his film debut in a major co-star role in the MGM war drama Never So Few (John Sturges, 1959), starring Frank Sinatra and Gina Lollobrigida. Subsequently he was contracted by MGM to appear in 1 film per year over 6 years. There he made his biggest films including Robert Wise’s The Haunting (1963), The Pumpkin Eater (Jack Clayton, 1964) and Khartoum (Basil Dearden, Eliot Elisofon, 1966), starring Laurence Olivier and Charlton Heston. In the early 1960s the director Terence Young had wanted Johnson to play James Bond in preference to Sean Connery. Johnson declined because he was under contract to MGM and did not relish the seven-year commitment. If the stardom for which his career seemed to be heading in the cinema of the early 1960s eluded him, he cut a dashingly romantic figure opposite Kim Novak, whom he married in real life at this time (albeit briefly – they divorced a year later), in the all-star romp, The Amorous Adventures of Moll Flanders (Terence Johnson, 1965). Johnson certainly displayed Bond-like qualities in some of his film roles, notably when he played a modern-day Bulldog Drummond (reimagined as a 007-type hero) in Deadlier Than the Male (Ralph Thomas, 1967) with Elke Sommer and Sylva Koscina and its less satisfactory sequel, Some Girls Do (Ralph Thomas, 1969) with Daliah Lavi. In 1969 he founded a production company called Pageant Entertainments Ltd. Its earliest productions included John Aubrey’s Brief Lives at the Criterion (1969). His feature films included the thriller Danger Route (Seth Holt, 1967), Oedipus the King (Philip Saville, 1968), Le calde notti di Lady Hamilton/Lady Hamilton (Christian Jaque, 1968) starring Michèle Mercier, Julius Caesar (Stuart Burge, 1970), and Hennessy (Don Sharp, 1975) for which he also wrote the original story.

 

Returning to the Royal Shakespeare Company in 1972, Richard Johnson played (both at Stratford and in London) Mark Antony in Julius Caesar, and Antony in Trevor Nunn’s Antony and Cleopatra (opposite Janet Suzman), a performance variously described as “fruity”, “genial” and “declining into a business ruffian”, but also firmly defining the warrior’s handsome gravity. After starring in a West End musical comedy, Thomas and the King, in 1975, in which he played Thomas, he joined the National Theatre Company for a couple of seasons, showing, again under Peter Hall’s direction, a sharp gift for farce in Noël Coward’s Blithe Spirit, and playing Pontius Pilate in The Passion (1977), Pinchwife in Wycherley’s The Country Wife (1977) and Nendor in The Guardsman in 1978. He went on to appear in such films as The Four Feathers (Don Sharp, 1978). He also appeared in several Italian films, including Lucio Fulci's cult classic, Zombi 2/Zombie (1979) which was banned for some years, and L'isola degli uomini pesce/Island of the Fishmen (Sergio Martino, 1979) with Barbara Bach. In 1983 Johnson became founder, chairman, and joint chief executive of a production company, United Artists, with Diana Rigg as director, and the actors Albert Finney and Glenda Jackson. They promoted such films as Turtle Diary (John Irvin, 1985) starring Glenda Jackson and Ben Kingsley, Castaway (Nicolas Roeg, 1986) with Oliver Reed, and The Lonely Passion of Judith Hearne (Jack Clayton, 1987) starring Maggie Smith. He made something of a comeback at Stratford-on-Avon in 1992 as Antony in Antony and Cleopatra, having two years earlier re-established himself on the television screen in two plays, The Camomile Lawn and Anglo-Saxon Attitudes. In later years, he was a charismatic presence in television productions such as Midsomer Murders, Waking the Dead, Silent Witness and Doc Martin. His later films include Lara Croft: Tomb Raider (Simon West, 2001) and The Boy in the Striped Pyjamas (Mark Herman, 2008). His last known film appearance was in Radiator (Tom Browne, 2014). Richard Johnson was married four times; first, in 1957 to the actress Sheila Sweet, by whom he had a son and daughter (the photographer, Sukey Parnell). After their divorce he married, in 1965, Kim Novak, a marriage which lasted a few months. In 1982 he married Mary-Louise Norlund, by whom he had a daughter. He also had a son with the French actress, Françoise Pascal. His fourth wife was Lynne Gurney, whom he married on a beach in Goa in 2004. She survives him with his four children and his stepson, the actor Paris Arrowsmith. Johnson’s family said he died on Saturday in the Royal Marsden hospital in Chelsea, west London, after a short illness.

 

Sources: The Telegraph, The New York Times, The Guardian, Wikipedia and IMDb.

Today's airbrushed style pinup photo features Kelly in this eighth and final in a series of 'color pinups'. This series has looked at the classic styles of artists such as Pearl Frush, Earl Moran, and Peter Driben who often features simplistic pinup artwork with just the pinup girl, possibly a few props, and a very bright colorful background. Light falling on the pinup girl for many of the pinups would come from offscreen somewhere, highlighting parts of the girl. This is a look back at these classic 1950s style of pinup artwork. This is the final one in this series after a month of posting 'color pinups.' Look for them to return again sometime in the future!

 

Did you know you can order many of the pinups you see posted on here? Check out the Dietz Dolls online store where you can find military pinups, classic pinups, the propaganda pinup poster series, and lots more in sizes ranging from 8x10 prints to 24x36 posters! www.dietzdolls.com/catalog

 

Model: Kelly

Photographer: Britt Dietz

Online Pinup Print and Poster Store: www.dietzdolls.com/catalog

© Dietz Dolls Vintage Pinup Photography: www.dietzdolls.com

Facebook Fan Page: www.facebook.com/DietzPinupPhotography

Features daily automobile and motorcycle exhibits and shows. Main hangout for the automotive enthusiast in Orlando. Jeff and I regularly patronize. Food is good and passenger trains are behind this restaurant, interstate faces the restaurant and Amway Sports Center is across the street.

Universal Studios Florida is a theme park located in Orlando, Florida. Opened on June 7, 1990, the park's theme is the entertainment industry, in particular movies and television. Universal Studios Florida inspires its guests to "ride the movies", and it features numerous attractions and live shows. The park is one component of the larger Universal Orlando Resort.

 

In 2013, the park hosted an estimated 7.06 million guests, ranking it the eighth-most visited theme park in the United States, and ranking it sixteenth worldwide.[2]

  

Contents [hide]

1 History 1.1 Park history

1.2 Branding

1.3 Timeline

1.4 Previous attractions

 

2 Park design 2.1 Production Central

2.2 New York

2.3 San Francisco

2.4 London/Diagon Alley

2.5 World Expo

2.6 Woody Woodpecker's Kidzone

2.7 Hollywood

 

3 Character appearances

4 Production facilities

5 Annual events 5.1 Grad Bash and Gradventure

5.2 Halloween Horror Nights

5.3 Macy's Holiday Parade

5.4 Mardi Gras

5.5 Rock the Universe

5.6 Summer Concert Series

 

6 Universal's Express Pass

7 Attendance

8 See also

9 References

10 External links

  

History[edit]

  

This section needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. (August 2010)

     

The original entrance to the theme park.

Over the years, Universal Studios Florida has not limited itself to attractions based on its own vast film library. It has occasionally licensed popular characters from other rival studios, many of whom did not operate theme parks themselves. Some examples include Ghostbusters and Men in Black, (Sony's Columbia Pictures), The Simpsons (20th Century Fox) and Shrek (DreamWorks Animation).

 

Many of the park's past and present attractions were developed with the actual creators of the films they were based on, and feature the original stars as part of the experience. Steven Spielberg helped create E.T. Adventure and was a creative consultant for Back to the Future: The Ride, Twister...Ride it Out, An American Tail Theatre, Jaws, Men in Black: Alien Attack and Transformers: The Ride.

 

In many current rides, the original stars reprised their film roles including: Rip Torn and Will Smith in Men in Black: Alien Attack, Brendan Fraser for Revenge of the Mummy: The Ride, Bill Paxton and Helen Hunt in Twister...Ride it Out, Arnold Schwarzenegger, Edward Furlong and Linda Hamilton reprised their roles for Terminator 2: 3-D Battle Across Time, Mike Myers, Eddie Murphy, Cameron Diaz, and John Lithgow for Shrek 4D, Steve Carell, Miranda Cosgrove, Dana Gaier, and Elsie Fisher reprised their roles from Despicable Me for Despicable Me: Minion Mayhem, and Peter Cullen and Frank Welker reprised their roles as Optimus Prime and Megatron for Transformers: The Ride.

 

In many former rides, the many original stars were also to reprise their film roles such as: Christopher Lloyd and Thomas F. Wilson in Back to the Future: The Ride, Roy Scheider recorded a voice over for the conclusion of Jaws, Alfred Hitchcock and Anthony Perkins appeared in Alfred Hitchcock: The Art of Making Movies, additionally, various Nicktoon voice actors reprised their roles in Jimmy Neutron's Nicktoon Blast.

 

Park history[edit]

 

From its inception in 1982,[3] Universal Studios Florida was designed as a theme park and a working studio. It was also the first time that Universal Studios had constructed an amusement park "from the ground up." However, the proposed project was put on hold until 1986, when a meeting between Steven Spielberg, a co-founder for the park, and Peter N. Alexander prompted for the creation of a Back to the Future simulator ride in addition to the already planned King Kong based ride.[4]

 

A major component of the original park in Hollywood is its studio tour, which featured several special-effects exhibits and encounters built into the tour, such as an attack by the great white shark from the film Jaws. For its Florida park, Universal Studios took the concepts of the Hollywood tour scenes and developed them into larger, stand-alone attractions. As an example, in Hollywood, the studio tour trams travel close to a shoreline and are "attacked" by Jaws before they travel to the next part of the tour. In Florida, guests entered the "Jaws" attraction and would board a boat touring the fictitious Amity Harbor, where they encountered the shark, then exited back into the park at the conclusion of the attraction. Universal Studios Florida originally had a Studio Tour attraction that visited the production facilities, but that tour has since been discontinued.

 

Branding[edit]

 

Previous slogans for Universal Studios Florida were: See the Stars. Ride the Movies. (1990 - 1998); No one makes believe like we do! (1990 - 1998); Ride the Movies (1998 - 2008); Jump into the Action (2008–2012). The current slogan is: Experience the Movies (2012–present).

 

Timeline[edit]

1986: Land clearing takes place on the swamp land purchased by MCA/Universal that would hold the park.

1987: Universal Studios Florida is announced at a press conference on the Hollywood property, with a planned opening date of December 1989.

1988: Universal Studios Florida's opening date is delayed from December, 1989 to May 1, 1990. Shortly following, MCA/Universal releases a video detailing the future park, which stars Christopher Lloyd as the Universal character Doc Brown interacting with the various attractions at the Florida park.[5] Universal Studios allows guests to witness the production of television shows and motion pictures in the Florida park's soundstages in middle 1988, while the rest of the studio/park is still under construction.[6]

1989: MCA/Universal Studios claims that The Walt Disney Company and its CEO, Michael Eisner copied several concepts of the Universal Studios Florida park, and integrated them into Disney's recently opened Disney/MGM Studios park.[7]

1990: On January 31, Universal Studios Florida's opening date is again delayed from May 1, 1990 to June 7, 1990.[8] Universal Studios Florida begins soft openings for the general public in late May.[9] Many of the park's attractions are not yet open at the time, and still under testing. Universal Studios Florida is officially opened with a grand opening style ceremony on June 7.[10] The park opens with five themed areas: The Front Lot (entrance area), Production Central, New York, San Francisco/Amity, Expo Center, Hollywood as well as a Lagoon located in the center of the park. The Front Lot and Production Central areas are referred to as "In Production", the New York section is referred to as "Now Shooting", the San Francisco and Amity sections are referred to as "On Location" and the Expo Center area is referred to as "The World of CineMagic Center". Nickelodeon Studios also opened on this day where there was a grand opening ceremony hosted by Marc Summers. Due to massive technical problems with the original Kongfrontation, Earthquake: The Big One and Jaws rides, Universal begins a temporary voucher service to allow guests to re-visit the studio/park when the attractions are operating.[10] Jaws is temporarily closed by Universal on September 30 due to persistent major technical problems. During the shut-down, Universal sues the original designer of the Jaws ride,[11] Ride & Show Engineering, and hires Totally Fun Company to create a re-designed version of most of the ride.

1991: Universal adds four new attractions to the park: The Blues Brothers Show, StreetBusters, The Screen Test Home Video Adventure and How to Make a Mega Movie Deal.[12] Back to the Future: The Ride officially opens in the World Expo Center area of the park, in a grand opening ceremony.[13] The ride is considered to be a success, and receives positive reception from theme park critics.[14] Fright Nights debuts at the park. In 1992, it is renamed to Halloween Horror Nights.

1993: Jaws is re-opened, with many scenes altered. MCA/Universal announces plans to expand Universal Studios Florida into the Universal City, Florida resort complex, including a second theme park and multiple hotels.[15]

1995: Universal Studios Florida celebrates its 5th anniversary. A Day in the Park with Barney opens in the World Expo area. The Production Studio Tour is closed due to a dwindle in the studios' recent Film/TV production.

1996: Terminator 2: 3-D Battle Across Time opens in the Hollywood area.[16]

1997: Universal announces that Ghostbusters Spooktacular will be replaced by Twister...Ride it Out, with a planned opening date of Spring 1998[17] Universal Studios announces that the sole Studio park will be expanded into the Universal Studios Escape, including the Islands of Adventure park, Universal CityWalk Orlando and multiple hotels. The Islands of Adventure Preview Center opens in the New York area, replacing The Screen Test Home Video Adventure. It is meant to give guests a preview of the up-coming Islands of Adventure park, as well as expansion of the Studio park into the Universal Studios Escape resort.

1998: The expansion begins as the original open parking lot for Universal Studios Florida is demolished and replaced by CityWalk and a parking garage complex.[18] Universal delays the opening of Twister...Ride it Out from March, 1998 to May 4, 1998 out of respect for the 42 deaths caused by a recent El Nino outbreak of tornadoes in the central Florida area. Twister...Ride it Out opens in the New York area, replacing Ghostbusters Spooktacular.[19] A new area of the park, Woody Woodpecker's Kidzone, is officially opened, holding the attractions Curious George Goes to Town, StarToons and the previously opened Fievel's Playland, E.T. Adventure, Animal Actors Stage and A Day in the Park with Barney; CityWalk opens outside of the park.

1999: Woody Woodpecker's Nuthouse Coaster opens in the Woody Woodpecker's Kidzone area. Islands of Adventure opens next door to Universal Studios Florida.[20]

2000: Men in Black: Alien Attack opens in the World Expo area, on the former site of The Swamp Thing Set. Universal Studios Florida's 10th anniversary celebration.

2001: Animal Planet Live opens, replacing Animal Actors Stage.

2002: Universal Studios Escape is renamed Universal Orlando Resort. Kongfrontation closes in a closing ceremony. Halloween Horror Nights is moved to Islands of Adventure. Macy's Holiday Parade debuts at the park.

2003: Jimmy Neutron's Nicktoon Blast opens, replacing The Funtastic World of Hanna-Barbera.[21] Shrek 4-D opens with Donkey's Photo Finish, replacing Alfred Hitchcock: The Art of Making Movies and Stage 54 respectively.[22]

2004: Revenge of the Mummy: The Ride opens, replacing Kongfrontation.[23] Halloween Horror Nights takes place in both Universal Studios Florida and Islands of Adventure.

2005: Universal Express Plus is introduced, replacing Universal Express. Nickelodeon Studios closes after nearly 15 years. Fear Factor Live opens, replacing The Wild Wild Wild West Stunt Show. Universal Studios Florida celebrates its 15th anniversary.

2006: Delancey Street Preview Center opens in the New York area. Universal 360: A Cinesphere Spectacular opens, replacing Dynamite Nights Stunt Spectacular. Animal Planet Live is closed, and replaced by Animal Actors on Location. Halloween Horror Nights returns to Universal Studios Florida for its "Sweet 16".

2007: Back to the Future: The Ride closes on March 30.[24] Blue Man Group Sharp Aquos Theatre opens in CityWalk, replacing Nickelodeon Studios. Earthquake: The Big One closes in the San Francisco area on November 5.

2008: Disaster!: A Major Motion Picture Ride...Starring You! opens, replacing Earthquake: The Big One.[25] Universal announces Hollywood Rip Ride Rockit, with a planned opening of Spring 2009. The Simpsons Ride opens, replacing Back to the Future: The Ride.[26]

2009: The Universal Music Plaza Stage opens, replacing The Boneyard. Hollywood Rip Ride Rockit opens.

2010: The 20th anniversary of Universal Studios Florida in June, as well as Halloween Horror Nights in October.

2011: The 10th anniversary of Macy's Holiday Parade at the park.[27]

2012: Jaws and the surrounding Amity themed area closes, as announced on December 2, 2011.[28] Universal announces the additions of Universal’s Cinematic Spectacular: 100 Years of Movie Memories and Universal's Superstar Parade to the park, with openings on May 8, 2012.[29] Despicable Me: Minion Mayhem, opens replacing Jimmy Neutron's Nicktoon Blast; as announced on March 14, 2011 as "...one of many exciting things planned for the next couple of years".[30] Universal Orlando Resort announced Transformers: The Ride will officially open in the summer of 2013, replacing Soundstages 44 and 54, which were demolished on June 24, 2012.[31] SpongeBob StorePants,a gift shop themed after SpongeBob SquarePants opened in Woody Woodpecker's Kidzone replacing the Universal Cartoon Store

2013: The opening date for Transformers The Ride is announced for June 20, 2013. Details of The Wizarding World of Harry Potter expansion are officially announced. Details for the new Simpsons Land are announced and expected to open in the summer of 2013. Transformers: The Ride officially opens in the Production Central area replacing Soundstage 44. Simpsons Fast Food Boulevard (renamed Springfield U.S.A.) concludes its expansion as it includes one new ride: Kang and Kodos Twirl 'n' Hurl.

2014: The opening date for The Wizarding World of Harry Potter Diagon Alley is announced for July 8, 2014 amid the Diagon Alley preview red carpet premiere on June 18, 2014 with Domhnall Gleeson, Bonnie Wright, Evanna Lynch, Matthew Lewis, James and Oliver Phelps, Tom Felton, Robbie Coltrane, Warwick Davis and Helena Bonham Carter attending the premiere. King's Cross station opens on July 1, 2014 as well as the Hogwarts Express Hogsmeade station at Universal's Islands of Adventure, connecting park visitors to both theme Harry Potter theme parks via a full scale replica of the train that appears in the Harry Potter film series. Diagon Alley officially opens, replacing Jaws and the Amity section of the park.

 

Previous attractions[edit]

 

Main article: List of former Universal Studios Florida attractions

     

The previous icon of the Jaws ride is still a popular photo spot.

Like all theme parks, attractions are sometimes closed due to aging and replaced with more contemporary attractions. Universal has seen this happen several times. Some notable closures include Kongfrontation, Back to the Future: The Ride, The Funtastic World of Hanna-Barbera and Jaws. The closures of Kongfrontation, Back to the Future, and Jaws have been given homages by the park to honor veteran visitors who revered the former rides.

 

Park design[edit]

 

Main article: List of Universal Studios Florida attractions

 

Universal Studios Florida features seven themed areas all situated around a large lagoon. In 2012, this lagoon was the site of Universal’s Cinematic Spectacular: 100 Years of Movie Memories, a thematic display that showcased scenes from various Universal films, featuring lasers, projectors and fountains, and pyrotechnics.

 

The seven surrounding themed areas, clockwise from the entrance, are Production Central, New York, San Francisco, London/Diagon Alley, World Expo, Woody Woodpecker's Kidzone and Hollywood. Each area features a combination of rides, shows, attractions, character appearances, dining outlets and merchandise stores. A new area, based on Harry Potter's Diagon Alley was added to the park in the July of 2014.

 

Production Central[edit]

  

Ride

 

Year opened

 

Manufacturer

  

Despicable Me: Minion Mayhem 2012 Intamin

Shrek 4-D 2003 PDI/DreamWorks

Hollywood Rip, Ride, Rockit 2009 Maurer Söhne

Transformers: The Ride 3D 2013 Oceaneering International

The Universal Music Plaza Stage 2009

  

The area is also home to a variety of dining outlets and merchandise shops. Food and beverage items can be purchased from Beverly Hills Boulangerie or Universal Studios' Classic Monsters Cafe while merchandise can be bought from a variety of themed stores including Universal Studios Store, Studio Sweets, It's a Wrap!, Super Silly Stuff, Shrek's Ye Olde Souvenir Shoppe, and Transformers: Supply Vault.[32][33]

 

Yellowstone National Park (Arapaho: Henihco'oo or Héetíhco'oo) is a national park located primarily in the U.S. state of Wyoming, although it also extends into Montana and Idaho. It was established by the U.S. Congress and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone, widely held to be the first national park in the world, is known for its wildlife and its many geothermal features, especially Old Faithful Geyser, one of the most popular features in the park. It has many types of ecosystems, but the subalpine forest is most abundant. It is part of the South Central Rockies forests ecoregion.

 

Yellowstone National Park spans an area of 3,468.4 square miles (8,983 km2), comprising lakes, canyons, rivers and mountain ranges. Yellowstone Lake is one of the largest high-altitude lakes in North America and is centered over the Yellowstone Caldera, the largest supervolcano on the continent. The caldera is considered an active volcano. It has erupted with tremendous force several times in the last two million years. Half of the world's geothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly-intact ecosystem in the Earth's northern temperate zone.

 

Hundreds of species of mammals, birds, fish and reptiles have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the Continental United States. Grizzly bears, wolves, and free-ranging herds of bison and elk live in the park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.

 

The park is located at the headwaters of the Yellowstone River, from which it takes its historical name. Near the end of the 18th century, French trappers named the river "Roche Jaune", which is probably a translation of the Hidatsa name "Mi tsi a-da-zi" (Rock Yellow River). Later, American trappers rendered the French name in English as "Yellow Stone". Although it is commonly believed that the river was named for the yellow rocks seen in the Grand Canyon of the Yellowstone, the Native American name source is not clear.

 

The first detailed expedition to the Yellowstone area was the Cook–Folsom–Peterson Expedition of 1869, which consisted of three privately funded explorers. The Folsom party followed the Yellowstone River to Yellowstone Lake. The members of the Folsom party kept a journal and based on the information it reported, a party of Montana residents organized the Washburn-Langford-Doane Expedition in 1870. It was headed by the surveyor-general of Montana Henry Washburn, and included Nathaniel P. Langford (who later became known as "National Park" Langford) and a U.S. Army detachment commanded by Lt. Gustavus Doane.

 

The expedition spent about a month exploring the region, collecting specimens and naming sites of interest. A Montana writer and lawyer named Cornelius Hedges, who had been a member of the Washburn expedition, proposed that the region should be set aside and protected as a national park; he wrote a number of detailed articles about his observations for the Helena Herald newspaper between 1870 and 1871. Hedges essentially restated comments made in October 1865 by acting Montana Territorial Governor Thomas Francis Meagher, who had previously commented that the region should be protected. Others made similar suggestions. In an 1871 letter from Jay Cooke to Ferdinand V. Hayden, Cooke wrote that his friend, Congressman William D. Kelley had also suggested "Congress pass a bill reserving the Great Geyser Basin as a public park forever".

 

By 1915, 1,000 automobiles per year were entering the park, resulting in conflicts with horses and horse-drawn transportation. Horse travel on roads was eventually prohibited.

 

The Civilian Conservation Corps (CCC), a New Deal relief agency for young men, played a major role between 1933 and 1942 in developing Yellowstone facilities. CCC projects included reforestation, campground development of many of the park's trails and campgrounds, trail construction, fire hazard reduction, and fire-fighting work. The CCC built the majority of the early visitor centers, campgrounds and the current system of park roads.

 

During World War II, tourist travel fell sharply, staffing was cut, and many facilities fell into disrepair. By the 1950s, visitation increased tremendously in Yellowstone and other national parks. To accommodate the increased visitation, park officials implemented Mission 66, an effort to modernize and expand park service facilities. Planned to be completed by 1966, in honor of the 50th anniversary of the founding of the National Park Service, Mission 66 construction diverged from the traditional log cabin style with design features of a modern style. During the late 1980s, most construction styles in Yellowstone reverted to the more traditional designs. After the enormous forest fires of 1988 damaged much of Grant Village, structures there were rebuilt in the traditional style. The visitor center at Canyon Village, which opened in 2006, incorporates a more traditional design as well.

A large arch made of irregular-shaped natural stone over a road

 

The 1959 Hebgen Lake earthquake just west of Yellowstone at Hebgen Lake damaged roads and some structures in the park. In the northwest section of the park, new geysers were found, and many existing hot springs became turbid. It was the most powerful earthquake to hit the region in recorded history.

 

In 1963, after several years of public controversy regarding the forced reduction of the elk population in Yellowstone, United States Secretary of the Interior Stewart Udall appointed an advisory board to collect scientific data to inform future wildlife management of the national parks. In a paper known as the Leopold Report, the committee observed that culling programs at other national parks had been ineffective, and recommended management of Yellowstone's elk population.

 

The wildfires during the summer of 1988 were the largest in the history of the park. Approximately 793,880 acres (321,272 ha; 1,240 sq mi) or 36% of the parkland was impacted by the fires, leading to a systematic re-evaluation of fire management policies. The fire season of 1988 was considered normal until a combination of drought and heat by mid-July contributed to an extreme fire danger. On "Black Saturday", August 20, 1988, strong winds expanded the fires rapidly, and more than 150,000 acres (61,000 ha; 230 sq mi) burned.

 

The expansive cultural history of the park has been documented by the 1,000 archeological sites that have been discovered. The park has 1,106 historic structures and features, and of these Obsidian Cliff and five buildings have been designated National Historic Landmarks. Yellowstone was designated an International Biosphere Reserve on October 26, 1976, and a UN World Heritage Site on September 8, 1978. The park was placed on the List of World Heritage in Danger from 1995 to 2003 due to the effects of tourism, infection of wildlife, and issues with invasive species. In 2010, Yellowstone National Park was honored with its own quarter under the America the Beautiful Quarters Program.

Heritage and Research Center

 

The Heritage and Research Center is located at Gardiner, Montana, near the north entrance to the park. The center is home to the Yellowstone National Park's museum collection, archives, research library, historian, archeology lab, and herbarium. The Yellowstone National Park Archives maintain collections of historical records of Yellowstone and the National Park Service. The collection includes the administrative records of Yellowstone, as well as resource management records, records from major projects, and donated manuscripts and personal papers. The archives are affiliated with the National Archives and Records Administration.

 

Approximately 96 percent of the land area of Yellowstone National Park is located within the state of Wyoming. Another three percent is within Montana, with the remaining one percent in Idaho. The park is 63 miles (101 km) north to south, and 54 miles (87 km) west to east by air. Yellowstone is 2,219,789 acres (898,317 ha; 3,468.420 sq mi) in area, larger than the states of Rhode Island or Delaware. Rivers and lakes cover five percent of the land area, with the largest water body being Yellowstone Lake at 87,040 acres (35,220 ha; 136.00 sq mi). Yellowstone Lake is up to 400 feet (120 m) deep and has 110 miles (180 km) of shoreline. At an elevation of 7,733 feet (2,357 m) above sea level, Yellowstone Lake is the largest high altitude lake in North America. Forests comprise 80 percent of the land area of the park; most of the rest is grassland.

 

The Continental Divide of North America runs diagonally through the southwestern part of the park. The divide is a topographic feature that separates Pacific Ocean and Atlantic Ocean water drainages. About one third of the park lies on the west side of the divide. The origins of the Yellowstone and Snake Rivers are near each other but on opposite sides of the divide. As a result, the waters of the Snake River flow to the Pacific Ocean, while those of the Yellowstone find their way to the Atlantic Ocean via the Gulf of Mexico.

 

The park sits on the Yellowstone Plateau, at an average elevation of 8,000 feet (2,400 m) above sea level. The plateau is bounded on nearly all sides by mountain ranges of the Middle Rocky Mountains, which range from 9,000 to 11,000 feet (2,700 to 3,400 m) in elevation. The highest point in the park is atop Eagle Peak (11,358 feet or 3,462 metres) and the lowest is along Reese Creek (5,282 feet or 1,610 metres). Nearby mountain ranges include the Gallatin Range to the northwest, the Beartooth Mountains in the north, the Absaroka Range to the east, and the Teton Range and the Madison Range to the southwest and west. The most prominent summit on the Yellowstone Plateau is Mount Washburn at 10,243 feet (3,122 m).

 

Yellowstone National Park has one of the world's largest petrified forests, trees which were long ago buried by ash and soil and transformed from wood to mineral materials. This ash and other volcanic debris, are believed to have come from the park area itself. This is largely due to the fact that Yellowstone is actually a massive caldera of a supervolcano. There are 290 waterfalls of at least 15 feet (4.6 m) in the park, the highest being the Lower Falls of the Yellowstone River at 308 feet (94 m).

 

Three deep canyons are located in the park, cut through the volcanic tuff of the Yellowstone Plateau by rivers over the last 640,000 years. The Lewis River flows through Lewis Canyon in the south, and the Yellowstone River has carved two colorful canyons, the Grand Canyon of the Yellowstone and the Black Canyon of the Yellowstone in its journey north.

 

Yellowstone is at the northeastern end of the Snake River Plain, a great U-shaped arc through the mountains that extends from Boise, Idaho some 400 miles (640 km) to the west. This feature traces the route of the North American Plate over the last 17 million years as it was transported by plate tectonics across a stationary mantle hotspot. The landscape of present-day Yellowstone National Park is the most recent manifestation of this hotspot below the crust of the Earth.

 

The Yellowstone Caldera is the largest volcanic system in North America. It has been termed a "supervolcano" because the caldera was formed by exceptionally large explosive eruptions. The magma chamber that lies under Yellowstone is estimated to be a single connected chamber, about 37 miles (60 km) long, 18 miles (29 km) wide, and 3 to 7 miles (5 to 12 km) deep. The current caldera was created by a cataclysmic eruption that occurred 640,000 years ago, which released more than 240 cubic miles (1,000 km³) of ash, rock and pyroclastic materials. This eruption was more than 1,000 times larger than the 1980 eruption of Mount St. Helens. It produced a caldera nearly five eighths of a mile (1 km) deep and 45 by 28 miles (72 by 45 km) in area and deposited the Lava Creek Tuff, a welded tuff geologic formation. The most violent known eruption, which occurred 2.1 million years ago, ejected 588 cubic miles (2,450 km³) of volcanic material and created the rock formation known as the Huckleberry Ridge Tuff and created the Island Park Caldera. A smaller eruption ejected 67 cubic miles (280 km³) of material 1.3 million years ago, forming the Henry's Fork Caldera and depositing the Mesa Falls Tuff.

 

Each of the three climactic eruptions released vast amounts of ash that blanketed much of central North America, falling many hundreds of miles away. The amount of ash and gases released into the atmosphere probably caused significant impacts to world weather patterns and led to the extinction of some species, primarily in North America.

Wooden walkways allow visitors to closely approach the Grand Prismatic Spring.

 

A subsequent caldera-forming eruption occurred about 160,000 years ago. It formed the relatively small caldera that contains the West Thumb of Yellowstone Lake. Since the last supereruption, a series of smaller eruptive cycles between 640,000 and 70,000 years ago, has nearly filled in the Yellowstone Caldera with >80 different eruptions of rhyolitic lavas such as those that can be seen at Obsidian Cliffs and basaltic lavas which can be viewed at Sheepeater Cliff. Lava strata are most easily seen at the Grand Canyon of the Yellowstone, where the Yellowstone River continues to carve into the ancient lava flows. The canyon is a classic V-shaped valley, indicative of river-type erosion rather than erosion caused by glaciation.

 

Each eruption is part of an eruptive cycle that climaxes with the partial collapse of the roof of the volcano's partially emptied magma chamber. This creates a collapsed depression, called a caldera, and releases vast amounts of volcanic material, usually through fissures that ring the caldera. The time between the last three cataclysmic eruptions in the Yellowstone area has ranged from 600,000 to 800,000 years, but the small number of such climactic eruptions cannot be used to make an accurate prediction for future volcanic events.

 

The most famous geyser in the park, and perhaps the world, is Old Faithful Geyser, located in Upper Geyser Basin. Castle Geyser, Lion Geyser and Beehive Geyser are in the same basin. The park contains the largest active geyser in the world—Steamboat Geyser in the Norris Geyser Basin. A study that was completed in 2011 found that at least 1283 geysers have erupted in Yellowstone. Of these, an average of 465 are active in a given year. Yellowstone contains at least 10,000 geothermal features altogether. Half the geothermal features and two-thirds of the world's geysers are concentrated in Yellowstone.

 

In May 2001, the U.S. Geological Survey, Yellowstone National Park, and the University of Utah created the Yellowstone Volcano Observatory (YVO), a partnership for long-term monitoring of the geological processes of the Yellowstone Plateau volcanic field, for disseminating information concerning the potential hazards of this geologically active region.

 

In 2003, changes at the Norris Geyser Basin resulted in the temporary closure of some trails in the basin. New fumaroles were observed, and several geysers showed enhanced activity and increasing water temperatures. Several geysers became so hot that they were transformed into purely steaming features; the water had become superheated and they could no longer erupt normally. This coincided with the release of reports of a multiple year United States Geological Survey research project which mapped the bottom of Yellowstone Lake and identified a structural dome that had uplifted at some time in the past. Research indicated that these uplifts posed no immediate threat of a volcanic eruption, since they may have developed long ago, and there had been no temperature increase found near the uplifts. On March 10, 2004, a biologist discovered 5 dead bison which apparently had inhaled toxic geothermal gases trapped in the Norris Geyser Basin by a seasonal atmospheric inversion. This was closely followed by an upsurge of earthquake activity in April 2004. In 2006, it was reported that the Mallard Lake Dome and the Sour Creek Dome— areas that have long been known to show significant changes in their ground movement— had risen at a rate of 1.5 to 2.4 inches (3.8 to 6.1 cm) per year from mid–2004 through 2006. As of late 2007, the uplift has continued at a reduced rate. These events inspired a great deal of media attention and speculation about the geologic future of the region. Experts responded to the conjecture by informing the public that there was no increased risk of a volcanic eruption in the near future. However, these changes demonstrate the dynamic nature of the Yellowstone hydrothermal system.

 

Yellowstone experiences thousands of small earthquakes every year, virtually all of which are undetectable to people. There have been six earthquakes with at least magnitude 6 or greater in historical times, including a 7.5‑magnitude quake that struck just outside the northwest boundary of the park in 1959. This quake triggered a huge landslide, which caused a partial dam collapse on Hebgen Lake; immediately downstream, the sediment from the landslide dammed the river and created a new lake, known as Earthquake Lake. Twenty-eight people were killed, and property damage was extensive in the immediate region. The earthquake caused some geysers in the northwestern section of the park to erupt, large cracks in the ground formed and emitted steam, and some hot springs that normally have clear water turned muddy. A 6.1‑magnitude earthquake struck inside the park on June 30, 1975, but damage was minimal.

 

For three months in 1985, 3,000 minor earthquakes were detected in the northwestern section of the park, during what has been referred to as an earthquake swarm, and has been attributed to minor subsidence of the Yellowstone caldera. Beginning on April 30, 2007, 16 small earthquakes with magnitudes up to 2.7 occurred in the Yellowstone Caldera for several days. These swarms of earthquakes are common, and there have been 70 such swarms between 1983 and 2008. In December 2008, over 250 earthquakes were measured over a four-day span under Yellowstone Lake, the largest measuring a magnitude of 3.9. In January 2010, more than 250 earthquakes were detected over a two-day period. Seismic activity in Yellowstone National Park continues and is reported hourly by the Earthquake Hazards Program of the U.S. Geological Survey.

 

On March 30, 2014, a magnitude 4.8 earthquake struck almost the very middle of Yellowstone near the Norris Basin at 6.34am; reports indicated no damage. This was the biggest earthquake to hit the park since February 22, 1980.

 

Over 1,700 species of trees and other vascular plants are native to the park. Another 170 species are considered to be exotic species and are non-native. Of the eight conifer tree species documented, Lodgepole Pine forests cover 80% of the total forested areas. Other conifers, such as Subalpine Fir, Engelmann Spruce, Rocky Mountain Douglas-fir and Whitebark Pine, are found in scattered groves throughout the park. As of 2007, the whitebark pine is threatened by a fungus known as white pine blister rust; however, this is mostly confined to forests well to the north and west. In Yellowstone, about seven percent of the whitebark pine species have been impacted with the fungus, compared to nearly complete infestations in northwestern Montana. Quaking Aspen and willows are the most common species of deciduous trees. The aspen forests have declined significantly since the early 20th century, but scientists at Oregon State University attribute recent recovery of the aspen to the reintroduction of wolves which has changed the grazing habits of local elk.

 

There are dozens of species of flowering plants that have been identified, most of which bloom between the months of May and September. The Yellowstone Sand Verbena is a rare flowering plant found only in Yellowstone. It is closely related to species usually found in much warmer climates, making the sand verbena an enigma. The estimated 8,000 examples of this rare flowering plant all make their home in the sandy soils on the shores of Yellowstone Lake, well above the waterline.

 

In Yellowstone's hot waters, bacteria form mats of bizarre shapes consisting of trillions of individuals. These bacteria are some of the most primitive life forms on earth. Flies and other arthropods live on the mats, even in the middle of the bitterly cold winters. Initially, scientists thought that microbes there gained sustenance only from sulfur. In 2005 researchers from the University of Colorado at Boulder discovered that the sustenance for at least some of the diverse hyperthermophilic species is molecular hydrogen.

 

Thermus aquaticus is a bacterium found in the Yellowstone hot springs that produces an important enzyme (Taq polymerase) that is easily replicated in the lab and is useful in replicating DNA as part of the polymerase chain reaction (PCR) process. The retrieval of these bacteria can be achieved with no impact to the ecosystem. Other bacteria in the Yellowstone hot springs may also prove useful to scientists who are searching for cures for various diseases.

 

Non-native plants sometimes threaten native species by using up nutrient resources. Though exotic species are most commonly found in areas with the greatest human visitation, such as near roads and at major tourist areas, they have also spread into the backcountry. Generally, most exotic species are controlled by pulling the plants out of the soil or by spraying, both of which are time consuming and expensive.

  

Yellowstone is widely considered to be the finest megafauna wildlife habitat in the lower 48 states. There are almost 60 species of mammals in the park, including the gray wolf, the threatened lynx, and grizzly bears. Other large mammals include the bison (often referred to as buffalo), black bear, elk, moose, mule deer, white-tailed deer, mountain goat, pronghorn, bighorn sheep, and mountain lion.

Bison graze near a hot spring

 

The Yellowstone Park bison herd is the largest public herd of American bison in the United States. The relatively large bison populations are a concern for ranchers, who fear that the species can transmit bovine diseases to their domesticated cousins. In fact, about half of Yellowstone's bison have been exposed to brucellosis, a bacterial disease that came to North America with European cattle that may cause cattle to miscarry. The disease has little effect on park bison, and no reported case of transmission from wild bison to domestic livestock has been filed. However, the Animal and Plant Health Inspection Service (APHIS) has stated that bison are the "likely source" of the spread of the disease in cattle in Wyoming and North Dakota. Elk also carry the disease and are believed to have transmitted the infection to horses and cattle. Bison once numbered between 30 and 60 million individuals throughout North America, and Yellowstone remains one of their last strongholds. Their populations had increased from less than 50 in the park in 1902 to 4,000 by 2003. The Yellowstone Park bison herd reached a peak in 2005 with 4,900 animals. Despite a summer estimated population of 4,700 in 2007, the number dropped to 3,000 in 2008 after a harsh winter and controversial brucellosis management sending hundreds to slaughter. The Yellowstone Park bison herd is believed to be one of only four free roaming and genetically pure herds on public lands in North America. The other three herds are the Henry Mountains bison herd of Utah, at Wind Cave National Park in South Dakota and on Elk Island in Alberta.

Elk Mother Nursing Her Calf

 

To combat the perceived threat of brucellosis transmission to cattle, national park personnel regularly harass bison herds back into the park when they venture outside of the area's borders. During the winter of 1996–97, the bison herd was so large that 1,079 bison that had exited the park were shot or sent to slaughter. Animal rights activists argue that this is a cruel practice and that the possibility for disease transmission is not as great as some ranchers maintain. Ecologists point out that the bison are merely traveling to seasonal grazing areas that lie within the Greater Yellowstone Ecosystem that have been converted to cattle grazing, some of which are within National Forests and are leased to private ranchers. APHIS has stated that with vaccinations and other means, brucellosis can be eliminated from the bison and elk herds throughout Yellowstone.

A reintroduced northwestern wolf in Yellowstone National Park

 

Starting in 1914, in an effort to protect elk populations, the U.S. Congress appropriated funds to be used for the purposes of "destroying wolves, prairie dogs, and other animals injurious to agriculture and animal husbandry" on public lands. Park Service hunters carried out these orders, and by 1926 they had killed 136 wolves, and wolves were virtually eliminated from Yellowstone. Further exterminations continued until the National Park Service ended the practice in 1935. With the passing of the Endangered Species Act in 1973, the wolf was one of the first mammal species listed. After the wolves were extirpated from Yellowstone, the coyote then became the park's top canine predator. However, the coyote is not able to bring down large animals, and the result of this lack of a top predator on these populations was a marked increase in lame and sick megafauna.

Bison in Yellowstone National Park

 

By the 1990s, the Federal government had reversed its views on wolves. In a controversial decision by the U.S. Fish and Wildlife Service (which oversees threatened and endangered species), northwestern wolves, imported from Canada, were reintroduced into the park. Reintroduction efforts have been successful with populations remaining relatively stable. A survey conducted in 2005 reported that there were 13 wolf packs, totaling 118 individuals in Yellowstone and 326 in the entire ecosystem. These park figures were lower than those reported in 2004 but may be attributable to wolf migration to other nearby areas as suggested by the substantial increase in the Montana population during that interval. Almost all the wolves documented were descended from the 66 wolves reintroduced in 1995–96. The recovery of populations throughout the states of Wyoming, Montana and Idaho has been so successful that on February 27, 2008, the U.S. Fish and Wildlife Service removed the Northern Rocky Mountain wolf population from the endangered species list.

 

An estimated 600 grizzly bears live in the Greater Yellowstone Ecosystem, with more than half of the population living within Yellowstone. The grizzly is currently listed as a threatened species, however the U.S. Fish and Wildlife Service has announced that they intend to take it off the endangered species list for the Yellowstone region but will likely keep it listed in areas where it has not yet recovered fully. Opponents of delisting the grizzly are concerned that states might once again allow hunting and that better conservation measures need to be implemented to ensure a sustainable population. Black bears are common in the park and were a park symbol due to visitor interaction with the bears starting in 1910. Feeding and close contact with bears has not been permitted since the 1960s to reduce their desire for human foods. Yellowstone is one of the few places in the United States where black bears can be seen coexisting with grizzly bears. Black bear observations occur most often in the park's northern ranges and in the Bechler area which is in the park's southwestern corner.

 

Population figures for elk are in excess of 30,000—the largest population of any large mammal species in Yellowstone. The northern herd has decreased enormously since the mid‑1990s; this has been attributed to wolf predation and causal effects such as elk using more forested regions to evade predation, consequently making it harder for researchers to accurately count them. The northern herd migrates west into southwestern Montana in the winter. The southern herd migrates southward, and the majority of these elk winter on the National Elk Refuge, immediately southeast of Grand Teton National Park. The southern herd migration is the largest mammalian migration remaining in the U.S. outside of Alaska.

 

In 2003 the tracks of one female lynx and her cub were spotted and followed for over 2 miles (3.2 km). Fecal material and other evidence obtained were tested and confirmed to be those of a lynx. No visual confirmation was made, however. Lynx have not been seen in Yellowstone since 1998, though DNA taken from hair samples obtained in 2001 confirmed that lynx were at least transient to the park. Other less commonly seen mammals include the mountain lion and wolverine. The mountain lion has an estimated population of only 25 individuals parkwide. The wolverine is another rare park mammal, and accurate population figures for this species are not known. These uncommon and rare mammals provide insight into the health of protected lands such as Yellowstone and help managers make determinations as to how best to preserve habitats.

 

Eighteen species of fish live in Yellowstone, including the core range of the Yellowstone cutthroat trout—a fish highly sought by anglers. The Yellowstone cutthroat trout has faced several threats since the 1980s, including the suspected illegal introduction into Yellowstone Lake of lake trout, an invasive species which consume the smaller cutthroat trout. Although lake trout were established in Shoshone and Lewis lakes in the Snake River drainage from U.S. Government stocking operations in 1890, it was never officially introduced into the Yellowstone River drainage. The cutthroat trout has also faced an ongoing drought, as well as the accidental introduction of a parasite—whirling disease—which causes a terminal nervous system disease in younger fish. Since 2001, all native sport fish species caught in Yellowstone waterways are subject to a catch and release law. Yellowstone is also home to six species of reptiles, such as the painted turtle and Prairie rattlesnake, and four species of amphibians, including the Boreal Chorus Frog.

 

311 species of birds have been reported, almost half of which nest in Yellowstone. As of 1999, twenty-six pairs of nesting bald eagles have been documented. Extremely rare sightings of whooping cranes have been recorded, however only three examples of this species are known to live in the Rocky Mountains, out of 385 known worldwide. Other birds, considered to be species of special concern because of their rarity in Yellowstone, include the common loon, harlequin duck, osprey, peregrine falcon and the trumpeter swan.

 

As wildfire is a natural part of most ecosystems, plants that are indigenous to Yellowstone have adapted in a variety of ways. Douglas-fir have a thick bark which protects the inner section of the tree from most fires. Lodgepole Pines —the most common tree species in the park— generally have cones that are only opened by the heat of fire. Their seeds are held in place by a tough resin, and fire assists in melting the resin, allowing the seeds to disperse. Fire clears out dead and downed wood, providing fewer obstacles for lodgepole pines to flourish. Subalpine Fir, Engelmann Spruce, Whitebark Pine, and other species tend to grow in colder and moister areas, where fire is less likely to occur. Aspen trees sprout new growth from their roots, and even if a severe fire kills the tree above ground, the roots often survive unharmed because they are insulated from the heat by soil. The National Park Service estimates that in natural conditions, grasslands in Yellowstone burned an average of every 20 to 25 years, while forests in the park would experience fire about every 300 years.

 

About thirty-five natural forest fires are ignited each year by lightning, while another six to ten are started by people— in most cases by accident. Yellowstone National Park has three fire lookout towers, each staffed by trained fire fighters. The easiest one to reach is atop Mount Washburn, though it is closed to the public. The park also monitors fire from the air and relies on visitor reports of smoke and/or flames. Fire towers are staffed almost continuously from late June to mid-September— the primary fire season. Fires burn with the greatest intensity in the late afternoon and evening. Few fires burn more than 100 acres (40 ha), and the vast majority of fires reach only a little over an acre (0.5 ha) before they burn themselves out. Fire management focuses on monitoring dead and down wood quantities, soil and tree moisture, and the weather, to determine those areas most vulnerable to fire should one ignite. Current policy is to suppress all human caused fires and to evaluate natural fires, examining the benefit or detriment they may pose on the ecosystem. If a fire is considered to be an immediate threat to people and structures, or will burn out of control, then fire suppression is performed.

 

In an effort to minimize the chances of out of control fires and threats to people and structures, park employees do more than just monitor the potential for fire. Controlled burns are prescribed fires which are deliberately started to remove dead timber under conditions which allow fire fighters an opportunity to carefully control where and how much wood is consumed. Natural fires are sometimes considered prescribed fires if they are left to burn. In Yellowstone, unlike some other parks, there have been very few fires deliberately started by employees as prescribed burns. However, over the last 30 years, over 300 natural fires have been allowed to burn naturally. In addition, fire fighters remove dead and down wood and other hazards from areas where they will be a potential fire threat to lives and property, reducing the chances of fire danger in these areas. Fire monitors also regulate fire through educational services to the public and have been known to temporarily ban campfires from campgrounds during periods of high fire danger. The common notion in early United States land management policies was that all forest fires were bad. Fire was seen as a purely destructive force and there was little understanding that it was an integral part of the ecosystem. Consequently, until the 1970s, when a better understanding of wildfire was developed, all fires were suppressed. This led to an increase in dead and dying forests, which would later provide the fuel load for fires that would be much harder, and in some cases, impossible to control. Fire Management Plans were implemented, detailing that natural fires should be allowed to burn if they posed no immediate threat to lives and property.

 

1988 started with a wet spring season although by summer, drought began moving in throughout the northern Rockies, creating the driest year on record to that point. Grasses and plants which grew well in the early summer from the abundant spring moisture produced plenty of grass, which soon turned to dry tinder. The National Park Service began firefighting efforts to keep the fires under control, but the extreme drought made suppression difficult. Between July 15 and 21, 1988, fires quickly spread from 8,500 acres (3,400 ha; 13.3 sq mi) throughout the entire Yellowstone region, which included areas outside the park, to 99,000 acres (40,000 ha; 155 sq mi) on the park land alone. By the end of the month, the fires were out of control. Large fires burned together, and on August 20, 1988, the single worst day of the fires, more than 150,000 acres (61,000 ha; 230 sq mi) were consumed. Seven large fires were responsible for 95% of the 793,000 acres (321,000 ha; 1,239 sq mi) that were burned over the next couple of months. A total of 25,000 firefighters and U.S. military forces participated in the suppression efforts, at a cost of 120 million dollars. By the time winter brought snow that helped extinguish the last flames, the fires had destroyed 67 structures and caused several million dollars in damage. Though no civilian lives were lost, two personnel associated with the firefighting efforts were killed.

 

Contrary to media reports and speculation at the time, the fires killed very few park animals— surveys indicated that only about 345 elk (of an estimated 40,000–50,000), 36 deer, 12 moose, 6 black bears, and 9 bison had perished. Changes in fire management policies were implemented by land management agencies throughout the United States, based on knowledge gained from the 1988 fires and the evaluation of scientists and experts from various fields. By 1992, Yellowstone had adopted a new fire management plan which observed stricter guidelines for the management of natural fires.

 

from Wikipedia

  

surface features of an area that are man-made #3

  

This owl features a striking, silhouetted owl sitting on a tree branch in front of the shimmering moon – painted in glow-in-the-dark paint. The irises of the owl’s eyes – created using broken, red, reflector lights, in a mosaic style, also glow in the dark, making this a luminously lovely Midnight Owl.

 

Artist: Jayne Deeley

Jayne Deeley, a Staffordshire based artist, was creative from an early age and this has continued to the present day. She studied HND 3D Design and it was during this time that she discovered new materials to work with and techniques to create Art and Craft works – skills that she later used in her role as a window dresser within a department store and still uses today, while creating handmade greetings cards, jewellery and anything else that inspires her!

Find out more about Jayne at www.facebook.com/JayneDeeleyArtDesign

 

Sponsor: Fort Dunlop

Auction Price: £6000

 

The Big Hoot captured the imagination of everyone in Birmingham and beyond, with hundreds of thousands of people taking to the streets with their Big Hoot Trail maps to explore the colourful invasion of individually designed owls. Taking in the city’s 10 districts, tourists and residents alike enjoyed their owl adventure, discovering and celebrating the extraordinary creativity produced by many of Birmingham’s artistic community and over 25,000 young people.

 

The Big Hoot owls went under the hammer on 15 October 2015 at The Big Hoot auction sponsored by Vodafone and we are thrilled to have smashed our target by raising the incredible sum of £508,035!

 

The money raised from the auction will support Birmingham Children’s Hospital Charity’s £3.65m Star Appeal. This appeal will enable us to create a first of its kind, a Rare Diseases Centre in the UK specifically for children. It will provide co-ordinated care, treatment, support and most importantly hope to children and families living with a rare or undiagnosed condition.

 

In addition the auction raised £15,000 for G’owl’d by Temper with proceeds going to Edward’s Trust, and £7,800 for Fleet and Free with proceeds going to Birchfield Harriers.

 

So thank you - we simply couldn’t have done it without you.

 

Artists have played a major role in The Big Hoot, creating almost 100 owl sculptures. We would like to thank all the artists for their incredible creativity and hard work.

Professional artists from Birmingham, the wider Midlands region and further afield have created extraordinary giant owls that are all unique in style and character and represent the city’s creativity, history and heritage, music, fashion, architecture and attractions.

Birmingham is home to a wealth of artistic and creative individuals and communities and many award-winning and nationally and internationally acclaimed artists. We are delighted with the response from Birmingham’s creative community and are thrilled to work in collaboration with them to transform the streets, squares and parks of the city.

For five months artists have been creating owls in their studios, at home and in The Big Hoot Artists’ Studio at the Custard Factory in Digbeth. Their inspiring and innovative designs have been realised in genres including graffiti, illustration, fine art, graphics, typography, mosaic and new media. They have worked with both community groups and with corporates to realise ideas and create their stunning designs.

The Big Hoot not only provides a high quality and ambitious free public event for families but also supports the creativity of artists and celebrates talent and diversity. The Big Hoot has provided an inspiring relationship between the city and the arts.

The artists have also reached out to communities enabling more people to participate in the arts, to experience working with professional artists and to be inspiring and inspired. From the north to the south of the city residents groups, youth groups and older peoples’ groups have been collaborating with artists to generate ideas, design and create owls for The Big Hoot.

Creativity is everywhere but the opportunity to participate is not. A range of activities have been programmed within Birmingham’s diverse communities and people from the age of 3 – 97 and from wards within the city boundaries have contributed to The Big Hoot and helped make the event extraordinary. Our projects have seen artists working with hundreds of residents and community members including children in looked after care, older peoples’ clubs, young people and residents organisations to design and decorate the owls displayed as part of the 10 week public event.

TOKYO, JAPAN - JUNE 09: Jason "f0rsakeN" Susanto of Paper Rex at VALORANT Masters Tokyo Features Day on June 9, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

TOKYO, JAPAN - JUNE 09: (L-R) Wang "Jinggg" Jing Jie, Jason "f0rsakeN" Susanto and Khalish "d4v41" Rusyaidee of Paper Rex at VALORANT Masters Tokyo Features Day on June 9, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

The 1991-92 UD set was released in two series of 500 and 200 cards, respectively. The front design features action photos with white borders. The player's name and position appear in the top white border, while the team name is given in the bottom white border. Biographical information, statistics, or player profile are displayed on the back alongside a second color photo. The All-Rookie Team and the Star Rookies are marked by the abbreviations ART and SR respectively in the list below. A randomly inserted Glasnost card (SP1) featuring Wayne Gretzky, Brett Hull and Valeri Kamensky and ballots by which fans could vote for their favorite NHL All-Stars were included in foil packs. Special subsets include members of the teams that participated in the IIHF World Junior Championships (650--699).

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Patrick Roy - Patrick Jacques Roy (born October 5, 1965) is a Canadian professional ice hockey coach, executive and former player who is the head coach for the New York Islanders of the National Hockey League. Roy previously served as head coach for the Colorado Avalanche of the NHL, as well as the Quebec Remparts of the Quebec Major Junior Hockey League. In 2017, he was named one of the 100 Greatest NHL Players in history and was hailed in sports media as "king of goaltenders".

 

Nicknamed "Saint Patrick", Roy split his playing career in the National Hockey League between the Montreal Canadiens, with whom he played for 11 years, and the Colorado Avalanche, with whom he played for eight years. Roy won the Stanley Cup four times during his career, two with each franchise.

 

In 2004, Roy was selected as the greatest goaltender in NHL history by a panel of 41 writers, coupled with a simultaneous fan poll. On November 13, 2006, Roy was inducted into the Hockey Hall of Fame. He is the only player in NHL history to win the Conn Smythe Trophy (the award given to the Most Valuable Player in the Stanley Cup playoffs) three times, the only one to do so in three different decades (1980s, 1990s, and 2000s), and the only one to do so for two different teams. Roy's number 33 sweater is retired by both the Canadiens and Avalanche.

 

Roy is widely credited with popularizing the butterfly style of goaltending, which has since become the dominant style of goaltending around the world.

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LINK to - Patrick Roy AutographFacts - www.psacard.com/autographfacts/hockey/patrick-roy/852 and - www.psacard.com/autographfacts/hockey/patrick-roy/images/852

 

By the time the trading card industry boomed, Roy was front and center as a hobby star and his autographs from 1991-92 Pro Set Series One were the first pack-inserted certified autographs in the hockey card market. More awards followed and he backstopped the Canadiens to a Stanley Cup in 1992-93. Traded to the Colorado Avalanche during the 1995-96 season, he played a key part in leading the former Quebec Nordiques to the franchise’s first title. Another followed five years later, along with a record third Conn Smythe Trophy.

 

“It’s really exciting to see what has happened in the last couple of years,” Roy said that winter day in early 1992. “When Upper Deck came in, their cards are so nice and different than anything we have ever had. There are other new companies too. The competition has made everybody get better, from the photography being used now to the quality of the cards.” Roy was, by this point, part of the Upper Deck stable of stars so it’s no surprise that he would extol their greatness. And he was right. In 1991 and 1992, Upper Deck was raising the bar in the sports card industry.

 

LINK to video - Patrick Roy talks about his autograph style and sports memorabilia - www.youtube.com/watch?v=dUejiGe3470

TOKYO, JAPAN - JUNE 09: Paper Rex at VALORANT Masters Tokyo Features Day on June 9, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

TOKYO, JAPAN - JUNE 09: Wang "Jinggg" Jing Jie of Paper Rex at VALORANT Masters Tokyo Features Day on June 9, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.

 

The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater. Due to the Yellowstone Plateau's high elevation the average boiling temperature at Yellowstone's geyser basins is 199 °F (93 °C). When properly confined and close to the surface it can periodically release some of the built-up pressure in eruptions of hot water and steam that can reach up to 390 feet (120 m) into the air (see Steamboat Geyser, the world's tallest geyser). Water erupting from Yellowstone's geysers is superheated above that boiling point to an average of 204 °F (95.5 °C) as it leaves the vent. The water cools significantly while airborne and is no longer scalding hot by the time it strikes the ground, nearby boardwalks, or even spectators. Because of the high temperatures of the water in the features it is important that spectators remain on the boardwalks and designated trails. Several deaths have occurred in the park as a result of falls into hot springs.

 

Prehistoric Native American artifacts have been found at Mammoth Hot Springs and other geothermal areas in Yellowstone. Some accounts state that the early people used hot water from the geothermal features for bathing and cooking. In the 19th century Father Pierre-Jean De Smet reported that natives he interviewed thought that geyser eruptions were "the result of combat between the infernal spirits". The Lewis and Clark Expedition traveled north of the Yellowstone area in 1806. Local natives that they came upon seldom dared to enter what we now know is the caldera because of frequent loud noises that sounded like thunder and the belief that the spirits that possessed the area did not like human intrusion into their realm. The first white man known to travel into the caldera and see the geothermal features was John Colter, who had left the Lewis and Clark Expedition. He described what he saw as "hot spring brimstone". Beaver trapper Joseph Meek recounted in 1830 that the steam rising from the various geyser basins reminded him of smoke coming from industrial smokestacks on a cold winter morning in Pittsburgh, Pennsylvania. In the 1850s famed trapper Jim Bridger called it "the place where Hell bubbled up".

 

The heat that drives geothermal activity in the Yellowstone area comes from brine (salty water) that is 1.5–3 miles (7,900–15,800 ft; 2,400–4,800 m) below the surface. This is actually below the solid volcanic rock and sediment that extends to a depth of 3,000 to 6,000 feet (900 to 1,800 m) and is inside the hot but mostly solid part of the pluton that contains Yellowstone's magma chamber. At that depth the brine is superheated to temperatures that exceed 400 °F (204 °C) but is able to remain a liquid because it is under great pressure (like a huge pressure cooker).

 

Convection of the churning brine and conduction from surrounding rock transfers heat to an overlaying layer of fresh groundwater. Movement of the two liquids is facilitated by the highly fractured and porous nature of the rocks under the Yellowstone Plateau. Some silica is dissolved from the fractured rhyolite into the hot water as it travels through the fractured rock. Part of this hard mineral is later redeposited on the walls of the cracks and fissures to make a nearly pressure-tight system. Silica precipitates at the surface to form either geyserite or sinter, creating the massive geyser cones, the scalloped edges of hot springs, and the seemingly barren landscape of geyser basins.

 

There are at least five types of geothermal features found at Yellowstone:

 

Fumaroles: Fumaroles, or steam vents, are the hottest hydrothermal features in the park. They have so little water that it all flashes into steam before reaching the surface. At places like Roaring Mountain, the result is loud hissing of steam and gases.

Geysers: Geysers such as Old Faithful are a type of geothermal feature that periodically erupt scalding hot water. Increased pressure exerted by the enormous weight of the overlying rock and water prevents deeper water from boiling. As the hot water rises it is under less pressure and steam bubbles form. They, in turn, expand on their ascent until the bubbles are too big and numerous to pass freely through constrictions. At a critical point the confined bubbles actually lift the water above, causing the geyser to splash or overflow. This decreases the pressure of the system and violent boiling results. Large quantities of water flash into tremendous amounts of steam that force a jet of water out of the vent: an eruption begins. Water (and heat) is expelled faster than the geyser's recharge rate, gradually decreasing the system's pressure and eventually ending the eruption.

Hot springs: Hot springs such as Grand Prismatic Spring are the most common hydrothermal features in the park. Their plumbing has no constrictions. Superheated water cools as it reaches the surface, sinks, and is replaced by hotter water from below. This circulation, called convection, prevents water from reaching the temperature needed to set off an eruption. Many hot springs give rise to streams of heated water.

Mudpots: Mudpots such as Fountain Paint Pots are acidic hot springs with a limited water supply. Some microorganisms use hydrogen sulfide (rotten egg smell), which rises from deep within the earth, as an energy source. They convert the gas into sulfuric acid, which breaks down rock into clay.

Travertine terraces: Travertine terraces, found at Mammoth Hot Springs, are formed from limestone (a rock type made of calcium carbonate). Thermal waters rise through the limestone, carrying high amounts of dissolved carbonate. Carbon dioxide is released at the surface and calcium carbonate deposited as travertine, the chalky white rock of the terraces. These features constantly and quickly change due to the rapid rate of deposition.

Geyser basins

 

The Norris Geyser Basin 44°43′43″N 110°42′16″W is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago.

 

The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters.

 

The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.

 

Algae on left bacteria on right at the intersection of flows from the Constant & Whirlgig Geysers at Norris Geyser Basin

The tallest active geyser in the world, Steamboat Geyser,[11] is located in Norris Basin. Unlike the slightly smaller but much more famous Old Faithful Geyser located in Upper Geyser Basin, Steamboat has an erratic and lengthy timetable between major eruptions. During major eruptions, which may be separated by intervals of more than a year (the longest recorded span between major eruptions was 50 years), Steamboat erupts over 300 feet (90 m) into the air. Steamboat does not lie dormant between eruptions, instead displaying minor eruptions of approximately 40 feet (12 m).

 

Norris Geyser Basin periodically undergoes a large-scale, basin-wide thermal disturbance lasting a few weeks. Water levels fluctuate, and temperatures, pH, colors, and eruptive patterns change throughout the basin. During a disturbance in 1985, Porkchop Geyser continually jetted steam and water; in 1989, the same geyser apparently clogged with silica and blew up, throwing rocks more than 200 feet (61 m). In 2003 a park ranger observed it bubbling heavily, the first such activity seen since 1991. Activity increased dramatically in mid-2003. Because of high ground temperatures and new features beside the trail much of Back Basin was closed until October. In 2004 the boardwalk was routed around the dangerous area and now leads behind Porkchop Geyser.

 

North of Norris, Roaring Mountain is a large, acidic hydrothermal area (solfatara) with many fumaroles. In the late 19th and early 20th centuries, the number, size, and power of the fumaroles were much greater than today. The fumaroles are most easily seen in the cooler, low-light conditions of morning and evening.

 

The Gibbon Geyser Basin 44°41′58″N 110°44′34″W includes several thermal areas in the vicinity of the Gibbon River between Gibbon Falls and Norris. The most accessible feature in the basin is Beryl Spring, with a small boardwalk right along the Grand Loop Road. Artists' Paintpots is a small hydrothermal area south of Norris Junction that includes colorful hot springs and two large mudpots.

 

The Monument Geyser Basin 44°41′03″N 110°45′14″W has no active geysers, but its 'monuments' are siliceous sinter deposits similar to the siliceous spires discovered on the floor of Yellowstone Lake. Scientists hypothesize that this basin's structures formed from a hot water system in a glacially dammed lake during the waning stages of the Pinedale Glaciation. The basin is on a ridge reached by a very steep one-mile (1.6 km) trail south of Artists' Paint Pots. Other areas of thermal activity in Gibbon Geyser Basin lie off-trail.

 

South of Norris along the rim of the caldera is the Upper Geyser Basin 44°27′52″N 110°49′45″W, which has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet (430 m) northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin.

 

The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.

 

Evidence of glacial activity is common, and it is one of the keys that allows geysers to exist. Glacier till deposits underlie the geyser basins providing storage areas for the water used in eruptions. Many landforms, such as Porcupine Hills north of Fountain Flats, are made up of glacial gravel and are reminders that 70,000 to 14,000 years ago, this area was buried under ice.

 

Signs of the forces of erosion can be seen everywhere, from runoff channels carved across the sinter in the geyser basins to the drainage created by the Firehole River. Mountain building is evident on the drive south of Old Faithful, toward Craig Pass. Here the Rocky Mountains reach a height of 8,262 feet (2,518 m), dividing the country into two distinct watersheds.

 

Midway Geyser Basin 44°31′04″N 110°49′56″W is much smaller than the other basins found alongside the Firehole River. Despite its small size, it contains two large features, the 200-by-300-foot-wide (60 by 90 m) Excelsior Geyser which pours over 4,000 U.S. gallons (15,000 L; 3,300 imp gal) per minute into the Firehole River. The largest hot spring in Yellowstone, the 370-foot-wide (110 m) and 121-foot-deep (37 m) Grand Prismatic Spring is found here. Also in the basin is Turquoise Pool and Opal Pool.

 

Lower Geyser Basin

Blue spring with steam rising from it; irregular blotches of red and orange residue are on the banks, along with dead tree trunks.

Silex Spring at Fountain Paint Pot

 

Farther north is the Lower Geyser Basin 44°32′58″N 110°50′09″W, which is the largest geyser basin in area, covering approximately 11 square miles. Due to its large size, it has a much less concentrated set of geothermal features, including Fountain Paint Pots. Fountain Paint Pots are mud pots, that is, a hot spring that contains boiling mud instead of water. The mud is produced by a higher acidity in the water which enables the spring to dissolve surrounding minerals to create an opaque, usually grey, mud. Also there is Firehole Spring, Celestine Pool, Leather Pool, Red Spouter, Jelly spring, and a number of fumaroles.

 

Geysers in Lower Geyser Basin include Great Fountain Geyser, whose eruptions reach 100 to 200 feet (30–61 m) in the air, while waves of water cascade down its sinter terraces., the Fountain group of Geysers (Clepsydra Geyser which erupts nearly continuously to heights of 45 feet (14 m), Fountain Geyser, Jelly Geyser, Jet Geyser, Morning Geyser, and Spasm Geyser), the Pink Cone group of geysers (Dilemma Geyser, Labial Geyser, Narcissus Geyser, Pink Geyser, and Pink Cone Geyser), the White Dome group of geysers (Crack Geyser, Gemini Geyser, Pebble Geyser, Rejuvenated Geyser, and White Dome Geyser), as well as Sizzler Geyser.

 

Clepsydra Geyser erupting. July 2019

Fountain Paint Pots

White Dome Geyser

West Thumb Geyser Basin

Several pools of blue water in ashen rock basin.

West Thumb Geyser Basin

Blackened basin with orange streaks; steam is rising from it with fir trees in the background.

Overflow areas of Silex springs

 

The West Thumb Geyser Basin 44°25′07″N 110°34′23″W, including Potts Basin to the north, is the largest geyser basin on the shores of Yellowstone Lake. The heat source of the thermal features in this location is thought to be relatively close to the surface, only 10,000 feet (3,000 m) down. West Thumb is about the same size as another famous volcanic caldera, Crater Lake in Oregon, but much smaller than the great Yellowstone Caldera which last erupted about 640,000 years ago. West Thumb is a caldera within a caldera.

 

West Thumb was created approximately 162,000 years ago when a magma chamber bulged up under the surface of the earth and subsequently cracked it along ring fracture zones. This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today.

 

The thermal features at West Thumb are not only found on the lake shore, but extend under the surface of the lake as well. Several underwater hydrothermal features were discovered in the early 1990s and can be seen as slick spots or slight bulges in the summer. During the winter, the underwater thermal features are visible as melt holes in the icy surface of the lake. The surrounding ice can reach three feet (one yard) in thickness.

 

Perhaps the most famous hydrothermal feature at West Thumb is a geyser on the lake shore known as Fishing Cone. Walter Trumbull of the 1870 Washburn-Langford-Doane Expedition described a unique event while a man was fishing adjacent to the cone: "...in swinging a trout ashore, it accidentally got off the hook and fell into the spring. For a moment it darted about with wonderful rapidity, as if seeking an outlet. Then it came to the top, dead, and literally boiled." Fishing Cone erupted frequently to the height of 40 feet (12 m) in 1919 and to lesser heights in 1939. One fisherman was badly burned in Fishing Cone in 1921. Fishing at the geyser is now prohibited.

 

Early visitors would arrive at West Thumb via stagecoach from the Old Faithful area. They had a choice of continuing on the stagecoach or boarding the steamship Zillah to continue the journey by water to Lake Hotel. The boat dock was located near the south end of the geyser basin near Lakeside Spring.

 

Backcountry Geyser Basins

The Heart Lake 44°18′00″N 110°30′56″W, Lone Star 44°24′50″N 110°49′04″W, and Shoshone Geyser Basins 44°21′16″N 110°47′57″W are located away from the road and require at least several miles of hiking to reach. These areas lack the boardwalks and other safety features of the developed areas. As falling into geothermal features can be fatal, it is usually advisable to visit these areas with an experienced guide or at the very least, travelers need to ensure they remain on well-marked trails.

 

The Heart Lake Geyser Basin contains several groups of geysers and deep blue hot springs near Heart Lake in the south-central portion of Yellowstone, southeast of most of the main geyser basins. Lying in the Snake River watershed east of Lewis Lake and south of Yellowstone Lake, Heart Lake was named sometime before 1871 for Hart Hunney, a hunter. Other explorers in the region incorrectly assumed that the lake's name was spelled 'heart' because of its shape. The Heart Lake Geyser Basin begins a couple miles from the lake and descends along Witch Creek to the lakeshore. Five groups of hydrothermal features comprise the basin, and all of them contain geysers, although some are dormant.

 

Between Shoshone Lake and Old Faithful is the Lone Star Geyser Basin, of which the primary feature is Lone Star Geyser, named for its isolation from the nearby geysers of the Upper Geyser Basin. The basin is reachable on foot or bicycle via a 3 mile road that is closed to vehicles.

 

The Shoshone Geyser Basin, reached by hiking or by boat, contains one of the highest concentrations of geysers in the world – more than 80 in an area 1,600 by 800 feet (490 by 240 m). Hot springs and mudpots dot the landscape between the geyser basin and Shoshone Lake.

 

Hot Spring Basin is located 15 miles (24 km) north-northeast of Fishing Bridge and has one of Yellowstone's largest collections of hot springs and fumaroles. The geothermal features there release large amounts of sulfur. This makes water from the springs so acidic that it has dissolved holes in the pants of people who sit on wet ground and causes mounds of sulfur three feet (1 m) high to develop around fumaroles. The very hot acidic water and steam have also created voids in the ground that are only covered by a thin crust.

 

Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas.

 

The thermal features at Mud Volcano and Sulphur Caldron are primarily mud pots and fumaroles because the area is situated on a perched water system with little water available. Fumaroles or "steam vents" occur when the ground water boils away faster than it can be recharged. Also, the vapors are rich in sulfuric acid that leaches the rock, breaking it down into clay. Because no water washes away the acid or leached rock, it remains as sticky clay to form a mud pot. Hydrogen sulfide gas is present deep in the earth at Mud Volcano and is oxidized to sulfuric acid by microbial activity, which dissolves the surface soils to create pools and cones of clay and mud. Along with hydrogen sulfide, steam, carbon dioxide, and other gases explode through the layers of mud.

 

A series of shallow earthquakes associated with the volcanic activity in Yellowstone struck this area in 1978. Soil temperatures increased to nearly 200 °F (93 °C). The slope between Sizzling Basin and Mud Geyser, once covered with green grass and trees, became a barren landscape of fallen trees known as "the cooking hillside".

 

Yellowstone National Park is a national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion.

 

While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park originally fell under the jurisdiction of the U.S. Department of the Interior, the first Secretary of the Interior to supervise the park being Columbus Delano. However, the U.S. Army was eventually commissioned to oversee the management of Yellowstone for 30 years between 1886 and 1916. In 1917, the administration of the park was transferred to the National Park Service, which had been created the previous year. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than a thousand archaeological sites.

 

Yellowstone National Park spans an area of 3,468.4 sq mi (8,983 km2), comprising lakes, canyons, rivers, and mountain ranges. Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest super volcano on the continent. The caldera is considered a dormant volcano. It has erupted with tremendous force several times in the last two million years. Well over half of the world's geysers and hydrothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly intact ecosystem in the Earth's northern temperate zone. In 1978, Yellowstone was named a UNESCO World Heritage Site.

 

Hundreds of species of mammals, birds, fish, reptiles, and amphibians have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the contiguous United States. Grizzly bears, cougars, wolves, and free-ranging herds of bison and elk live in this park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one-third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing, and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.

 

Teton County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 23,331. Its county seat is Jackson. Its west boundary line is also the Wyoming state boundary shared with Idaho and the southern tip of Montana. Teton County is part of the Jackson, WY-ID Micropolitan Statistical Area.

 

Teton County contains the Jackson Hole ski area, all of Grand Teton National Park, and 40.4% of Yellowstone National Park's total area, including over 96.6% of its water area (largely in Yellowstone Lake).

 

Wyoming is a state in the Mountain West subregion of the Western United States. It borders Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in 2020, Wyoming is the least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is Cheyenne, which had an estimated population of 63,957 in 2018.

 

Wyoming's western half consists mostly of the ranges and rangelands of the Rocky Mountains; its eastern half consists of high-elevation prairie, and is referred to as the High Plains. Wyoming's climate is semi-arid in some parts and continental in others, making it drier and windier overall than other states, with greater temperature extremes. The federal government owns just under half of Wyoming's land, generally protecting it for public uses. The state ranks sixth in the amount of land—-and fifth in the proportion of its land—-that is owned by the federal government. Its federal lands include two national parks (Grand Teton and Yellowstone), two national recreation areas, two national monuments, and several national forests, as well as historic sites, fish hatcheries, and wildlife refuges.

 

Indigenous peoples inhabited the region for thousands of years. Historic and currently federally recognized tribes include the Arapaho, Crow, Lakota, and Shoshone. Part of the land that is now Wyoming came under American sovereignty via the Louisiana Purchase, part via the Oregon Treaty, and, lastly, via the Mexican Cession. With the opening of the Oregon Trail, the Mormon Trail, and the California Trail, vast numbers of pioneers travelled through parts of the state that had once been traversed mainly by fur trappers, and this spurred the establishment of forts, such as Fort Laramie, that today serve as population centers. The Transcontinental Railroad supplanted the wagon trails in 1867 with a route through southern Wyoming, bringing new settlers and the establishment of founding towns, including the state capital of Cheyenne. On March 27, 1890, Wyoming became the union's 44th state.

 

Farming and ranching, and the attendant range wars, feature prominently in the state's history. Today, Wyoming's economy is largely based on tourism and the extraction of minerals such as coal, natural gas, oil, and trona. Its agricultural commodities include barley, hay, livestock, sugar beets, wheat, and wool.

 

Wyoming was the first state to allow women the right to vote (not counting New Jersey, which had allowed it until 1807), and the right to assume elected office, as well as the first state to elect a female governor. In honor of this part of its history, its most common nickname is "The Equality State" and its official state motto is "Equal Rights". It is among the least religious states in the country, and is known for having a political culture that leans towards libertarian conservatism. The Republican presidential nominee has carried the state in every election since 1968.

The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.

 

The various geyser basins are located where rainwater and snowmelt can percolate into the ground, get indirectly superheated by the underlying Yellowstone hotspot, and then erupt at the surface as geysers, hot springs, and fumaroles. Thus flat-bottomed valleys between ancient lava flows and glacial moraines are where most of the large geothermal areas are located. Smaller geothermal areas can be found where fault lines reach the surface, in places along the circular fracture zone around the caldera, and at the base of slopes that collect excess groundwater. Due to the Yellowstone Plateau's high elevation the average boiling temperature at Yellowstone's geyser basins is 199 °F (93 °C). When properly confined and close to the surface it can periodically release some of the built-up pressure in eruptions of hot water and steam that can reach up to 390 feet (120 m) into the air (see Steamboat Geyser, the world's tallest geyser). Water erupting from Yellowstone's geysers is superheated above that boiling point to an average of 204 °F (95.5 °C) as it leaves the vent. The water cools significantly while airborne and is no longer scalding hot by the time it strikes the ground, nearby boardwalks, or even spectators. Because of the high temperatures of the water in the features it is important that spectators remain on the boardwalks and designated trails. Several deaths have occurred in the park as a result of falls into hot springs.

 

Prehistoric Native American artifacts have been found at Mammoth Hot Springs and other geothermal areas in Yellowstone. Some accounts state that the early people used hot water from the geothermal features for bathing and cooking. In the 19th century Father Pierre-Jean De Smet reported that natives he interviewed thought that geyser eruptions were "the result of combat between the infernal spirits". The Lewis and Clark Expedition traveled north of the Yellowstone area in 1806. Local natives that they came upon seldom dared to enter what we now know is the caldera because of frequent loud noises that sounded like thunder and the belief that the spirits that possessed the area did not like human intrusion into their realm. The first white man known to travel into the caldera and see the geothermal features was John Colter, who had left the Lewis and Clark Expedition. He described what he saw as "hot spring brimstone". Beaver trapper Joseph Meek recounted in 1830 that the steam rising from the various geyser basins reminded him of smoke coming from industrial smokestacks on a cold winter morning in Pittsburgh, Pennsylvania. In the 1850s famed trapper Jim Bridger called it "the place where Hell bubbled up".

 

The heat that drives geothermal activity in the Yellowstone area comes from brine (salty water) that is 1.5–3 miles (7,900–15,800 ft; 2,400–4,800 m) below the surface. This is actually below the solid volcanic rock and sediment that extends to a depth of 3,000 to 6,000 feet (900 to 1,800 m) and is inside the hot but mostly solid part of the pluton that contains Yellowstone's magma chamber. At that depth the brine is superheated to temperatures that exceed 400 °F (204 °C) but is able to remain a liquid because it is under great pressure (like a huge pressure cooker).

 

Convection of the churning brine and conduction from surrounding rock transfers heat to an overlaying layer of fresh groundwater. Movement of the two liquids is facilitated by the highly fractured and porous nature of the rocks under the Yellowstone Plateau. Some silica is dissolved from the fractured rhyolite into the hot water as it travels through the fractured rock. Part of this hard mineral is later redeposited on the walls of the cracks and fissures to make a nearly pressure-tight system. Silica precipitates at the surface to form either geyserite or sinter, creating the massive geyser cones, the scalloped edges of hot springs, and the seemingly barren landscape of geyser basins.

 

There are at least five types of geothermal features found at Yellowstone:

 

Fumaroles: Fumaroles, or steam vents, are the hottest hydrothermal features in the park. They have so little water that it all flashes into steam before reaching the surface. At places like Roaring Mountain, the result is loud hissing of steam and gases.

Geysers: Geysers such as Old Faithful are a type of geothermal feature that periodically erupt scalding hot water. Increased pressure exerted by the enormous weight of the overlying rock and water prevents deeper water from boiling. As the hot water rises it is under less pressure and steam bubbles form. They, in turn, expand on their ascent until the bubbles are too big and numerous to pass freely through constrictions. At a critical point the confined bubbles actually lift the water above, causing the geyser to splash or overflow. This decreases the pressure of the system and violent boiling results. Large quantities of water flash into tremendous amounts of steam that force a jet of water out of the vent: an eruption begins. Water (and heat) is expelled faster than the geyser's recharge rate, gradually decreasing the system's pressure and eventually ending the eruption.

Hot springs: Hot springs such as Grand Prismatic Spring are the most common hydrothermal features in the park. Their plumbing has no constrictions. Superheated water cools as it reaches the surface, sinks, and is replaced by hotter water from below. This circulation, called convection, prevents water from reaching the temperature needed to set off an eruption. Many hot springs give rise to streams of heated water.

Mudpots: Mudpots such as Fountain Paint Pots are acidic hot springs with a limited water supply. Some microorganisms use hydrogen sulfide (rotten egg smell), which rises from deep within the earth, as an energy source. They convert the gas into sulfuric acid, which breaks down rock into clay.

Travertine terraces: Travertine terraces, found at Mammoth Hot Springs, are formed from limestone (a rock type made of calcium carbonate). Thermal waters rise through the limestone, carrying high amounts of dissolved carbonate. Carbon dioxide is released at the surface and calcium carbonate deposited as travertine, the chalky white rock of the terraces. These features constantly and quickly change due to the rapid rate of deposition.

Geyser basins

 

The Norris Geyser Basin 44°43′43″N 110°42′16″W is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago.

 

The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters.

 

The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.

 

Algae on left bacteria on right at the intersection of flows from the Constant & Whirlgig Geysers at Norris Geyser Basin

The tallest active geyser in the world, Steamboat Geyser,[11] is located in Norris Basin. Unlike the slightly smaller but much more famous Old Faithful Geyser located in Upper Geyser Basin, Steamboat has an erratic and lengthy timetable between major eruptions. During major eruptions, which may be separated by intervals of more than a year (the longest recorded span between major eruptions was 50 years), Steamboat erupts over 300 feet (90 m) into the air. Steamboat does not lie dormant between eruptions, instead displaying minor eruptions of approximately 40 feet (12 m).

 

Norris Geyser Basin periodically undergoes a large-scale, basin-wide thermal disturbance lasting a few weeks. Water levels fluctuate, and temperatures, pH, colors, and eruptive patterns change throughout the basin. During a disturbance in 1985, Porkchop Geyser continually jetted steam and water; in 1989, the same geyser apparently clogged with silica and blew up, throwing rocks more than 200 feet (61 m). In 2003 a park ranger observed it bubbling heavily, the first such activity seen since 1991. Activity increased dramatically in mid-2003. Because of high ground temperatures and new features beside the trail much of Back Basin was closed until October. In 2004 the boardwalk was routed around the dangerous area and now leads behind Porkchop Geyser.

 

North of Norris, Roaring Mountain is a large, acidic hydrothermal area (solfatara) with many fumaroles. In the late 19th and early 20th centuries, the number, size, and power of the fumaroles were much greater than today. The fumaroles are most easily seen in the cooler, low-light conditions of morning and evening.

 

The Gibbon Geyser Basin 44°41′58″N 110°44′34″W includes several thermal areas in the vicinity of the Gibbon River between Gibbon Falls and Norris. The most accessible feature in the basin is Beryl Spring, with a small boardwalk right along the Grand Loop Road. Artists' Paintpots is a small hydrothermal area south of Norris Junction that includes colorful hot springs and two large mudpots.

 

The Monument Geyser Basin 44°41′03″N 110°45′14″W has no active geysers, but its 'monuments' are siliceous sinter deposits similar to the siliceous spires discovered on the floor of Yellowstone Lake. Scientists hypothesize that this basin's structures formed from a hot water system in a glacially dammed lake during the waning stages of the Pinedale Glaciation. The basin is on a ridge reached by a very steep one-mile (1.6 km) trail south of Artists' Paint Pots. Other areas of thermal activity in Gibbon Geyser Basin lie off-trail.

 

South of Norris along the rim of the caldera is the Upper Geyser Basin 44°27′52″N 110°49′45″W, which has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet (430 m) northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin.

 

The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.

 

Evidence of glacial activity is common, and it is one of the keys that allows geysers to exist. Glacier till deposits underlie the geyser basins providing storage areas for the water used in eruptions. Many landforms, such as Porcupine Hills north of Fountain Flats, are made up of glacial gravel and are reminders that 70,000 to 14,000 years ago, this area was buried under ice.

 

Signs of the forces of erosion can be seen everywhere, from runoff channels carved across the sinter in the geyser basins to the drainage created by the Firehole River. Mountain building is evident on the drive south of Old Faithful, toward Craig Pass. Here the Rocky Mountains reach a height of 8,262 feet (2,518 m), dividing the country into two distinct watersheds.

 

Midway Geyser Basin 44°31′04″N 110°49′56″W is much smaller than the other basins found alongside the Firehole River. Despite its small size, it contains two large features, the 200-by-300-foot-wide (60 by 90 m) Excelsior Geyser which pours over 4,000 U.S. gallons (15,000 L; 3,300 imp gal) per minute into the Firehole River. The largest hot spring in Yellowstone, the 370-foot-wide (110 m) and 121-foot-deep (37 m) Grand Prismatic Spring is found here. Also in the basin is Turquoise Pool and Opal Pool.

 

Lower Geyser Basin

Blue spring with steam rising from it; irregular blotches of red and orange residue are on the banks, along with dead tree trunks.

Silex Spring at Fountain Paint Pot

 

Farther north is the Lower Geyser Basin 44°32′58″N 110°50′09″W, which is the largest geyser basin in area, covering approximately 11 square miles. Due to its large size, it has a much less concentrated set of geothermal features, including Fountain Paint Pots. Fountain Paint Pots are mud pots, that is, a hot spring that contains boiling mud instead of water. The mud is produced by a higher acidity in the water which enables the spring to dissolve surrounding minerals to create an opaque, usually grey, mud. Also there is Firehole Spring, Celestine Pool, Leather Pool, Red Spouter, Jelly spring, and a number of fumaroles.

 

Geysers in Lower Geyser Basin include Great Fountain Geyser, whose eruptions reach 100 to 200 feet (30–61 m) in the air, while waves of water cascade down its sinter terraces., the Fountain group of Geysers (Clepsydra Geyser which erupts nearly continuously to heights of 45 feet (14 m), Fountain Geyser, Jelly Geyser, Jet Geyser, Morning Geyser, and Spasm Geyser), the Pink Cone group of geysers (Dilemma Geyser, Labial Geyser, Narcissus Geyser, Pink Geyser, and Pink Cone Geyser), the White Dome group of geysers (Crack Geyser, Gemini Geyser, Pebble Geyser, Rejuvenated Geyser, and White Dome Geyser), as well as Sizzler Geyser.

 

Clepsydra Geyser erupting. July 2019

Fountain Paint Pots

White Dome Geyser

West Thumb Geyser Basin

Several pools of blue water in ashen rock basin.

West Thumb Geyser Basin

Blackened basin with orange streaks; steam is rising from it with fir trees in the background.

Overflow areas of Silex springs

 

The West Thumb Geyser Basin 44°25′07″N 110°34′23″W, including Potts Basin to the north, is the largest geyser basin on the shores of Yellowstone Lake. The heat source of the thermal features in this location is thought to be relatively close to the surface, only 10,000 feet (3,000 m) down. West Thumb is about the same size as another famous volcanic caldera, Crater Lake in Oregon, but much smaller than the great Yellowstone Caldera which last erupted about 640,000 years ago. West Thumb is a caldera within a caldera.

 

West Thumb was created approximately 162,000 years ago when a magma chamber bulged up under the surface of the earth and subsequently cracked it along ring fracture zones. This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today.

 

The thermal features at West Thumb are not only found on the lake shore, but extend under the surface of the lake as well. Several underwater hydrothermal features were discovered in the early 1990s and can be seen as slick spots or slight bulges in the summer. During the winter, the underwater thermal features are visible as melt holes in the icy surface of the lake. The surrounding ice can reach three feet (one yard) in thickness.

 

Perhaps the most famous hydrothermal feature at West Thumb is a geyser on the lake shore known as Fishing Cone. Walter Trumbull of the 1870 Washburn-Langford-Doane Expedition described a unique event while a man was fishing adjacent to the cone: "...in swinging a trout ashore, it accidentally got off the hook and fell into the spring. For a moment it darted about with wonderful rapidity, as if seeking an outlet. Then it came to the top, dead, and literally boiled." Fishing Cone erupted frequently to the height of 40 feet (12 m) in 1919 and to lesser heights in 1939. One fisherman was badly burned in Fishing Cone in 1921. Fishing at the geyser is now prohibited.

 

Early visitors would arrive at West Thumb via stagecoach from the Old Faithful area. They had a choice of continuing on the stagecoach or boarding the steamship Zillah to continue the journey by water to Lake Hotel. The boat dock was located near the south end of the geyser basin near Lakeside Spring.

 

Backcountry Geyser Basins

The Heart Lake 44°18′00″N 110°30′56″W, Lone Star 44°24′50″N 110°49′04″W, and Shoshone Geyser Basins 44°21′16″N 110°47′57″W are located away from the road and require at least several miles of hiking to reach. These areas lack the boardwalks and other safety features of the developed areas. As falling into geothermal features can be fatal, it is usually advisable to visit these areas with an experienced guide or at the very least, travelers need to ensure they remain on well-marked trails.

 

The Heart Lake Geyser Basin contains several groups of geysers and deep blue hot springs near Heart Lake in the south-central portion of Yellowstone, southeast of most of the main geyser basins. Lying in the Snake River watershed east of Lewis Lake and south of Yellowstone Lake, Heart Lake was named sometime before 1871 for Hart Hunney, a hunter. Other explorers in the region incorrectly assumed that the lake's name was spelled 'heart' because of its shape. The Heart Lake Geyser Basin begins a couple miles from the lake and descends along Witch Creek to the lakeshore. Five groups of hydrothermal features comprise the basin, and all of them contain geysers, although some are dormant.

 

Between Shoshone Lake and Old Faithful is the Lone Star Geyser Basin, of which the primary feature is Lone Star Geyser, named for its isolation from the nearby geysers of the Upper Geyser Basin. The basin is reachable on foot or bicycle via a 3 mile road that is closed to vehicles.

 

The Shoshone Geyser Basin, reached by hiking or by boat, contains one of the highest concentrations of geysers in the world – more than 80 in an area 1,600 by 800 feet (490 by 240 m). Hot springs and mudpots dot the landscape between the geyser basin and Shoshone Lake.

 

Hot Spring Basin is located 15 miles (24 km) north-northeast of Fishing Bridge and has one of Yellowstone's largest collections of hot springs and fumaroles. The geothermal features there release large amounts of sulfur. This makes water from the springs so acidic that it has dissolved holes in the pants of people who sit on wet ground and causes mounds of sulfur three feet (1 m) high to develop around fumaroles. The very hot acidic water and steam have also created voids in the ground that are only covered by a thin crust.

 

Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas.

 

The thermal features at Mud Volcano and Sulphur Caldron are primarily mud pots and fumaroles because the area is situated on a perched water system with little water available. Fumaroles or "steam vents" occur when the ground water boils away faster than it can be recharged. Also, the vapors are rich in sulfuric acid that leaches the rock, breaking it down into clay. Because no water washes away the acid or leached rock, it remains as sticky clay to form a mud pot. Hydrogen sulfide gas is present deep in the earth at Mud Volcano and is oxidized to sulfuric acid by microbial activity, which dissolves the surface soils to create pools and cones of clay and mud. Along with hydrogen sulfide, steam, carbon dioxide, and other gases explode through the layers of mud.

 

A series of shallow earthquakes associated with the volcanic activity in Yellowstone struck this area in 1978. Soil temperatures increased to nearly 200 °F (93 °C). The slope between Sizzling Basin and Mud Geyser, once covered with green grass and trees, became a barren landscape of fallen trees known as "the cooking hillside".

 

Yellowstone National Park is a national park located in the western United States, largely in the northwest corner of Wyoming and extending into Montana and Idaho. It was established by the 42nd U.S. Congress with the Yellowstone National Park Protection Act and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first national park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially the Old Faithful geyser, one of its most popular. While it represents many types of biomes, the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion.

 

While Native Americans have lived in the Yellowstone region for at least 11,000 years, aside from visits by mountain men during the early-to-mid-19th century, organized exploration did not begin until the late 1860s. Management and control of the park originally fell under the jurisdiction of the U.S. Department of the Interior, the first Secretary of the Interior to supervise the park being Columbus Delano. However, the U.S. Army was eventually commissioned to oversee the management of Yellowstone for 30 years between 1886 and 1916. In 1917, the administration of the park was transferred to the National Park Service, which had been created the previous year. Hundreds of structures have been built and are protected for their architectural and historical significance, and researchers have examined more than a thousand archaeological sites.

 

Yellowstone National Park spans an area of 3,468.4 sq mi (8,983 km2), comprising lakes, canyons, rivers, and mountain ranges. Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest super volcano on the continent. The caldera is considered a dormant volcano. It has erupted with tremendous force several times in the last two million years. Well over half of the world's geysers and hydrothermal features are in Yellowstone, fueled by this ongoing volcanism. Lava flows and rocks from volcanic eruptions cover most of the land area of Yellowstone. The park is the centerpiece of the Greater Yellowstone Ecosystem, the largest remaining nearly intact ecosystem in the Earth's northern temperate zone. In 1978, Yellowstone was named a UNESCO World Heritage Site.

 

Hundreds of species of mammals, birds, fish, reptiles, and amphibians have been documented, including several that are either endangered or threatened. The vast forests and grasslands also include unique species of plants. Yellowstone Park is the largest and most famous megafauna location in the contiguous United States. Grizzly bears, cougars, wolves, and free-ranging herds of bison and elk live in this park. The Yellowstone Park bison herd is the oldest and largest public bison herd in the United States. Forest fires occur in the park each year; in the large forest fires of 1988, nearly one-third of the park was burnt. Yellowstone has numerous recreational opportunities, including hiking, camping, boating, fishing, and sightseeing. Paved roads provide close access to the major geothermal areas as well as some of the lakes and waterfalls. During the winter, visitors often access the park by way of guided tours that use either snow coaches or snowmobiles.

 

Teton County is a county in the U.S. state of Wyoming. As of the 2020 United States Census, the population was 23,331. Its county seat is Jackson. Its west boundary line is also the Wyoming state boundary shared with Idaho and the southern tip of Montana. Teton County is part of the Jackson, WY-ID Micropolitan Statistical Area.

 

Teton County contains the Jackson Hole ski area, all of Grand Teton National Park, and 40.4% of Yellowstone National Park's total area, including over 96.6% of its water area (largely in Yellowstone Lake).

 

Wyoming is a state in the Mountain West subregion of the Western United States. It borders Montana to the north and northwest, South Dakota and Nebraska to the east, Idaho to the west, Utah to the southwest, and Colorado to the south. With a population of 576,851 in 2020, Wyoming is the least populous state despite being the 10th largest by area, with the second-lowest population density after Alaska. The state capital and most populous city is Cheyenne, which had an estimated population of 63,957 in 2018.

 

Wyoming's western half consists mostly of the ranges and rangelands of the Rocky Mountains; its eastern half consists of high-elevation prairie, and is referred to as the High Plains. Wyoming's climate is semi-arid in some parts and continental in others, making it drier and windier overall than other states, with greater temperature extremes. The federal government owns just under half of Wyoming's land, generally protecting it for public uses. The state ranks sixth in the amount of land—-and fifth in the proportion of its land—-that is owned by the federal government. Its federal lands include two national parks (Grand Teton and Yellowstone), two national recreation areas, two national monuments, and several national forests, as well as historic sites, fish hatcheries, and wildlife refuges.

 

Indigenous peoples inhabited the region for thousands of years. Historic and currently federally recognized tribes include the Arapaho, Crow, Lakota, and Shoshone. Part of the land that is now Wyoming came under American sovereignty via the Louisiana Purchase, part via the Oregon Treaty, and, lastly, via the Mexican Cession. With the opening of the Oregon Trail, the Mormon Trail, and the California Trail, vast numbers of pioneers travelled through parts of the state that had once been traversed mainly by fur trappers, and this spurred the establishment of forts, such as Fort Laramie, that today serve as population centers. The Transcontinental Railroad supplanted the wagon trails in 1867 with a route through southern Wyoming, bringing new settlers and the establishment of founding towns, including the state capital of Cheyenne. On March 27, 1890, Wyoming became the union's 44th state.

 

Farming and ranching, and the attendant range wars, feature prominently in the state's history. Today, Wyoming's economy is largely based on tourism and the extraction of minerals such as coal, natural gas, oil, and trona. Its agricultural commodities include barley, hay, livestock, sugar beets, wheat, and wool.

 

Wyoming was the first state to allow women the right to vote (not counting New Jersey, which had allowed it until 1807), and the right to assume elected office, as well as the first state to elect a female governor. In honor of this part of its history, its most common nickname is "The Equality State" and its official state motto is "Equal Rights". It is among the least religious states in the country, and is known for having a political culture that leans towards libertarian conservatism. The Republican presidential nominee has carried the state in every election since 1968.

Some rooftop old world architectural features seen in afternoon light .

 

Queen St.

Brisbane

TOKYO, JAPAN - JUNE 09: Jason "f0rsakeN" Susanto of Paper Rex at VALORANT Masters Tokyo Features Day on June 9, 2023 in Tokyo, Japan. (Photo by Lee Aiksoon/Riot Games)

Zuckuss features: Custom molded head and vest, fabric cloak and hand painted details.

 

For this Zuckuss Bounty Hunter and other custom minifigures visit www.minifigmaker.com

www.youtube.com/watch?v=Bn9oxb052bI

And on the second weekend of the year, I take my two camera bodies out for a bit of churchcrawling.

 

Wingham is a substantial town/village between Dover and Canterbury, and was once the terminus of a branch of the East Kent Light Railway, though the nearby mine failed to produce any coal.

 

It is an attractive place, but is blighted by the main road that cuts the town in half, and it is a busy road too. On the road there are three pubs, and many fine and ancient houses.

 

St Mary sits beside the road, and it skirts the churchyard to the south and east, and despite being on a grand scale, mature trees in the churchyard do well to hide it from view.

 

I did come here many years ago back in the early days of the Kent Church project, and took no more than a handful of shots, I thought I could do better that that this time.

 

It is a church full of grand tombs, memorials and other features that I am looking forward to share with you, most curious of which is a curved passageway that leads from the northeast corner of the Oxenden chapel to the chancel.

 

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An enormous church, picturesquely set at an angle of the village street. It owes its size to the fact that it supported a college of priests in the Middle Ages. During the sixteenth century it was substantially rebuilt, but the north aisle was not replaced, reducing the church to the odd shape we see today. The unusual pillars which divide the nave from the south aisle are of timber, not stone as a result of lack of money. At the end of the south aisle is the Oxenden chapel, which contains that family's excellent bull's head monument. The contemporary metalwork screens and black and white pavements add great dignity to this part of the building. By going through a curved passage from the chapel you can emerge in the chancel, which is dominated by a stone reredos of fifteenth-century date. This French construction was a gift to the church in the 1930s and while it is not good quality carving, is an unusual find in a Kent church.

 

www.kentchurches.info/church.asp?p=Wingham

 

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hortly after 1280AD Archbishop Peckham of Canterbury established a college of priests at Wingham, with a provost and six canons. From 1286 the priests lived in the attractive timber-framed house opposite St Mary's church. The college accounts for the size of the church, which seems enormous considering the present size of Wingham itself.

 

There was a cruciform church here before the college was established, but that building was remodelled around 1290, leaving us several excellent Geometric Gothic windows. A south porch and tower were added around 1400. The porch is curious in that there are two stories externally, but internally only one. There are many reminders of the church's past, however; the arch between the south transept and south nave aisle is late Norman, as is a blocked arch on the west wall of the north transept.

 

By the early 16th century the nave was in poor condition. A local brewer named George Ffogarde of Canterbury was granted a license to raise money for its repair. Having a considerable sum of money for church repair, the unscrupulous brewer absconded with the funds, embezzling £224, a huge sum for the time. The missing funds may explain why the nave was rebuilt using cheaper timber posts to support the arcades, rather than more costly stone.

 

The octagonal timber posts are of chestnut wood, topped by a crown-post timber roof. Sometime before the mid-19th century the timbers were encased in plaster to resemble Doric columns, but thankfully the plaster has been stripped off and we can appreciate the timber! The nave was rebuilt in the late 16th century, diminishing its footprint and leaving behind some rather odd features, like an external piscina on what was originally the easternmost pier of the nave arcade. Another odd touch is provided by the north transept, remodelled with wood frames in the Georgian period. I'm not sure I can call to mind another essentially medieval church with wooden-framed windows!

 

In the chancel is a lovely 14th century triple-seat sedilia and piscina. The chancel and nave are separated by a 15th century screen, now truncated, with blank panels which must have once boasted painted figures of saints. But the real treasure in the chancel is a series of ten 14th century misericords. Six of the misericord carvings are simply decorative, with floral or foliage designs. Two show animals; one appears to be a horse, another a donkey. The final two carvings are the most interesting; one shows a woman in a wimple, the other a Green Man peering out from a screen of foliage.

 

Behind the altar is a lovely 15th century reredos, brought here from Troyes in France. The reredos is in two sections, the upper section depicting the Passion of Christ, the lower showing the Last Supper and the Adoration of the Kings. There are small fragments of rather attractive 14th century grisailles glass in the chancel windows, and near the font are a number of surviving medieval floor tiles.

 

The interior is full of monuments to the Oxenden and Palmer families. The finest of these are to be found in the north transept chapel. On the east wall of the chapel is a memorial to Sir Nicholas Palmer (d. 1624). The memorial was designed by Nicholas Stone and shows effigies of Palmer and his wife under Corinthian columns and an open pediment. On the north wall is the monument to a later Thomas Palmer (d. 1656) with a bust of the deceased, now somewhat the worse for wear. A tablet to Streynsham Master (d. 1718) is on the south chapel wall, and has a fairly typical pair of skulls at the base of the tablet, wreathed in olive branches.

 

The most extravagant and eye-catching memorial in the church, however, is to be found in the north transept chapel, which is guarded by ornate wrought-iron screens. In the centre of the chapel is an ebullient obelisk, dated 1682, commemorating the Oxenden family. This free-standing obelisk, possibly designed by Arnold Quellin, is of white stone, with exquisite fruit and flowers cascading down each side, with large black ox heads at each angle of the base. The base is embellished with four putti (cherubic 'infants'). The effect is quite extraordinary; most people will either love it or hate it (I loved it). Also in the south transept is a wall tablet to Charles Tripp (d. 1624).

Other monuments worth mentioning include a 14th century tomb recess in the south aisle wall and a number of 15th century indents in the chancel floor which once contained memorial brasses to canons.

 

The church is set within a large walled enclosure, dating to the 16th and 17th centuries. Unusually, the churchyard wall has been listed Grade-II by the Department of the Environment for its historical interest.

 

www.britainexpress.com/counties/kent/churches/wingham.htm

 

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WINGHAM

IS the next adjoining parish south-westward from Ash, situated for the most part in the upper half hundred of the same name, and having in it the boroughs of Wingham-street, Deane, Twitham, and Wenderton, which latter is in the lower half hundred of Wingham.

 

WINGHAM is situated in a healthy pleasant country, the greatest part of it is open uninclosed arable lands, the soil of which, though chalky, is far from being unfertile. The village, or town of Wingham, is nearly in the middle of the parish, having the church and college at the south-west part of it; behind the latter is a field, still called the Vineyard. The village contains about fifty houses, one of which is the court-lodge, and is built on the road leading from Canterbury to Sandwich, at the west end of it runs the stream, called the Wingham river, which having turned a corn-mill here, goes on and joins the Lesser Stour, about two miles below; on each side the stream is a moist tract of meadow land. Near the south boundary of the parish is the mansion of Dene, situated in the bottom, a dry, though dull and gloomy habitation; and at the opposite side, next to Staple, the ruinated mansion of Brook, in a far more open and pleasant situation. To the northward the parish extends a considerable way, almost as far as the churches of Preston and Elmstone. The market, granted anno 36 king Henry III. as mentioned hereafter, if it ever was held, has been disused for a number of years past; though the market-house seems yet remaining. There are two fairs held yearly here, on May 12, and November 12, for cattle and pedlary.

 

In 1710 there was found on the court-lodge farm, by the plough striking against it, a chest or coffin, of large thick stones, joined together, and covered with a single one at the top. At the bottom were some black ashes, but nothing else in it. The ground round about was searched, but nothing else was sound.

 

Henry de Wengham, a person of great note and extraordinary parts, and much in favour with Henry III. was born here, who in 1255 made him lord chancellor. In 1259, he was elected bishop of Winchester, which he resused, but towards the latter end of the same year he was chosen bishop of London, being still chancellor, and was consecrated the beginning of the year following. He died in 1262, and was buried in his own cathedral. He bore for his arms, Gules, a heart between two wings, displayed, or.

 

WILLIAM COWPER, ESQ. eldest son of Sir William Cowper, bart. of Ratling-court, in Nonington, having been made lord-keeper of the great seal in 1705, was afterwards by letters patent, dated Dec. 14, 1706, created lord Cowper, baron Cowper of Wingham; and in 1709, was declared lord chancellor. After which, anno 4 George I. he was created earl Cowper and viscount Fordwich, in whose descendants these titles have continued down to the right hon. Peter-Lewis-Francis Cowper, the fifth and present earl Cowper, viscount Fordwich and baron of Wingham. (fn. 1)

 

The MANOR OF WINGHAM was part of the antient possessions of the see of Canterbury, given to it in the early period of the Saxon heptarchy, but being torn from it during the troubles of those times, it was restored to the church in the year 941, by king Edmund, his brother Eadred, and Edwin that king's son. (fn. 2) Accordingly it is thus entered, under the general title of the archbishop's possessions, taken in the survey of Domesday:

 

In the lath of Estrei, in Wingeham hundred, the archbishop himself holds Wingeham in demesne. It was taxed at forty sulings in the time of king Edward the Consessor, and now for thirty-five. The arable land is . . . . . . In demesne there are eight carucates, and four times twenty and five villeins, with twenty borderers having fifty-seven carucates. There are eight servants, and two mills of thirty-four sulings. Wood for the pannage of five hogs, and two small woods for fencing. In its whole value, in the time of king Edward the Consessor, it was worth seventy-seven pounds, when he received it the like, and now one hundred pounds. Of this manor William de Arcis holds one suling in Fletes, and there be has in demesne one carucate, and four villeins, and one knight with one carucate, and one fisbery, with a saltpit of thirty pence. The whole value is forty shillings. Of this ma nor five of the archbishop's men hold five sulings and an half and three yokes, and there they have in demesne eight carucates, and twenty-two borderers, and eight servants. In the whole they are worth twenty-one pounds.

 

In the 36th year of king Henry III. archbishop Boniface obtained the grant of a market at this place. The archbishops had a good house on this manor, in which they frequently resided. Archbishop Baldwin, in king Henry II.'s reign, staid at his house here for some time during his contention with the monks of Christ-church, concerning his college at Hackington. Archbishop Winchelsea entertained king Edward I. here in his 23d year, as did archbishop Walter Reynolds king Edward II. in his 18th year. And king Edward III. in his 5th year, having landed at Dover, with many lords and nobles in his train, came to Wingham, where he was lodged and entertained by archbishop Meopham. And this manor continued part of the see of Canterbury till archbishop Cranmer, in the 29th year of king Henry VIII. exchanged it with the king for other premises. After which it continued in the crown till king Charles I. in his 5th year, granted the scite, called Wingham court, with the demesne lands of the manor, to trustees, for the use of the city of London. From whom, by the direction of the mayor and commonalty, it was conveyed, at the latter end of that reign, to Sir William Cowper, knight and baronet, in whose descendants it has continued down to the right hon. Peter-Francis Cowper, earl Cowper, who is the present owner of it. (fn. 3)

 

BUT THE MANOR ITSELF, with the royalties, profits of courts, &c. remained still in the crown. Since which, the bailiwic of it, containing the rents and pro fits of the courts, with the fines, amerciaments, reliess, &c. and the privilege of holding the courts of it, by the bailiff of it, have been granted to the family of Oxenden, and Sir Henry Oxenden, bart. of Brome, is now in possession of the bailiwic of it. A court leet and court baron is held for this manor.

 

TRAPHAM is a mansion in this parish, which was formerly in the possession of a family of the same name, who resided at it, but after they were extinct it passed into that of Trippe, who bore for their arms, Gules, a chevron, or, between three borses heads erased, sable, bridled, collared and crined of the second; (fn. 4) and John Tripp, esq. resided here in queen Elizabeth's reign, as did his grandson Charles, who seems to have alienated it to Sir Christopher Harflete, of St. Stephen's, whose son Tho. Harflete, esq. left an only daughter and heir Afra, who carried it in marriage to John St. Leger, esq. of Doneraile, in Ireland, descended from Sir Anthony St. Leger, lord deputy of Ireland in Henry VIII.'s reign, and they joined in the alienation of it to Brook Bridges, esq of the adjoining parish of Goodneston, whose descendant Sir Brook Wm. Bridges, bart. of that place, is the present owner of it.

 

The MANOR OF DENE, situated in the valley, at the southern boundary of this parish, was antiently the inheritance of a family who took their surname from it, and held it by knight's service of the archbishop, in king Edward I's reign, but they seem to have been extinct here in that of king Edward III. After which it passed into the family of Hussey, who bore for their arms, Per chevron, argent and vert, three birds counterchanged; and then to Wood, before it came by sale into the family of Oxenden, who appear to have been possessed of it at the latter end of Henry VI.'s reign, about which time they had become by marriage, owners of Brook and other estates in this parish. The family of Oxenden have been resident in this county from the reign of king Edward III. Solomon Oxenden, being the first mentioned in the several pedigrees of it, whose near relation Richard Oxenden was prior of Christchurch, Canterbury, in that reign; in this name and family of Oxenden, whose arms were Argent, a chevron, gules, between three oxen, sable, armed, or; which coat was confirmed to the family by Gyan, king at arms, anno 24 Henry VI. this manor and seat continued down to Sir Henry Oxenden, of Dene, who was on May 8, 1678, created a baronet, whose youngest grandson Sir George Oxenden, bart. succeeding at length to the title on the death of his eldest brother Sir Henry, resided at Dene, where he died in 1775, having served in parliament for Sandwich, and been employed in high offices in administration, and leaving behind him the character of a compleat gentleman. He married Elizabeth, one of the daughters and coheirs of Edward Dunck, esq. of Little Wittenham, in Berkshire, by whom he had two sons, of whom George, the second, was made by will heir to the estate of Sir Basil Dixwell, bart. of Brome, on his death, s. p. and changed his name to Dixwell as enjoined by it, but died soon afterwards likewise, s. p. and that estate came at length to his eldest brother Henry, who succeeded his father in the title of Baronet. He married Margaret, daughter and coheir of Sir George Chudleigh, bart. of Devonshire, since deceased, by whom he has issue Henry Oxenden, esq. of Madekyn, in Barham, who married Mary, one of the daughters of Col. Graham, of St. Laurence, near Canterbury, by whom he has issue. Sir Henry Oxenden, bart. now resides at Brome, and is the present possessor of this manor and seat, as well as the rest of his father's estates in this parish. (fn. 5) Lady Hales, widow of Sir Thomas Pym Hales, bart. of Bekesborne, now resides in it.

 

TWITHAM, now usually called Twittam, is a hamlet in this parish, adjoining to Goodneston, the principal estate in which once belonged to a family of that name, one of whom Alanus de Twitham is recorded as having been with king Richard I. at the siege of Acon, in Palestine, who bore for his arms, Semee of crosscroslets, and three cinquesoils, argent, and held this estate in Twitham, of the archbishop, and they appear to have continued possessed of it in the 3d year of king Richard II. Some time after which it came into the possession of Fineux, and William Fineux sold it anno 33 Henry VIII. to Ingram Wollet, whose heirs passed it away to one of the family of Oxenden, of Wingham, in whose descendants it has continued down to Sir Henry Oxenden, bart. of Brome, the present possessor of it.

 

On the foundation of the college of Wingham, archbishop Peckham, in 1286, endowed the first diaconal prebend in it, which he distinguished by the name of the prebend of Twitham, with the tithes of the lands of Alanus de Twitham, which he freely held of the archbishop there in Goodwynestone, at Twytham. (fn. 6)

 

BROOK is an estate in this parish, situated northward from Twitham, which was formerly the estate of the Wendertons, of Wenderton, in this parish, in which it remained till by a female heir Jane, it went in marriage to Richard Oxenden, gent. of Wingham, who died in 1440, and was buried in Wingham church, in whose name and family it continued down to Henry Oxenden, of Brook, who left two daughters and coheirs, of whom Mary married Richard Oxenden, of Grays Inn, barrister-at-law, fourth son of Sir Henry Oxenden, bart, who afterwards, on his wife's becoming sole heiress of Brook, possessed it, and resided here. He left Elizabeth his sole daughter and heir, who carried it in marriage to Streynsham Master, esq. a captain in the royal navy, the eldest surviving son of James Master, esq. of East Langdon, who died some few days after his marriage; upon which she became again possessed of it in her own right, and dying in 1759, s. p. gave it by will to Henry Oxenden, esq. now Sir Henry Oxenden, bart. of Brome, and he is the present owner of it.

 

WENDERTON is a manor and antient seat, situated northward from Wingham church, eminent, says Philipott, for its excellent air, situation, and prospect, which for many successive generations had owners of that surname, one of whom, John de Wenderton, is mentioned in Fox's Martyrology, as one among other tenants of the manor of Wingham, on whom archbishop Courtnay, in 1390, imposed a penance for neglecting to perform some services due from that manor. In his descendants this seat continued till John Wenderton, of Wenderton, in the 1st year of Henry VIII. passed it away to archbishop Warham, who at his decease in 1533, gave it to his youngest brother John Warham, whose great-grandson John, by his will in 1609, ordered this manor to be sold, which it accordingly soon afterwards was to Manwood, from which name it was alienated, about the middle of the next reign of king Charles I. to Vincent Denne, gent. who resided here, and died in 1642, s. p. whose four nieces afterwards became by will possessed of it, and on the partition of their estates, the manor and mansion, with part of the lands since called Great Wenderton, was allotted to Mary, the youngest of them, who afterwards married Vincent Denne, sergeant-at-law, and the remaining part of it, which adjoins to them, since called Little Wenderton, to Dorothy, the third sister, afterwards married to Roger Lukin, gent. of London, who soon afterwards sold his share to Richard Oxenden, esq. of Brook, from one of which family it was sold to Underdown, by a female heir of which name, Frances, it went in marriage to John Carter, esq. of Deal, the present owner of it.

 

BUT GREAT WENDERTON continued in the possession of Sergeant Denne, till his death in 1693, when Dorothy, his eldest daughter and coheir, carried it in marriage to Mr. Thomas Ginder, who bore Argent, on a pale, sable, a cross fuchee, or, impaling azure, three lions heads, or; as they are on his monument. He resided at it till his death in 1716, as did his widow till her decease in 1736, when it came to her nephew Mr. Thomas Hatley, who left two daughters his coheirs, the eldest surviving of whom, Anne, carried it in marriage, first to Richard Nicholas, esq. and then successively to Mr. Smith and Mr. James Corneck, of London, and Mrs. Corneck, the widow of the latter, is the present possessor of it.

 

At the boundary of this parish, adjoining to Preston and Ash, lies THE MANOR OF WALMESTONE, usually called Wamston, which was antiently part of the possessions of the family of Septvans, one of whom, Robert de Septvans, held it in king Edward II.'s reign, of the archbishop; whose descendant Sir William de Septvans died possessed of it in the 25th year of that reign. (fn. 7) How long it continued in this name I have not found; but at the beginning of king Edward IV.'s reign it was become the property of William Bonington, of Canterbury, who died in 1463, and directed it by his will to be sold. After which it became, about the latter end of king Henry VIII.'s reign, the property of Walter Hendley, esq. the king's attorney-general, who left three daughters his coheirs, and they joined in the sale of it to Alday, who alienated it to Benedict Barnham, esq. alderman of London, one of whose daughters and coheirs, Elizabeth, carried it in marriage to Mervin Touchet, earl of Castlehaven, who being convicted of high crimes and misdemeanors, was executed anno 7 Charles I. Soon after which this manor seems to have been divided, and one part of it, since called Little Walmestone, in which was included the manor and part of the demesne lands, passed from his heirs to the Rev. John Smith, rector of Wickham Breaus, who having founded a scholarship at Oxford, out of the lands of it, presently afterwards sold it to Solly, of Pedding, in which name it continued till Stephen Solly, gent. of Pedding, and his two sons, John and Stephen, in 1653, joined in the conveyance of it to Thomas Winter, yeoman, of Wingham, in which name it remained for some time. At length, after some intermediate owners, it was sold to Sympson, and John Sympson, esq. of Canterbury, died possessed of it in 1748, leaving his wife surviving, who held it at her decease, upon which it came to her husband's heir-atlaw, and it is now accordingly in the possession of Mr. Richard Simpson.

 

BUT GREAT WALMESTONE, consisting of the mansion-house, with a greater part of the demesne lands of the manor, was passed away by the heirs of the earl of Castlehaven to Brigham, and Mr. Charles Brigham, of London, in the year 1653, sold it to William Rutland, of London, who left two daughters his coheirs, of whom Mary married John Ketch, by whom she had a sole daughter Anne, who afterwards at length became possessed of it, and carried it in marriage to Samuel Starling, gent. of Worcestershire, who in 1718, conveyed it, his only son Samuel joining in it, to Thomas Willys, esq. of London, afterwards created a baronet. After which it passed in the same manner, and in the like interests and shares, as the manor of Dargate, in Hernehill, down to Matthew, Robert and Thomas Mitchell, the trustees for the several uses to which this, among other estates belonging to the Willis's, had been limited; and they joined in the sale of it, in 1789, to Mr. William East, whose son, Mr. John East, of Wingham, is the present owner of it.

 

ARCHBISHOP KILWARBY intended to found a college in this church of Wingham, but resigning his archbishopric before he could put his design in practice, archbishop Peckham, his successor, in the year 1286, perfected his predecessor's design, and founded A COLLEGE in this church, for a provost, whose portion, among other premises, was the profits of this church and the vicarage of it, and six secular canons; the prebends of which he distinguished by the names of the several places from whence their respective portions arose, viz. Chilton, Pedding, Twitham, Bonnington, Ratling, and Wimlingswold. The provost's lodge, which appears by the foundation charter to have before been the parsonage, was situated adjoining to the church-yard; and the houses of the canons, at this time called Canon-row, opposite to it. These latter houses are, with their gardens and appurtenances, esteemed to be within the liberty of the town and port of Hastings, and jurisdiction of the cinque ports. This college was suppressed in the 1st year of king Edward VI. among others of the like sort, when the whole revenue of it was valued at 208l. 14s. 3½d. per annum, and 193l. 2s. 1d. clear; but Leland says, it was able to dispend at the suppression only eighty-four pounds per annum. Edward Cranmer, the last master, had at the dissolution a pension of twenty pounds per annum, which he enjoyed in 1553. (fn. 8)

 

After the dissolution of the college, the capital mansion, late belonging to the provost, remained in the crown till king Edward VI. in his 7th year, granted the scite of it, with the church appropriate of Wingham, and all tithes whatsoever arising within the parish, and one acre of glebe-land in it, to Sir Henry Palmer, subject to a payment of twenty pounds annually to the curate or vicar of it.

 

The Palmers of Wingham were descended from a very antient one at Angmerin, in Suffex, who bore for their arms, Or, two bars, gules, each charged with three tresoils of the field, in chief, a greyhound, currant, sable. In the seventh descent from Ralph Palmer, esq. of that place, in king Edward II.'s reign, was descended Sir Edward Palmer, of Angmerin, who left three sons, born on three successive Sundays, of whom John, the eldest, was of Sussex, which branch became extinct in queen Elizabeth's reign; Sir Henry, the second son, was of Wingham; and Sir Thomas, the youngest, was beheaded in queen Mary's reign. Sir Henry Palmer, the second son, having purchased the grant of the college of Wingham, as before-mentioned, made it the seat of his residence, as did his son Sir Thomas Palmer, who was sheriff anno 37 Elizabeth, and created a baronet in 1621. He so constantly resided at Wingham, that he is said to have kept sixty Christmases, without intermission, in this mansion, with great hospitality. He had three sons, each of whom were knighted. From the youngest of whom, Sir James, descended the Palmers, of Dauney, in Buckinghamshire, who upon the eldest branch becoming extinct, have succeeded to the title of baronet; and by his second wife he had Roger Palmer, earl of Castlemain. Sir Thomas Palmer, the eldest of the three brothers, died in his father's life-time, and left Sir Thomas Palmer, bart. of Wingham, heir to his grandfather; in whose descendants, baronets, of this place, this mansion, with the parsonage of Wingham appropriate, continued down to Sir Thomas Palmer, bart. of Wingham, who died possessed of it in 1723, having had three wives; by the first he had four daughters; by the second he had a son Herbert, born before marriage, and afterwards a daughter Frances; the third was Mrs. Markham, by whom he had no issue; and she afterwards married Thomas Hey, esq. whom she likewise survived. Sir Thomas Palmer, by his will, gave this seat, with the parsonage appropriate and tithes of Wingham, inter alia, after his widow's decease, to his natural son Herbert Palmer, esq. above-mentioned, who married Bethia, fourth daughter of Sir Thomas D'Aeth, bart. of Knolton. He died in 1760, s. p. and by will devised his interest in the reversion of this seat, with the parsonage, to his wife Bethia, for her life, and afterwards to his sister Mrs. Frances Palmer, in tail. But he never had possession of it, for lady Palmer furvived him, on whose death in 1763, Mrs. Bethia Palmer, his widow, became entitled to it, and afterwards married John Cosnan, esq. who died in 1773. She survived him, and resided here till her death in 1789. In the intermediate time, Mrs. Frances Palmer having barred the entail made by her natural brother Herbett above-mentioned, died, having devised the see of this estate, by her will in 1770, to the Rev. Thomas Hey, rector of Wickhambreaux, and his heirs, being the eldest son of the last lady Palmer by her last husband. Mr. Hey accordingly, on the death of Mrs. Cosnan, who died s. p. succeeded to this seat and estate. He married first Ethelreda, eldest daughter and coheir of dean Lynch, since deceased, by whom he has no surviving issue; and secondly, Mrs. Pugett, widow of Mr. Puget, of London. He now resides in this seat of Wingham college, having been created D. D. and promoted to a prebend of the church of Rochester.

 

Charities.

JOHN CHURCH, yeoman, of this parish, in 1604, gave 1cl. to the poor, to distribute yearly at Easter, 10s. to the poor for the interest of it.

 

HECTOR DU MONT, a Frenchman, born in 1632, gave the silver cup and patten for the holy communion.

 

SIR GEORGE OXENDEN, president for the East-India Company at Surat, in 1660, gave the velvet cushion and pulpitcloth.

 

JOHN RUSHBEACHER, gent. of this parish, in 1663, gave five acres of land in Woodnesborough, the rents to be annually distributed to ten of the meaner sort of people of Wingham, not receiving alms of the parish, now of the yearly value of 4l.

 

SIR GEORGE OXENDEN, above-mentioned, in 1682, gave 500l. for the repairing and beautifying this church, and the Dene chancel.

 

SIR JAMES OXENDEN, knight and baronet, of Dene, founded and endowed a school in this parish with 16l. per annum for ever, for teaching twenty poor children reading and writing, now in the patronage of Sir Henry Oxenden, bart.

 

RICHARD OXENDEN, esq. of Brook, in 1701, gave an annuity of 4l. for ever, to the minister, for the reading of divine service and preaching a sermon, in this church, on every Wednesday in Lent, and on Good Friday; and he at the same time gave 20s. yearly for ever, to be distributed, with the consent of the heirs of the Brook estate, to eight poor people, who should be at divine service on Easter-day, to be paid out of the lands of Brook, now vested in Sir Henry Oxenden, bart.

 

THOMAS PALMER, esq. of St. Dunstan's in the East, London, gave 300l for the repairing, adorning and beautifying the great chancel of this church.

 

MRS. ELIZABETH MASTER, esq. relict of Strensham Master, of Brook, in 1728, gave the large silver flaggon; and MRS. SYBILLA OXENDEN, spinster, of Brook, at the same time gave a large silver patten for the communion.

 

Besides the above benefactions, there have been several lesser ones given at different times in money, both to the poor and for the church. All which are recorded in a very handsome table in the church, on which are likewise painted the arms of the several benefactors

 

There are about forty poor constantly relieved, and casually twenty.

 

THIS PARISH is within the ECCLESIASTICAL JURISDICTION of the diocese of Canterbury, and deanry of Bridge.

 

The church, which is exempt from the archdeacon, is dedicated to St. Mary. It is a handsome building, consisting of two isles and three chancels, having a slim spire steeple at the west end, in which is a peal of eight bells and a clock. The church consists of two isles and three chancels. The former appear to have been built since the reformation; the latter are much more antient. It is handsome and well built; the pillars between the isles, now cased with wood, are slender and well proportioned. The outside is remarkably beautiful in the flint-work, and the windows throughout it, were regular and handsomely disposed, superior to other churches, till later repairs destroyed their uniformity. The windows were formerly richly ornamented with painted glass, the remains of which are but small. In the south window, in old English letters, is Edward Warham, gentill . . . . of making this window . . . . and underneath the arms of Warham. In the north isle is a brass tablet for Christopher Harris, curate here, and rector of Stourmouth, obt. Nov. 24, 1719. Over the entrance from this isle into the high chancel, is carved on the partition, the Prince of Wales's badge and motto. In the south wall is a circular arch, plain, seemingly over a tomb. A monument for T. Ginder, gent. obt. 1716. In the south east window the arms of Warham. A memorial for Vincent Denne, gent. of Wenderton, obt. 1642. In the high chancel are seven stalls on each side. On the pavement are several stones, robbed of their brasses, over the provosts and religious of the college. A stone, coffin-shaped, and two crosses pomelle, with an inscription round in old French capitals, for master John de Sarestone, rector, ob. XII Kal. May MCCLXXI. Several monuments and memorials for the family of Palmer. The south chancel is called the Dene chancel, belonging to that seat, under which is a vault, in which the family of Oxenden, owners of it, are deposited. In the middle, on the pavement, is a very costly monument, having at the corners four large black oxens beads, in allusion to their name and arms. It was erected in 1682. On the four tablets on the base is an account of the family of Oxenden, beginning with Henry, who built Denehouse, and ending with Dr. Oxenden, dean of the arches, who died in 1704. There are monuments in it likewise for the Trippes. The north chancel is called the Brook chancel, as belonging to that seat, in which are monuments for the Oxendens and Masters's of this seat. This chancel is shut out from the church, and is made use of as a school-room, by which means the monuments are much desaced, and the gravestones, from the filth in it, have become wholly obliterated. On one of these stones was a brass plate, now gone, for Henry Oxenden, esq. who built Dene, obt. 1597.

 

Elizabeth, daughter of the marquis of Juliers, and widow of John, son of Edmund of Woodstock, earl of Kent, after being solemnly veiled a nun, quitted her prosession, and was clandestinely married to Sir Eustace de Danbrichescourt, in a chapel of the mansion-house of Robert de Brome, a canon of this collegiate church, in 1360; for which she and her husband were enjoined different kinds of penance during their lives, which is well worth the reading, for the uncommon superstitious mockery of them. (fn. 9)

 

At the time of the reformation, the church was partly collegiate, and partly parochial. The high chancel, separated from the rest of the church by a partition, served for the members of the college to perform their quire service in. The two isles of the church were for the parishioners, who from thence could hear the quire service; and in the north isle was a roodlost, where one of the vicars went up and read the gospel to the people. At which time, I find mention of a parish chancel likewise.

 

The church of Wingham formerly comprehended not only this parish, but those likewise of Ash, Goodnestone, Nonington, and Wimlingswold; but archbishop Peckham, in 1282, divided them into four distinct parochial churches, and afterwards appropriated them to his new-founded college of Wingham, with a saving to them of certain portions which the vicars of them were accustomed to receive. The profits of this church and the vicarage of it, together with the parsonage-house, being thus appropriated and allotted to the provost, as part of his portion and maintenance, the archbishop, in order that the church should be duly served, by his foundation charter, ordered, that the provost and canons should each of them keep a vicar who should constantly serve in it. In which state it continued till the suppression of the college, in the 1st year of king Edward VI. when it came, among the rest of the revenues of the college, into the hands of the crown, where this parsonage appropriate, to which was annexed, the nomination of the perpetual curate serving in this church, remained till it was granted by king Edward VI. in his 7th year, to Sir Thomas Palmer, bart. Since which it has continued in like manner, together with the scite of the college, as has been already mentioned, to the Rev. Dr. Hey, who is the present possessor of this parsonage, together with the patronage of the perpetual curacy of the church of Wingham.

 

In 1640 the communicants here were three hundred and sixty-one.

 

¶The curacy is endowed with a stipend of twenty pounds per annum, paid by the owner of the parsonage, and reserved to the curate in the original grant of the college by king Edward VI. and with four pounds per annum, being the Oxenden gift before mentioned; besides which, the stipend of the resident curate, and his successors, was increased in 1797, by a liberal benefaction made by the Rev. Dr. Hey, of one hundred pounds per annum, clear of all deductions, to be paid out of the parsonage, and of a house, garden, and piece of pasture land adjoining, for the curate's use, both which were settled by him on trustees for that purpose.

 

www.british-history.ac.uk/survey-kent/vol9/pp224-241

Northumberland Park

Landscape In Tynemouth, Tyne And Wear

 

A traditional Victorian Park packed with features sitting between Tynemouth and North Shields.

 

Situated twixt North Shields and Tynemouth sits Northumberland Park, a traditional Victorian Park positioned in the gently sloping natural dene created by the Pow Burn.

 

The park is 12 hectares in size, but has lots crammed into it including St Leonard's hospital and chapel, sculpture trail, play area, herb garden, BMX track, bowling green, lake, herb garden, a bandstand with regular musical performances and most importantly a tea room!

 

Admission is free and there are plenty of tracks and green spaces to have a quiet saunter and while away an afternoon.

 

The park was created when a local Tynemouth Alderman called John Foster-Spence asked the Duke of Northumberland for some land for the park. The park was to help provide work for unemployed shipbuilders and also create a leisure area for the town. When the work started in 1884, the workmen uncovered the remains of St Leonard's medieval hospital, which was annexed to Tynemouth Priory during the 14th century.

 

The park was opened in August 1885 by the Duke of Northumberland and he planted a Turkey Oak tree which you can still see today.

 

North Shields is a town in the Borough of North Tyneside in Tyne and Wear, England. It is 8 miles (13 km) north-east of Newcastle upon Tyne and borders nearby Wallsend and Tynemouth.

 

Since 1974, it has been in the North Tyneside borough of Tyne and Wear: its historic administration was as part of the Castle ward in county of Northumberland. It was part of the Tynemouth County Borough; when abolished in 1974, the borough became an unparished area.

 

It is on the northern bank of the River Tyne, opposite to South Shields on the other bank. The name derives from Middle English schele meaning "temporary sheds or huts used by fishermen"

 

Earliest records

North Shields is first recorded in 1225, when the Prior of Tynemouth, Germanus, decided to create a fishing port to provide fish for the Priory which was situated on the headland at the mouth of the River Tyne.[5] He also supplied ships anchored near the priory. A number of rudimentary houses or 'shiels' were erected at the mouth of the Pow Burn where the stream enters the Tyne, as well as wooden quays which were used to unload the fishing boats. The quays were also used to ship coal from local collieries owned by the Priory. Soon the population of the new township numbered 1,000. The burgesses of Newcastle upon Tyne were determined to preserve the custom rights that they had enjoyed up till then, which covered the whole length of the river. They successfully petitioned the king in 1290 and managed to suspend trade from the new settlement. It was forbidden to victual ships or to load and unload cargoes at North Shields. The opposition of the Newcastle burgesses remained for a considerable time but despite this, North Shields continued to develop as a centre for fishing and exporting salt, produced at local saltpans. For a considerable period the Newcastle burgesses, known as the Hostmen, who controlled the export of coal from the Tyne, resisted the export of this commodity from North Shields.

 

Geographic development

The town was originated on a narrow strip of land alongside the river (around the present-day Clive Street) because of the steep bank which hemmed it in. Eventually becoming overcrowded, in the 18th century buildings began to be erected on the plateau 60 feet (20 m) above the old insanitary dwellings alongside the river. Prosperous businessmen and shipowners occupied the new town whereas working people remained in the lower part of town. The low, riverside part of the town was linked to the newer, higher part of the town by a series of stairs. These stairs were initially surrounded by slum dwellings, and although the houses have since been cleared the stairs remain.

 

One of the first developments of the new town was Dockwray Square, built in 1763, a set of elegant town houses that was populated by wealthy families. Due to the poor provision of water and drainage facilities, however, the wealthy families soon moved to the more central part of the new town, and particularly the new Northumberland Square. Dockwray Square eventually deteriorated into slums. In the early twentieth century Stan Laurel lived at a house in Dockwray Square for a few years, before he became famous. The square has since been re-developed, initially in the 1960s, and again in the 1990s. A statue of Laurel stands in the middle to commemorate his stay there.

 

The land on which the new town was built was largely owned by the Earl of Carlisle. In 1796, John Wright produced plans that included a grand processional way, now Howard Street, leading to the Georgian Northumberland Square. A railway tunnel, built in the 1840s, left the west and south sides of the square largely unfinished, until a 1960s library building was constructed, somewhat out of keeping with the rest of the architecture. In 1844–45, John Dobson built the town hall, on the corner of Howard and Saville Streets.

 

Geography

The town is bounded to the north by Whitley Bay and to the south by the River Tyne. The town of Tynemouth is to its east and the A19 road marks the boundary between North Shields and Wallsend to the west of the town. It is part of the North Tyneside conurbation.

 

Over the years, North Shields has grown from a small fishing village to incorporate the nearby areas of Chirton, Preston, Billy Mill, Percy Main, East Howdon and Marden estate.

 

The 2011 definition of the town of Tynemouth includes North Shields, which means a population figure can only be given as a combination of wards rather than as a USD.

 

Town Centre

In September 2020, the North Tyneside Council published prospective plans for regeneration of the town centre, which include developing a distinctive route to the Fish Quay, pedestrianisation of key streets, consolidation of retail units, creation of a town square, renovation of Northumberland Square and the establishment of a transport hub. At the time of publication, the plan was not financed and the council sought the views of local residents and business owners.

 

In summer 2020, work was being completed on the refurbishment of the terraced row to the north of Northumberland Square, as well as the development of a newly built row of homes on nearby Albion Road. The newly restored Wooden Dolly was also returned to the Square.

 

A new square, adjacent to Bedford Street, was completed as part of the Transport Hub development in September 2023.

 

Meadow Well

A large council estate, Meadow Well (alternatively spelt Meadowell or Meadowwell on local signs) to the west of the town, was constructed in the 1930s to house residents displaced by the clearance of the Dockwray Square and Low Town slum areas. These flats were replaced with better quality homes in the 1960s and 70s. Meadow Well was formerly known as the Ridges[17] Estate – a name occasionally used today – since it was built on the site of the Ridges farm. Its present name is derived from a well situated in a meadow upon which the estate was built.

 

On Monday, 9 September 1991, Meadow Well was featured heavily in the news across the UK as riots broke out which continued for three days. Many properties were damaged, cars burned out and the local community centre burned down. As a result of the riots, the local housing was gradually improved by the council over the next three years through demolition and rebuilding, as well as renovation. A number of community development organisations, including the Cedarwood Trust, Meadow Well Connected and the Phoenix Detached Youth Project, have worked in the area for many years.

 

The film Dream On (1991) is set on the estate.

 

Following the Meadow Well riots, in July 1992 the Government granted £37.5 million over five years to regenerate that area of the town, as part of the City Challenge scheme.

 

Royal Quays

An extensive regeneration programme costing £16 million saw the revitalisation of the redundant Albert Edward docks. Across an 80 hectare area, the former Tyne and Wear Development Corporation partnered with North Tyneside Council and the private sector to provide a mix of housing, leisure facilities, office space and industrial sites. The Wet N Wild indoor water park, an outlet shopping centre, a bowling alley, a soccer dome and a marina form the centrepiece to the Royal Quays development to the west of the town. Mark di Suvero's Tyne Anew (1999), his only large-scale public artwork in the UK, can be seen at Albert Edward Dock.

 

Fish Quay

Similarly, major regeneration of the Fish Quay, on the riverside to the south-east of the town centre, has included the construction of luxury apartments and the conversion of existing buildings into restaurants and bars alongside the working quay. In November 2018, North Tyneside Council announced plans for further development to enhance the area as a food and drink destination.

 

Smith's Docks

The site of the former Smith's Docks was acquired by the developer Places For People in 2007. In January 2015 they sought planning permission for the construction of homes on the site. The first of those homes, including some designed by George Clarke, was sold in 2017 and as of April 2018, work continues on the site. The second phase, the Smokehouses, was completed in autumn 2018.

 

Heritage Action Zone

Having been awarded £900,000 through the High Street Heritage Action Zone programme, North Tyneside Council plans to add £1 million additional funding to revive the conservation area around Howard Street and Northumberland Square. It will also see work done on the streetscape connecting to the main shopping thoroughfare of Bedford Street in order to better link the areas and decrease the dominance of motor vehicles.

 

Collingwood Grange

In 2017, North Tyneside Council granted planning permission for up to 400 new homes on formerly industrial land to the west of Norham Road. In April 2020, the developer, Miller Homes, announced that work had been halted by the Covid-19 pandemic and that plans may be altered as a result. Work on the development recommenced in January 2021.

 

Industry

Former

In 1887, the town's businesses were listed as a marine engine, chain cable and anchor manufacturer, shipbuilding yards, roperies, salt-works, and an earthenware and stained glass manufacturer. Fishing was also a major industry of employment. The Smith's Dock Company was another major employer for many years, eventually closing in 1987.

 

Shipyards

Shipyards have been in existence in North Shields since near its founding. The smaller yards built the Northumbrian coble, a small inshore fishing vessel with a lug sail, well known in the North East. Larger yards built wooden sailing collier brigs, used to transport local coal to London. Eventually these small yards were replaced by larger yards such as the Tyne Dock and Engineering Company and the Smith's Dock Company. These yards produced iron vessels for various uses, including fishing and the coal trade. In later years the North Shields yards were used for ship repair work, with Smith's dock surviving until the 1990s. None of these yards remain.

 

Oil terminal

Esso formerly had an oil terminal on the banks of the Tyne, off Howdon Road. In April 1994, a bomb planted by the IRA exploded tearing a 3-foot square hole in one of the tanks. A second device, which did not detonate, was later found nearby. Six hundred gallons of crude oil leaked from the tank, but was caught in a channel designed to prevent leakages. A second explosion occurred in June 1994, perpetrated by the same bombers.

 

Maritime

With its fishing industry and shipbuilding history, a number of maritime related companies remain in the town. John Lilley and Gillie Ltd, a marine equipment manufacturer is headquartered there.

 

Mining

Collieries in the town were located at three of the outlying villages since incorporated into the town, at Preston, at the location of the present cemetery gates, Percy Main and New York.

 

Office and business parks

Following the demise of coal mining and shipbuilding in the area, several business parks, industrial estates and trading estates were established providing alternative employment. The biggest of these are The Silverlink and Cobalt Park, the UK's largest office park. Atmel had a plant located at Silverlink, previously occupied by Siemens but the plant is now demolished apart from the office building, now home to Cobalt Business Exchange. Cobalt is home to an Orange call centre. The town's association with the early days of the railways is recognised at the Stephenson Railway Museum on Middle Engine Lane near The Silverlink.

 

Other industries

Potts Print, based in Cramlington since 2006, was originally founded in North Shields in 1875. They occupied various sites in the town over the years.

 

Spicers has a large factory in the town, producing tea. It bought the site from Twinings in 2012.

 

Donald Campbell's Bluebird K7, which crashed during a water speed record attempt on Coniston Water, was restored in a workshop in the town by local engineer Bill Smith.

 

Transport

The Newcastle and North Shields Railway opened in 1839. In 1847, the railway was extended to Tynemouth when a railway station was built in Oxford Street, off Tynemouth Road. Eventually, it was replaced by a new station further away from the river after new rail lines were developed. The riverside tracks were removed for the creation of Hadrian's Way, part of the national cycle network, but the remaining tracks were absorbed in the Tyne and Wear Metro system in 1982. The town centre station, originally constructed for the Newcastle and North Shields Railway, was redeveloped between 1980 and 1982 for the Metro. It was subsequently refurbished in 2012. The Tyne and Wear Metro links North Shields to Newcastle city centre, and to other destinations in Tyne and Wear including Whitley Bay, Newcastle Airport and Sunderland. The town is also served by stations in Percy Main and Meadow Well.

 

The Tyneside Tramways and Tramroads Company also operated an electric tramway service in the town.

 

Shipping

Local ferry

A half-hourly ferry service connects North Shields to the town of South Shields on the opposite bank of the Tyne. The present Shields Ferry was established in 1972. Its first female skipper was appointed in 2016. Shieldsman, a former ferry retired in 2007, has since been moved to Shoreham, West Sussex, and transformed into a houseboat.

 

From June to October, river trips by ferry operate.

 

In November 2018, the local council announced plans to consider the feasibility of moving the ferry landing. In July 2021 it was announced that the planned relocation was delayed until 2023.

 

International ferry

From the International Ferry Terminal, based at Royal Quays, the Danish company DFDS Seaways operates a daily service to IJmuiden.

 

The ferry service to Gothenburg, Sweden (run by DFDS Seaways), ceased operation at the end of October 2006. DFDS Seaways' sister company, DFDS Tor Line, continues to run scheduled freight ships between Gothenburg and several English ports, including Newcastle, but these have limited capacity for passengers and do not carry private vehicles.

 

Port of Tyne International Passenger Terminal

The passenger terminal regularly welcomes tourists travelling on cruises that call at North Shields as an access point for Newcastle upon Tyne and the wider North East of England. In 2017, 52 ships docked, bringing 120,000 visitors to the region. A number of "dudes" - red and blue powder coated figures designed by artist Perminder Kaur - can be seen on a grassy mound at the entrance to the terminal.

 

Culture

In 2009, seating inspired by Plasticine, the inventor of which was born in North Shields, was installed on Bedford Street in the town centre. The seats proved unpopular as their shape prevented rainwater draining off, so they were replaced by more traditional metal benches and moved to the Royal Quays Marina in 2011.

 

YMCA

YMCA North Tyneside was founded in 1870 and was originally known as The Borough of Tynemouth YMCA. After an inaugural meeting on 7 June 1879, weekly meetings followed in the Sons of Temperance Hall, Norfolk Street, North Shields. The YMCA grew in popularity. Within a year, larger premises were needed. Meetings moved to 53 Tyne Street, North Shields and in 1879 to Camden Street, North Shields. In 1920 the YMCA moved to a building in Bedford Street (which is still owned by the YMCA and now occupied by the Citizens Advice Bureau) where it remained until 1938, when it moved to the present building and the current registered office at Church Way, North Shields.

 

Fish Quay Festival

Between 1987 and 2001, a community festival was organised on the fish quay, during which the fleet of fishing boats would be blessed and various local talents would entertain the crowds. At its peak, the festival attracted 600,000 visitors. A smaller-scale family festival, in order to save costs, was held annually between 2002 and 2006, before it too was scrapped as a money-saving measure.

 

Retail

Town Centre

A significant part of the town centre is pedestrianised and it is dominated by the Beacon, a partly-covered shopping mall which was constructed in the late 1970s and originally named The Bedford Centre.

 

As with many British high streets, a number of large chains have closed their branches in the town in recent years, including Littlewoods, Woolworths and McDonald's. As of 2019, Wilko has a large store in the Beacon, alongside high street regulars such as Specsavers, Superdrug and Boots. A number of discount retailers including B & M, Home Bargains, Peacocks and Heron Foods have branches in the town centre, as well as numerous charity stores.

 

Greggs, Cooplands, and Costa Coffee have outlets. Charities YMCA North Tyneside, Age UK and Operation Veteran both have independent coffee shops. Barista Boho, opened in 2022 in the former Alnwick Castle public house, also serves local coffee blends and hosts musicians. There are numerous independent butchers in the town centre, as well as a local independent bakery, Canatrice, located nearby.

 

Asda acquired a former Netto store in the town centre in 2011. The Co-op has a number of branches in the town, including convenience stores in Tynemouth and Preston. Morrisons also has a large store in Preston.

 

Other shopping centres

There are three further shopping centres in the town, as well as parades of shops in Balkwell, Preston and Chirton.

 

The Royal Quays Outlet Centre is home to a number of discount stores including outlets for Next, Clarks and Mountain Warehouse, as well as independent retailers such as a photographic studio and pet shop. The closures of a Marks & Spencer Outlet and, in late 2019, the Nike store have somewhat diminished the centre. In January 2020, Thorntons posted notices announcing the closure of their shop and coffee shop. Costa Coffee, The Body Shop, Cotton Traders, Dreams, Edinburgh Woollen Mill, Moss, Tog 24, Trespass and Poundland also had branches in early 2020. In April 2023, it was reported that the centre's owners had appointed receivers who were advertising it for sale as a going concern. It remains open as usual.

 

The Coast Road Retail Park is adjacent to a large Tesco supermarket and, as of 2020, home to Dunelm, B & M, Pets at Home, Carpetright and The Food Warehouse stores.

 

The Silverlink Shopping Park, as of 2020, includes branches of Boots, Next, H&M, Halfords, Marks and Spencer and River Island. In September 2016, a large expansion of the retail park opened. Odeon also has a multi-screen cinema at the park, alongside restaurants.

 

Business

Over 100 businesses in the town are members of The North Shields Chamber of Trade and Commerce.

 

The Mercantile Building Society, established in the town and formerly headquartered at the Silverlink Business Park, merged with the Leeds Building Society in 2006.

 

Recreation

In 2000, the local authority established more than 30 miles (48 km) of walking routes, primarily following the paths of 19th-century waggonways. A Tynemouth walk begins from the Metro station in the town centre and drops down on to the fish quay before following a route to Tynemouth, while the Royal Quays walk begins from the Meadowell Metro station and completes a route around the redeveloped riverside area including the marina, before ending at Percy Main Metro station.

 

Sport

The town is home to the non-League football club North Shields F.C. Founded in 1896, the team competes in Northern Football League and plays home games at Daren Persson Stadium (formerly Ralph Gardner Park). The team has twice played at Wembley Stadium, winning 2–1 on both occasions: against Sutton United on 12 April 1969 at the old Wembley to win the FA Amateur Cup and against Glossop North End at the new stadium on 9 May 2015 to win the FA Vase, the Amateur Cup's successor. The stadium is presently named as such because of a sponsorship by a local funeral director.

 

Leisure facilities

The Parks Sports Centre was opened in 1998, after the construction of the Royal Quays. It has a large sports hall, gym, multi-sensory room, outdoor football pitches, indoor and outdoor bowls facilities and a cafe.

 

Royal Quays facilities

The Wet'n'Wild indoor water park was constructed in 1992 and opened in summer 1993 as part of the Royal Quays development. It was originally designed with rides: six speed slides, five conventional flumes and one "lazy river" ride. The "Twister", a speed slide, was 85 metres (279 ft) long, and started from a height of 12.5 metres (41 ft). It closed in 2013 after its owner entered administration, but was reopened in 2014, having been bought by another company. In 2020, the owner announced that it would not reopen after the winter, citing financial losses due to poor visitor numbers.

 

A bowling alley, originally Star Bowl, also forms part of the development. In 2019, having been closed for some time, it was reopened as Gutterball.

 

A trampoline park, Xtreme Bounce, was opened in 2017 in an air-locked dome in the outlet centre's car park. In 2019, the Inflatanation chain took over the site and reopened the venue with inflatables replacing the trampolines.

 

In 2019, a leisure hub housed in the health and fitness section of the former JJB Soccerdome adjacent to the outlet centre, was announced. Everyone Entertained was to feature climbing walls, soft play, laser tag and adventure golf, and employ 100 people. As of May 2020, the venue remains unopened. The pitches and bar were reopened as The Evolution Football Centre in autumn 2018. In early 2020, it was announced that the centre was to close having proved financially nonviable.

 

Parks

There are a number of parks and play areas in the town.

Northumberland Park lies on the border of North Shields and Tynemouth and was set out around 1885, in an area formerly known as Spittal Dene. In 2015, North Tyneside Council completed a major project to revive and restore parts of the park. The multi-million pound scheme saw archaeological investigations carried out around the medieval St Leonard's Hospital and the restoration historical features that had been lost over the years. Iron railings, park furniture, fountains were installed amid historic planting schemes. A pavilion housing a cafe and toilet facilities as well as offices and storage for the park staff was also opened.

 

There is a children's play area at the south end of the park, bowling greens on the western border and a historical pet cemetery to the north. A number of trees along a pathway in the northern half feature plaques commemorating their planting by various local dignitaries.

 

West End Park and Linear Park, Chirton Dene

West End Park lies adjacent to The Parks sports centre and was laid out prior to the 1940s. To its south, Linear Park runs down to the Royal Quays Marina and was created as part of the Royal Quays development in the mid-1990s.

 

Redburn Dene

As with Linear Park, Redburn Dene was created as part of the 1990s redevelopment of former industrial and dockland areas, following a natural water course. It features sculptures made from reclaimed staithes. The park was given a Green Flag award in 2020.

 

Culture

Art

Fiddler's Green, a steel sculpture that serves as a memorial to fishermen lost at sea, was unveiled in 2017.

 

A number of pieces were installed as part of the Royal Quays development. Located in Chirton Dene, Redburn Dene, by the marina, and near the shopping outlet, they include works by Richard Broderick, Graham Robinson, Linda France, Alec Peever, Gilly Rogers, Mark di Suvero, Perminder Kaur and Andy Plant.

 

In film

Dream On (1991) was produced by Amber Films and filmed on location in Meadow Well. Its original release was around the time of the Meadow Well riots.

 

On television

The BBC series When the Boat Comes In, though set in the fictional Gallowshield, was essentially set in North Shields and filmed on location around the town. Various episodes of the series Spender, which starred Jimmy Nail, and Vera, with Brenda Blethyn, were also filmed there.

 

In songs

Sweden's foremost troubadour of the 20th century, Evert Taube, wrote the song "Mary Strand", which is set in North Shields in 1909. Mary Strand is the proprietress of the cigar shop Tiger Brand on Dock Street and hides a young sailor from the police. The song is based on Taube's own experience, when he ran away from the steamship Australic in Newcastle upon Tyne.

 

Twin town

In 2017, the town was twinned with Merthyr Tydfil, in Wales, as part of the Carnegie Twin Towns Project. The project aimed to pair towns that had similar characteristics, and socio-economic challenges, in order to consider how they might make positive changes to their communities.

 

Landmarks

Lights of North Shields

Because of the difficulty of navigating ships into the mouth of the river past the dangerous Black Midden rocks, buildings were erected in the 16th century with permanent lights burning to be used as a guide by the mariners. High and Low lights are pictured on a 1655 map of the river Tyne: a pair of square castellated towers. Both lights were rebuilt in 1727, and these buildings still stand today (albeit the Old Low Light was remodelled in 1830 to serve as an almshouse). In 1810, the Old Lights were replaced by new High and Low Lights, placed respectively at the top and bottom of the steep bank alongside the river. All these lights were owned and operated by Trinity House of Newcastle-upon-Tyne until they ceased operation. Today, the Old High Beacon, as well as the High and Low Lights, are private residences; they remain prominent landmarks. In 2014 the black-painted Old Low Light was opened to the public following a substantial refurbishment; it contains a café, shop, museum, viewing platform and event space.

 

Fish Quay

In 1806, a market place was opened on New Quay. In 1870, work began on constructing a fish quay to provide shelter for the docked fishing boats. This quay is still in use today. In 2017, a sculpture by artist Ray Lonsdale of a lone fisherman – made of corten steel and weighing over 2 tonnes – was installed on the quay.

 

Clifford's Fort

Clifford's Fort, located on the Fish Quay, was built in the 17th century as a coastal defence against the Dutch. The Fort was active during the Napoleonic Wars and played a significant role during World War I, being the birthplace of the Tyne Electrical Engineers. The fort was officially evacuated by the military in May 1928, sold to the Tynemouth Corporation, and redeveloped as new fish processing facilities.[161] Very little now remains of the original fort buildings, though the walls are intact. The area has undergone considerable restoration, with most of the fish processing units demolished. The remaining excellent modern retail units are very popular. During restoration work, part of the foundations of the 18th century Master Gunner's House (demolished in 1973) were found below the concrete floor of a fish processing unit. Elsewhere on the site, part of the stone edging of Cable Tanks belonging to the Submarine Mining Depot, established at the fort in 1888, was uncovered. The gun embrasures have been revealed, the ground resurfaced, and there are some traffic restrictions. The Old Low Light, built in 1735 and Grade II-listed, within Clifford’s Fort, has been restored and operates as a Heritage Centre, café, and community space.

 

Wooden Dolly

One of North Shields' oldest landmarks is the "Wooden Dolly" statue. In 1814, the female figurehead of a collier brig was placed at the entrance to Custom House Quay, on Liddell Street, and stood there until 1850, when it was vandalised. A second figurehead was placed on the same spot. The "Wooden Dolly", as the figurehead was known, was used by seafarers as a source of good-luck charms, by cutting pieces of wood from her to be taken with them on voyages. Eventually the figurehead was defaced beyond repair and after 14 years was replaced by Wooden Dolly No. 3. This remained until 1901 when it was replaced with Wooden Dolly No. 4 in the shape of a fishwife. A fifth Wooden Dolly, also a fishwife, was placed in Northumberland Square in 1958 and was removed for restoration in December 2019. Once restoration has been completed it will be placed in the Library and a replacement figure installed in the square. In 1992, a sixth Wooden Dolly was placed where the first four had been, at the entrance to Custom House Quay, and can still be seen there, next to the Prince of Wales public house.

Yamzzi of GENG at the 2026 VALORANT Game Changers Championship Features Day in São Paulo, Brazil on October 20, 2026. (Photo by Heaven Wolf/Riot Games)

Collection:

Images from the History of Medicine (IHM)

 

Author(s):

Haeckel, Ernst Heinrich Philipp August, 1834-1919, author

 

Publication:

Berlin: Reimer, 1870

 

Language(s):

German

 

Format:

Still image

 

Genre(s):

Book Illustrations

 

Abstract:

A series of heads that progressively develop anthropomorphic features.

 

Related Title(s):

Is part of: Naturliche Schopfungsgeschichte, pl. XIII.; See related catalog record: 60830080R

 

Extent:

1 print

 

Technique:

lithograph

 

NLM Unique ID: 101449208

 

NLM Image ID: A030210

 

Permanent Link:

resource.nlm.nih.gov/101449208

The main geographic features of Rajasthan are the Thar Desert and the Aravalli Range, which runs through the state from southwest to northeast, almost from one end to the other, for more than 850 km. Mount Abu is at the southwestern end of the range, separated from the main ranges by the West Banas River, although a series of broken ridges continues into Haryana in the direction of Delhi where it can be seen as outcrops in the form of the Raisina Hill and the ridges farther north. About three-fifths of Rajasthan lies northwest of the Aravallis, leaving two-fifths on the east and south.

 

The northwestern portion of Rajasthan is generally sandy and dry. Most of the region is covered by the Thar Desert, which extends into adjoining portions of Pakistan. The Aravalli Range does not intercept the moisture-giving southwest monsoon winds off the Arabian Sea, as it lies in a direction parallel to that of the coming monsoon winds, leaving the northwestern region in a rain shadow. The Thar Desert is thinly populated; the town of Bikaner is the largest city in the desert. The Northwestern thorn scrub forests lie in a band around the Thar Desert, between the desert and the Aravallis. This region receives less than 400 mm of rain in an average year. Temperatures can exceed 45 °C in the summer months and drop below freezing in the winter. The Godwar, Marwar, and Shekhawati regions lie in the thorn scrub forest zone, along with the city of Jodhpur. The Luni River and its tributaries are the major river system of Godwar and Marwar regions, draining the western slopes of the Aravallis and emptying southwest into the great Rann of Kutch wetland in neighboring Gujarat. This river is saline in the lower reaches and remains potable only up to Balotara in Barmer district. The Ghaggar River, which originates in Haryana, is an intermittent stream that disappears into the sands of the Thar Desert in the northern corner of the state and is seen as a remnant of the primitive Saraswati river.

 

The Aravalli Range and the lands to the east and southeast of the range are generally more fertile and better watered. This region is home to the Kathiarbar-Gir dry deciduous forests ecoregion, with tropical dry broadleaf forests that include teak, Acacia, and other trees. The hilly Vagad region lies in southernmost Rajasthan, on the border with Gujarat. With the exception of Mount Abu, Vagad is the wettest region in Rajasthan, and the most heavily forested. North of Vagad lies the Mewar region, home to the cities of Udaipur and Chittaurgarh. The Hadoti region lies to the southeast, on the border with Madhya Pradesh. North of Hadoti and Mewar is the Dhundhar region, home to the state capital of Jaipur. Mewat, the easternmost region of Rajasthan, borders Haryana and Uttar Pradesh. Eastern and southeastern Rajasthan is drained by the Banas and Chambal rivers, tributaries of the Ganges.

 

The Aravali Range runs across the state from the southwest peak Guru Shikhar (Mount Abu), which is 1,722 m in height, to Khetri in the northeast. This divides the state into 60% in the northwest of the range and 40% in the southeast. The northwest tract is sandy and unproductive with little water but improves gradually from desert land in the far west and northwest to comparatively fertile and habitable land towards the east. The area includes the Thar Desert. The south-eastern area, higher in elevation (100 to 350 m above sea level) and more fertile, has a very diversified topography. in the south lies the hilly tract of Mewar. In the southeast, a large area within the districts of Kota and Bundi forms a tableland. To the northeast of these districts is a rugged region (badlands) following the line of the

 

SAN FRANCISCO, CALIFORNIA - NOVEMBER 01: Hwang "Kingen" Seong-hoon of DRX poses at the League of Legends World Championship Finals Features Day on November 1, 2022 in San Francisco, CA. (Photo by Lance Skundrich/Riot Games)

Features: Custom waterslide decals, weapon and Kama. Please visit www.minifigmaker.com for more info.

ATLANTA, GEORGIA - OCTOBER 26: Han "Peanut" Wang-ho (L) and Jeong "Chovy" Ji-hoon of Gen.G pose at the League of Legends World Championship Semifinals Features Day on October 26, 2022 in Atlanta, GA. (Photo by Fernando Decillis/Riot Games)

Geeks on the web tend to gravitate to elaborate lists to break down competing gadgets. In the case of Apple, they usually break out a list that features a lot of what's missing from a Apple product, without mentioning what's missing from a competing product.

 

For instance, I've seen many lists that compare the Nexus One to the iPhone. While the lists always seem to mention the fact that the iPhone doesn't have multi-tasking (for third party apps) they seem to omit the fact that the Nexus One doesn't have a good native music app or support Multi-touch for native apps. And if you bring up the Multi-touch flaw, the Android Fanboys will argue that you can get Multi-touch for third party apps, which to them, makes the point irrelevant. Of course, I invariably counter with the fact that the iPhone does have multi-tasking for NATIVE APPS, the logic being that if you're going to omit one flaw for the Nexus One based on a technicality, then you got to do the same for multi-tasking on the iPhone. Fair is fair.

 

But I digress. I present the 10 Reasons to buy an iPad. To prove that I'm not a total Fanboy (even though I am), I've included 5 things missing from the current iPad.

  

10 Reasons to buy the iPad.

 

1) 3G. The 3G plan is great. $15 for a plan with a 250 MB cap or $30 for unlimited. The iPad comes with a built-in mic and headphone jack, which means you can connect the default headphones that feature the mic that people use to make Skype calls on the iPod Touch. That means the iPad can replace my cell phone and unlike the iPod Touch, I can use it anywhere, not just in places that have Wi-Fi.

 

2) The Mac-Like Apps. The default apps on the iPad are actually more like Mac apps, but optimized for Multi-touch. I've watched several videos of people using the iPad and the apps are more fully featured than the ones on the iPhone or iPod Touch. The apps in iWork would have never worked on an iPhone for instance. The iPad apps have new features like Popovers and Split Views, which again, take advantage of the larger screen real estate. The faster processor speed means more robust apps. Maybe the iPad won't be able to run the 2009 version of Photoshop, but it definitely will be able to run something equivalent to the 2001 version of Photoshop. This is huge and will create a variety of apps that are a vast improvement over the current apps available in the App Store, to say nothing of the fully featured games that will now come out for the iPad.

 

3) The App Store. There are 140,000 apps available from the start. You don't have to wait for apps, like say, the people who are waiting for stuff to come out on Android. And the SDK has already been released, which means many developers will have enhanced their apps specifically for the iPad before it even launches.

 

4) The Bigger Screen. Multi-touch is going to be much easier to manage on the iPad than on a little screen. The reading is going to be much easier than an iPhone screen. You don't have to pinch to enlarge as often on the iPad screen.

 

5) Video. Because of the bigger screen, the movies and video will be desktop resolution. Also, one of the less talked about features are the external speakers. Assuming you use the dock or a third party stand, the external speakers will allow you to watch video or movies like you would a regular TV.

 

6) The Battery Life. The battery is 10 hours for constant use, with 30 DAYS of standby time. That's good enough for me. I don't plan on reading e-books more than 10 hours. Maybe 5, tops. Steve Jobs made a similar comment the day of the iPad Keynote to Walt Mossberg, saying in effect that no one would be reading for more than 10 hours, which for some reason enraged a lot of people. My question, who are these people who have more than 10 hours of time to read? What kind of jobs do you people have? Please send me an e-mail and let me know where to sign up.

 

7) The Weight. The iPad's weight is much better than a Laptop. If I got to bolt from the house for a few minutes, maybe wait in line at the post office, I would much rather have an iPad with me. A laptop is just not feasible in situations where you're waiting in line somewhere with nothing to rest the laptop on and the availability of iWork on the iPad means that I'll actually be able to do some real work.

 

8) The iPhone OS. Because Apple decided to use the iPhone OS instead of the Mac OS, we actually have a large selection of games, which means the iPad is the largest portable gaming device on the market. The iPhone OS also happens to be so simple to use that babies have been given the device and were able to figure it out, but now we have that same easy to use OS on an oversized device. This will be huge for people who are scared of computers. Apple is ushering in a new era of computer as appliance. It doesn't surprise me in the least that geeks don't quite get it yet (or maybe they DO get it and are angry that their technical support won't be needed any longer).

 

9) The Price. The price is essentially the same as the iPhone three years ago, but the features are bigger and more robust than the iPhone.

 

10) No Flash. Unlike many geeks, the option for no flash is actually a selling point for me. If the iPad were to become an unqualified hit, it would signal the death knell for Flash, especially if the iPad became THE default device for the mobile web, much like the iPhone and iPod touch are becoming that now. It only takes a couple of major companies saying no to a standard to kill it in its tracks. This is a major reason why Microsoft never got a major foothold on standards governing the internet. Apple's banning of WMA and WMV file formats from iTunes caused their marginalization in the market. Sure, those formats are still around, but they don't dominate like MP3 and AAC.

 

twitpic.com/10fjic

  

5 Things I would like to see in future iPads.

 

1) A TV Tuner. For the life of me, I can't understand why Apple doesn't have TV Tuners in all their Macs. I've managed to solve this omission on my iMac by buying a TV Tuner from Elgato, the makers of the popular EyeTV software, but come on Apple, this would make the iPad an alternative TV! This would be the start of something very huge. I'm not advocating that the TV Tuner be integrated into the iPad itself, because TV Tuners need either bulky digital antennas or to be connected to coax cable to work properly and that obviously won't work for a mobile device, but if the tuner could be integrated into that dock that allows the iPad to be free standing, I could set this iPad on my entertainment center and stream TV signals. The iPad is just screaming for this!

 

2) A Camera. Although I consider myself a geek by a wide margin, I am fairly enlightened when it comes to the desires of the ordinary consumer (which is why I want a TV Tuner for this thing), but you just can't have modern gadgets without slapping on a camera somewhere. It's just not permitted. Of course, I would be remiss to forget all the tech analysts who said that the original iPhone wouldn't be good for Enterprise because it featured a camera, which are banned by plenty of corporations. I'm quite sure a lot of those same dicks are currently bashing the iPad for not having a camera. Of course, the iPad is being marketed as a consumer level device, so I might have to agree with them here. The iPad should have a camera, just to shut the dirty masses up.

 

3) Multi-tasking. Even though I don't think most regular consumers are even aware that the current iPhone and iPod Touches don't feature multi-tasking, except for native apps, I still think it would be nice if we just had the OPTION for multi-tasking for third party apps. Heck, Apple, turn off multi-tasking by default, code in a pop-up that warns me of the decreased battery life and the consequences for performance for enabling multi-tasking, but for the love of God, GIVE ME A CHOICE. I would be satisfied with the ability to run only three apps at a time. I'm not asking for much.

 

4) A full iTunes client. Apple provided a blazing fast processor for the iPad and ported versions of desktop apps like Pages, Keynote and Numbers to the iPad, but they can't port the desktop version of iTunes? What gives! With the iPad's big screen, I should be able to manage my music, I shouldn't have to tether it to a desktop. If Steve Jobs truly wants the iPad to kill netbooks, it's going to have to be in some ways as robust as a netbook. The upgrades of the native iPhone apps and the addition of iWork are steps in the right direction, but I believe iTunes is even more important.

 

5) One USB slot. I've got my geek hat on now, and the geek inside tells me that a USB slot would be good for stuff like file transfer, you know, adding a little external flash drive and moving stuff like pictures from digital cameras. Theoretically, Bluetooth will suffice for printing and other functions, but USB comes with the added bonus of shutting up all the other annoying geeks who HAVE to have a USB connector for some reason (If you think I'm just adding a USB slot to fill out my list with five items, because four would be awkward, you're probably right).

 

For those of you shaking with anger that your unicorn wishes for the iPad didn't pan out, maybe you need to relax and watch the wisdom of Louis C.K., you spoiled brats.

 

www.youtube.com/watch?v=UN0MpBQG3-E

 

Universal Studios Florida is a theme park located in Orlando, Florida. Opened on June 7, 1990, the park's theme is the entertainment industry, in particular movies and television. Universal Studios Florida inspires its guests to "ride the movies", and it features numerous attractions and live shows. The park is one component of the larger Universal Orlando Resort.

 

In 2013, the park hosted an estimated 7.06 million guests, ranking it the eighth-most visited theme park in the United States, and ranking it sixteenth worldwide.[2]

  

Contents [hide]

1 History 1.1 Park history

1.2 Branding

1.3 Timeline

1.4 Previous attractions

 

2 Park design 2.1 Production Central

2.2 New York

2.3 San Francisco

2.4 London/Diagon Alley

2.5 World Expo

2.6 Woody Woodpecker's Kidzone

2.7 Hollywood

 

3 Character appearances

4 Production facilities

5 Annual events 5.1 Grad Bash and Gradventure

5.2 Halloween Horror Nights

5.3 Macy's Holiday Parade

5.4 Mardi Gras

5.5 Rock the Universe

5.6 Summer Concert Series

 

6 Universal's Express Pass

7 Attendance

8 See also

9 References

10 External links

  

History[edit]

  

This section needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. (August 2010)

     

The original entrance to the theme park.

Over the years, Universal Studios Florida has not limited itself to attractions based on its own vast film library. It has occasionally licensed popular characters from other rival studios, many of whom did not operate theme parks themselves. Some examples include Ghostbusters and Men in Black, (Sony's Columbia Pictures), The Simpsons (20th Century Fox) and Shrek (DreamWorks Animation).

 

Many of the park's past and present attractions were developed with the actual creators of the films they were based on, and feature the original stars as part of the experience. Steven Spielberg helped create E.T. Adventure and was a creative consultant for Back to the Future: The Ride, Twister...Ride it Out, An American Tail Theatre, Jaws, Men in Black: Alien Attack and Transformers: The Ride.

 

In many current rides, the original stars reprised their film roles including: Rip Torn and Will Smith in Men in Black: Alien Attack, Brendan Fraser for Revenge of the Mummy: The Ride, Bill Paxton and Helen Hunt in Twister...Ride it Out, Arnold Schwarzenegger, Edward Furlong and Linda Hamilton reprised their roles for Terminator 2: 3-D Battle Across Time, Mike Myers, Eddie Murphy, Cameron Diaz, and John Lithgow for Shrek 4D, Steve Carell, Miranda Cosgrove, Dana Gaier, and Elsie Fisher reprised their roles from Despicable Me for Despicable Me: Minion Mayhem, and Peter Cullen and Frank Welker reprised their roles as Optimus Prime and Megatron for Transformers: The Ride.

 

In many former rides, the many original stars were also to reprise their film roles such as: Christopher Lloyd and Thomas F. Wilson in Back to the Future: The Ride, Roy Scheider recorded a voice over for the conclusion of Jaws, Alfred Hitchcock and Anthony Perkins appeared in Alfred Hitchcock: The Art of Making Movies, additionally, various Nicktoon voice actors reprised their roles in Jimmy Neutron's Nicktoon Blast.

 

Park history[edit]

 

From its inception in 1982,[3] Universal Studios Florida was designed as a theme park and a working studio. It was also the first time that Universal Studios had constructed an amusement park "from the ground up." However, the proposed project was put on hold until 1986, when a meeting between Steven Spielberg, a co-founder for the park, and Peter N. Alexander prompted for the creation of a Back to the Future simulator ride in addition to the already planned King Kong based ride.[4]

 

A major component of the original park in Hollywood is its studio tour, which featured several special-effects exhibits and encounters built into the tour, such as an attack by the great white shark from the film Jaws. For its Florida park, Universal Studios took the concepts of the Hollywood tour scenes and developed them into larger, stand-alone attractions. As an example, in Hollywood, the studio tour trams travel close to a shoreline and are "attacked" by Jaws before they travel to the next part of the tour. In Florida, guests entered the "Jaws" attraction and would board a boat touring the fictitious Amity Harbor, where they encountered the shark, then exited back into the park at the conclusion of the attraction. Universal Studios Florida originally had a Studio Tour attraction that visited the production facilities, but that tour has since been discontinued.

 

Branding[edit]

 

Previous slogans for Universal Studios Florida were: See the Stars. Ride the Movies. (1990 - 1998); No one makes believe like we do! (1990 - 1998); Ride the Movies (1998 - 2008); Jump into the Action (2008–2012). The current slogan is: Experience the Movies (2012–present).

 

Timeline[edit]

1986: Land clearing takes place on the swamp land purchased by MCA/Universal that would hold the park.

1987: Universal Studios Florida is announced at a press conference on the Hollywood property, with a planned opening date of December 1989.

1988: Universal Studios Florida's opening date is delayed from December, 1989 to May 1, 1990. Shortly following, MCA/Universal releases a video detailing the future park, which stars Christopher Lloyd as the Universal character Doc Brown interacting with the various attractions at the Florida park.[5] Universal Studios allows guests to witness the production of television shows and motion pictures in the Florida park's soundstages in middle 1988, while the rest of the studio/park is still under construction.[6]

1989: MCA/Universal Studios claims that The Walt Disney Company and its CEO, Michael Eisner copied several concepts of the Universal Studios Florida park, and integrated them into Disney's recently opened Disney/MGM Studios park.[7]

1990: On January 31, Universal Studios Florida's opening date is again delayed from May 1, 1990 to June 7, 1990.[8] Universal Studios Florida begins soft openings for the general public in late May.[9] Many of the park's attractions are not yet open at the time, and still under testing. Universal Studios Florida is officially opened with a grand opening style ceremony on June 7.[10] The park opens with five themed areas: The Front Lot (entrance area), Production Central, New York, San Francisco/Amity, Expo Center, Hollywood as well as a Lagoon located in the center of the park. The Front Lot and Production Central areas are referred to as "In Production", the New York section is referred to as "Now Shooting", the San Francisco and Amity sections are referred to as "On Location" and the Expo Center area is referred to as "The World of CineMagic Center". Nickelodeon Studios also opened on this day where there was a grand opening ceremony hosted by Marc Summers. Due to massive technical problems with the original Kongfrontation, Earthquake: The Big One and Jaws rides, Universal begins a temporary voucher service to allow guests to re-visit the studio/park when the attractions are operating.[10] Jaws is temporarily closed by Universal on September 30 due to persistent major technical problems. During the shut-down, Universal sues the original designer of the Jaws ride,[11] Ride & Show Engineering, and hires Totally Fun Company to create a re-designed version of most of the ride.

1991: Universal adds four new attractions to the park: The Blues Brothers Show, StreetBusters, The Screen Test Home Video Adventure and How to Make a Mega Movie Deal.[12] Back to the Future: The Ride officially opens in the World Expo Center area of the park, in a grand opening ceremony.[13] The ride is considered to be a success, and receives positive reception from theme park critics.[14] Fright Nights debuts at the park. In 1992, it is renamed to Halloween Horror Nights.

1993: Jaws is re-opened, with many scenes altered. MCA/Universal announces plans to expand Universal Studios Florida into the Universal City, Florida resort complex, including a second theme park and multiple hotels.[15]

1995: Universal Studios Florida celebrates its 5th anniversary. A Day in the Park with Barney opens in the World Expo area. The Production Studio Tour is closed due to a dwindle in the studios' recent Film/TV production.

1996: Terminator 2: 3-D Battle Across Time opens in the Hollywood area.[16]

1997: Universal announces that Ghostbusters Spooktacular will be replaced by Twister...Ride it Out, with a planned opening date of Spring 1998[17] Universal Studios announces that the sole Studio park will be expanded into the Universal Studios Escape, including the Islands of Adventure park, Universal CityWalk Orlando and multiple hotels. The Islands of Adventure Preview Center opens in the New York area, replacing The Screen Test Home Video Adventure. It is meant to give guests a preview of the up-coming Islands of Adventure park, as well as expansion of the Studio park into the Universal Studios Escape resort.

1998: The expansion begins as the original open parking lot for Universal Studios Florida is demolished and replaced by CityWalk and a parking garage complex.[18] Universal delays the opening of Twister...Ride it Out from March, 1998 to May 4, 1998 out of respect for the 42 deaths caused by a recent El Nino outbreak of tornadoes in the central Florida area. Twister...Ride it Out opens in the New York area, replacing Ghostbusters Spooktacular.[19] A new area of the park, Woody Woodpecker's Kidzone, is officially opened, holding the attractions Curious George Goes to Town, StarToons and the previously opened Fievel's Playland, E.T. Adventure, Animal Actors Stage and A Day in the Park with Barney; CityWalk opens outside of the park.

1999: Woody Woodpecker's Nuthouse Coaster opens in the Woody Woodpecker's Kidzone area. Islands of Adventure opens next door to Universal Studios Florida.[20]

2000: Men in Black: Alien Attack opens in the World Expo area, on the former site of The Swamp Thing Set. Universal Studios Florida's 10th anniversary celebration.

2001: Animal Planet Live opens, replacing Animal Actors Stage.

2002: Universal Studios Escape is renamed Universal Orlando Resort. Kongfrontation closes in a closing ceremony. Halloween Horror Nights is moved to Islands of Adventure. Macy's Holiday Parade debuts at the park.

2003: Jimmy Neutron's Nicktoon Blast opens, replacing The Funtastic World of Hanna-Barbera.[21] Shrek 4-D opens with Donkey's Photo Finish, replacing Alfred Hitchcock: The Art of Making Movies and Stage 54 respectively.[22]

2004: Revenge of the Mummy: The Ride opens, replacing Kongfrontation.[23] Halloween Horror Nights takes place in both Universal Studios Florida and Islands of Adventure.

2005: Universal Express Plus is introduced, replacing Universal Express. Nickelodeon Studios closes after nearly 15 years. Fear Factor Live opens, replacing The Wild Wild Wild West Stunt Show. Universal Studios Florida celebrates its 15th anniversary.

2006: Delancey Street Preview Center opens in the New York area. Universal 360: A Cinesphere Spectacular opens, replacing Dynamite Nights Stunt Spectacular. Animal Planet Live is closed, and replaced by Animal Actors on Location. Halloween Horror Nights returns to Universal Studios Florida for its "Sweet 16".

2007: Back to the Future: The Ride closes on March 30.[24] Blue Man Group Sharp Aquos Theatre opens in CityWalk, replacing Nickelodeon Studios. Earthquake: The Big One closes in the San Francisco area on November 5.

2008: Disaster!: A Major Motion Picture Ride...Starring You! opens, replacing Earthquake: The Big One.[25] Universal announces Hollywood Rip Ride Rockit, with a planned opening of Spring 2009. The Simpsons Ride opens, replacing Back to the Future: The Ride.[26]

2009: The Universal Music Plaza Stage opens, replacing The Boneyard. Hollywood Rip Ride Rockit opens.

2010: The 20th anniversary of Universal Studios Florida in June, as well as Halloween Horror Nights in October.

2011: The 10th anniversary of Macy's Holiday Parade at the park.[27]

2012: Jaws and the surrounding Amity themed area closes, as announced on December 2, 2011.[28] Universal announces the additions of Universal’s Cinematic Spectacular: 100 Years of Movie Memories and Universal's Superstar Parade to the park, with openings on May 8, 2012.[29] Despicable Me: Minion Mayhem, opens replacing Jimmy Neutron's Nicktoon Blast; as announced on March 14, 2011 as "...one of many exciting things planned for the next couple of years".[30] Universal Orlando Resort announced Transformers: The Ride will officially open in the summer of 2013, replacing Soundstages 44 and 54, which were demolished on June 24, 2012.[31] SpongeBob StorePants,a gift shop themed after SpongeBob SquarePants opened in Woody Woodpecker's Kidzone replacing the Universal Cartoon Store

2013: The opening date for Transformers The Ride is announced for June 20, 2013. Details of The Wizarding World of Harry Potter expansion are officially announced. Details for the new Simpsons Land are announced and expected to open in the summer of 2013. Transformers: The Ride officially opens in the Production Central area replacing Soundstage 44. Simpsons Fast Food Boulevard (renamed Springfield U.S.A.) concludes its expansion as it includes one new ride: Kang and Kodos Twirl 'n' Hurl.

2014: The opening date for The Wizarding World of Harry Potter Diagon Alley is announced for July 8, 2014 amid the Diagon Alley preview red carpet premiere on June 18, 2014 with Domhnall Gleeson, Bonnie Wright, Evanna Lynch, Matthew Lewis, James and Oliver Phelps, Tom Felton, Robbie Coltrane, Warwick Davis and Helena Bonham Carter attending the premiere. King's Cross station opens on July 1, 2014 as well as the Hogwarts Express Hogsmeade station at Universal's Islands of Adventure, connecting park visitors to both theme Harry Potter theme parks via a full scale replica of the train that appears in the Harry Potter film series. Diagon Alley officially opens, replacing Jaws and the Amity section of the park.

 

Previous attractions[edit]

 

Main article: List of former Universal Studios Florida attractions

     

The previous icon of the Jaws ride is still a popular photo spot.

Like all theme parks, attractions are sometimes closed due to aging and replaced with more contemporary attractions. Universal has seen this happen several times. Some notable closures include Kongfrontation, Back to the Future: The Ride, The Funtastic World of Hanna-Barbera and Jaws. The closures of Kongfrontation, Back to the Future, and Jaws have been given homages by the park to honor veteran visitors who revered the former rides.

 

Park design[edit]

 

Main article: List of Universal Studios Florida attractions

 

Universal Studios Florida features seven themed areas all situated around a large lagoon. In 2012, this lagoon was the site of Universal’s Cinematic Spectacular: 100 Years of Movie Memories, a thematic display that showcased scenes from various Universal films, featuring lasers, projectors and fountains, and pyrotechnics.

 

The seven surrounding themed areas, clockwise from the entrance, are Production Central, New York, San Francisco, London/Diagon Alley, World Expo, Woody Woodpecker's Kidzone and Hollywood. Each area features a combination of rides, shows, attractions, character appearances, dining outlets and merchandise stores. A new area, based on Harry Potter's Diagon Alley was added to the park in the July of 2014.

 

Production Central[edit]

  

Ride

 

Year opened

 

Manufacturer

  

Despicable Me: Minion Mayhem 2012 Intamin

Shrek 4-D 2003 PDI/DreamWorks

Hollywood Rip, Ride, Rockit 2009 Maurer Söhne

Transformers: The Ride 3D 2013 Oceaneering International

The Universal Music Plaza Stage 2009

  

The area is also home to a variety of dining outlets and merchandise shops. Food and beverage items can be purchased from Beverly Hills Boulangerie or Universal Studios' Classic Monsters Cafe while merchandise can be bought from a variety of themed stores including Universal Studios Store, Studio Sweets, It's a Wrap!, Super Silly Stuff, Shrek's Ye Olde Souvenir Shoppe, and Transformers: Supply Vault.[32][33]

 

Rapid strata formation in soft sand (field evidence).

Photos of strata formation in soft sand on a beach, created by tidal action of the sea.

Formed in a single, tidal event of turbulent, high tide.

 

See many other examples of rapid stratification with geological features: www.flickr.com/photos/101536517@N06/sets/72157635944904973/

 

This natural example of rapid, simultaneous stratification refutes the Superposition Principle, the Principle of Original Horizontality and the Principle of Lateral Continuity.

 

Superposition only applies on a rare occasion of sedimentary deposits in perfectly, still water. Superposition is required for the long evolutionary timescale, but the evidence shows it is not the general rule, as was once believed. Most sediment is laid down in moving water, where particle segregation is the rule, resulting in the simultaneous deposition of strata/layers as shown in the photo.

Where the water movement is very turbulent, violent, or catastrophic, great depths of stratified sediment can be laid down in a short time. Certainly not the many millions of years assumed by evolutionists.

The composition of strata formed in any deposition event. is related to whatever materials are in the sediment mix. Whatever is in the mix will be automatically sorted into strata/layers. It could be sand, or material added from mud slides, erosion of chalk deposits, volcanic ash etc. Any organic material (potential fossils) will also be sorted and buried within the rapidly, formed strata.

 

Stratified, soft sand deposit. demonstrates the rapid, stratification principle.

Important, field evidence which supports the work of the eminent, sedimentologist Dr Guy Berthault.

(Dr Berthault's experiments (www.sedimentology.fr/)

And also the experimental work of Dr M.E. Clark (Professor Emeritus, U of Illinois @ Urbana), Andrew Rodenbeck and Dr. Henry Voss, (www.ianjuby.org/sedimentation/)

 

Location: Sandown beach, Isle of Wight. Formed 17/11/2016, This field evidence demonstrates that multiple strata in sedimentary deposits do not need millions of years to form and can be formed rapidly. This natural example confirms the principle demonstrated by the sedimentation experiments carried out by Dr Guy Berthault and other sedimentologists. It calls into question the standard, multi-million year dating of sedimentary rocks, and the dating of fossils by depth of burial or position in the strata.

 

Strata lines/layers and cross bedding is present in this example.

 

Dr Berthault's experiments (www.sedimentology.fr/) and other experiments (www.ianjuby.org/sedimentation/) and field studies of floods and volcanic action show that, rather than being formed by gradual, slow deposition of sucessive layers superimposed upon previous layers, with the strata or layers representing a timescale or even a particular, environmental epoch, particle segregation in moving water or airborne particles can form strata or layers very quickly, frequently, in a single event. Such field studies and the experiments show that there is no longer any reason to conclude that strata in sedimentary rocks relate to different geological eras and/or a multi-million year timescale. www.youtube.com/watch?v=5PVnBaqqQw8&feature=share&amp.... It also shows that the relative position of fossils in rocks is not indicative of an order of evolutionary succession. Obviously, the uniformitarian principle, on which the geologic column is based, can no longer be considered valid. And the multi-million, year dating of sedimentary rocks and fossils needs to be reassessed. Rapid deposition of stratified sediments also explains the enigma of polystrate fossils, i.e. large fossils that intersect several strata. In some cases, tree trunk fossils are found which intersect the strata of sedimentary rock up to forty feet in depth. upload.wikimedia.org/wikipedia/commons/thumb/0/08/Lycopsi... They must have been buried in stratified sediment in a short time (certainly not millions or even thousands of years), or they would have rotted away. youtu.be/vnzHU9VsliQ

 

In fact, the vast majority of fossils are found in good, intact condition, which is testament to their rapid burial. You don't get good fossils from gradual burial, because they would be damaged or destroyed by decay, predation or erosion. The existence of so many fossils in sedimentary rock on a global scale is stunning evidence for the rapid depostion of sedimentary rock as the general rule. It is obvious that all rock containing good intact fossils was formed from sediment laid down in a very short time, not millions, or even thousands of years.

 

See set of photos of other examples of rapid stratification: www.flickr.com/photos/101536517@N06/sets/72157635944904973/

 

Carbon dating of coal should not be possible if it is millions of years old, yet significant amounts of Carbon 14 have been detected in coal and other fossil material, which indicates that it is less than 50,000 years old. www.ldolphin.org/sewell/c14dating.html

 

www.grisda.org/origins/51006.htm

 

Evolutionists confidently cite multi-million year ages for rocks and fossils, but what most people don't realise is that no one actually knows the age of sedimentary rocks or the fossils found within them. So how are evolutionists so sure of the ages they so confidently quote? The astonishing thing is they aren't. Sedimentary rocks cannot be dated by radiometric methods*, and fossils can only be dated to less than 50,000 years with Carbon 14 dating. The method evolutionists use is based entirely on assumptions. Unbelievably, fossils are dated by the assumed age of rocks, and rocks are dated by the assumed age of fossils, that's right ... it is known as circular reasoning.

 

* Regarding the radiometric dating of igneous rocks, which is claimed to be relevant to the dating of sedimentary rocks, in an occasional instance there is an igneous intrusion associated with a sedimentary deposit -

Prof. Aubouin says in his Précis de Géologie: "Each radioactive element disintegrates in a characteristic and constant manner, which depends neither on the physical state (no variation with pressure or temperature or any other external constraint) nor on the chemical state (identical for an oxide or a phosphate)."

"Rocks form when magma crystallizes. Crystallisation depends on pressure and temperature, from which radioactivity is independent. So, there is no relationship between radioactivity and crystallisation.

Consequently, radioactivity doesn't date the formation of rocks. Moreover, daughter elements contained in rocks result mainly from radioactivity in magma where gravity separates the heavier parent element, from the lighter daughter element. Thus radiometric dating has no chronological signification." Dr. Guy Berthault www.sciencevsevolution.org/Berthault.htm

 

Visit the fossil museum:

www.flickr.com/photos/101536517@N06/sets/72157641367196613/

 

Just how good are peer reviews of scientific papers?

www.sciencemag.org/content/342/6154/60.full

www.examiner.com/article/want-to-publish-science-paper-ju...

 

The neo-Darwinian idea that the human genome consists entirely of an accumulation of billions of mutations is, quite obviously, completely bonkers. Nevertheless, it is compulsorily taught in schools and universities as 'science'.

www.flickr.com/photos/truth-in-science/35505679183

Features: Custom waterslide decals, weapon and Kama. Please visit www.minifigmaker.com for more info.

"Pinky" was made for a bunch of requests for a female clone trooper.

Just like the Moto G, Motorola’s latest the Moto E is redefining our price expectations. On paper it sounds pretty impressive, but what’s it like in action?

 

Read on to find out more…

 

blog.pre-pay-as-you-go.co.uk/2014/06/16/moto-e-review-ref...

 

Features on: Typographische Monatsblätter, Octavo, Typography Books, Nobuhiro Yamaguchi, Critical Development of Sans Serifs.

This Chrysler Concept Show Car encompassed several evolving new design & engineering features, such as a Power Retractable Hardtop, which stored in the Front-Opening Trunk.

 

A successor to the less attractive Chrysler "Airflow" of 1934, this car was intended to improve on and advance the original Airflow concept produced by Chrysler form 1934 – 1937, but in a more attractive package.

 

This car encompassed many newly evolving features of that era, such as an envelope body with "hidden", fold-away Headlamps, Recessed & Enclosed License Plate niches front & rear, and to “Top” it off, a Power Retractable Convertible Hardtop.

 

The design began with an “envelope” style body to join & enclose the front hood & fenders, then added "hidden" fold-away Headlamps, similar to those used on the 1938 Cord 810, and also including enclosed license plate recesses front & rear. Then to “Top” it off, one of the earliest examples of a Convertible Hardtop was created. This Power Retractable Hardtop was not manually operated, but powered to stow itself, in one piece, into the Front-Opening Trunk. The top is a one-piece steel Hardtop that lifted & inverted itself, and stowed itself into the Front-Opening Trunk.

 

This car is one of the original examples made to promote the Chrysler brand, and was toured to a number of Automobile Shows Nationwide. As each of these original 5 or 6 Show Cars [experts differ on the number made] was rendered in a different color, this is the only one done in Red. It is believed that 4 of those originals still exist.

 

Design credit goes to Alex Tremulis at the age of 25.

 

Chrysler Thunderbolt LeBaron Convertible, 1941. [PB 2019

DSC_1082].