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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 hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris' superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F (80 °C). Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes (fenced off) can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till. [Source: en.wikipedia.org/wiki/Mammoth_Hot_Springs]
Yellowstone National Park is a national park located in the U.S. states of Wyoming, 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 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 Old Faithful Geyser, one of its most popular features. It has many types of ecosystems, but the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion. [Source: en.wikipedia.org/wiki/Yellowstone_National_Park]
The sunset was just developing into its full glory as we watched from high up on the esplanade in Domme overlooking the river Dordogne. And then as I clicked away with the D610 a shadow came across the images as if the camera strap had blown across the front of the lens mid shot on a very windy day. And three frames later, the shutter jammed solid, with "err" coming up on the LCD display. It seems there is nothing one can do but send it off to Nikon. Fortunately I had the Samsung phone handy to grab a lasting memory of a Dordogne sunset......and a friend who then leant me his D5100 until the D610 can be fixed.
Avatar by alpha.tribe slurl.com/secondlife/alphatribe/100/88/1 (except for the shape, entirely my fault, too much time on the computer...)
After reviewing my captures from an outing on the the ice of the bay, I found myself selecting more and more to process for posting. I now have a series exploring different compositions of ice shapes, formations and patterns in the gorgeous light o winter sunset to publish.
San Andreas Fault in San Francisco. Mother nature has now covered her tracks where the earth spit open and dropped.
Mahazedi Pagoda, Bago, Myanmar
Mahazedi Pagoda (Burmese: မဟာစေတီ) is a prominent Buddhist pagoda in Bago, Myanmar. The pagoda was built by King Bayinnaung in 1560 to house a gold and jewel-encrusted tooth relic of the Buddha. The tooth relic was, in fact, a fake replica from Dharmapala of Kotte, the king of the Kingdom of Kotte, who gifted the tooth, along with an alms bowl and his daughter. The relics arrived in 1576. In 1599, King Anaukpetlun conquered Bago and removed the relics to Taungoo. In 1636, King Thalun invaded Taungoo and removed the relics to Innwa, enshrining them at the Kaunghmudaw Pagoda in Sagaing. Throughout its history, the pagoda has been destroyed by several earthquakes on the Sagaing Fault, on 13 September 1564, 1583, and 8 October 1888, and completely leveled in 1930. Mahazedi Pagoda was rebuilt in the 1950s.
Þingvellir is a place in the administrative district of Bláskógabyggð in southwestern Iceland, near the Reykjanes peninsula and the Hengill volcanic area. Þingvellir is a site of historical, cultural, and geological importance and is one of the most popular tourist destinations in Iceland. It lies in a rift valley that marks the crest of the Mid-Atlantic Ridge. It is at the northern end of Þingvallavatn, the largest natural lake in Iceland.
Parliament or Alþingi ("Althing" in English) was established at Þingvellir in 930 and remained there until 1798.[3] Þingvellir National Park was founded in 1930, marking the 1000th anniversary of the Althing. It was later expanded to protect natural phenomena in the surrounding area, and became a World Heritage Site in 2004.
Creo que mereció la pena levantarse para este amanecer de lunes, ya no por las fotos que saqué, que no me han gustado tanto como hubiese querido, sino por el espectáculo que pude ver.
Ahora mismo estoy escuchando Not Your Fault, Awolnation.
“O happy fault, O necessary sin of Adam, which gained for us so great a Redeemer!” (Exultet of the Great Vigil of Easter)
Canon EF 24-105mm f/4L IS USM
©2014 Patrick J Bayens
From February 1st to 20th, you can't miss the incredible new ACCESS event. Let's make love a little spicy... This will be "Your new favorite Valentine's fetish" !!!
STAY TUNED ----> www.access-sl.com/cupidsfault
Laguna Salada斷層是卡爾教授起家的地方.
本來以為這次地震也是同一條斷層引發的.但是這次這條斷層似乎不是主角,最大垂直位移只有30cm左右(照片中咖啡色條帶就是這次的位移),而1892年的地表破裂(在咖啡色上方深褐色的部分)最大垂直位移有3.5米,最大右移分量有4米.
Multiple levels (parallel planes; rock surface curves down to right) of slickensided fault surfaces in an outcrop of Marron Fm. andesitic volcanic rock (in south-central British Columbia), with one of my fingers for scale. Above my finger, the lighter coloured material is a mineral vein (fluid flowed along a fault plane and mineral precipitated from solution) with a patchy distribution now because it is partly eroded away.
The slickenlines present have two different groove lineation directions, diagonal down to the left and down to the right in both the purplish-brown host rock and the light brown vein material. They record two different steep (sub-vertical) directions of fault motion at this site back in the Eocene (ca. 50 million years ago), a time of post-orogenic normal faulting in this part of western Canada.
C. J.R. Devaney
en.wikipedia.org/wiki/York_Minster
The Cathedral and Metropolitical Church of Saint Peter in York, commonly known as York Minster, is the cathedral of York, England, and is one of the largest of its kind in Northern Europe. The minster is the seat of the Archbishop of York, the second-highest office of the Church of England, and is the cathedral for the Diocese of York. It is run by a dean and chapter, under the Dean of York. The title "minster" is attributed to churches established in the Anglo-Saxon period as missionary teaching churches, and serves now as an honorific title.[1] Services in the minster are sometimes regarded as on the High Church or Anglo-Catholic end of the Anglican continuum.[2]
The minster has a very wide Decorated Gothic nave and chapter house, a Perpendicular Gothic Quire and east end and Early English North and South transepts. The nave contains the West Window, constructed in 1338, and over the Lady Chapel in the east end is the Great East Window, (finished in 1408), the largest expanse of medieval stained glass in the world. In the north transept is the Five Sisters Window, each lancet being over 52 feet (16 m) high.[citation needed] The south transept contains a rose window, while the West Window contains a heart-shaped design colloquially known as 'The Heart of Yorkshire'.
History
York has had a verifiable Christian presence from the 4th century. However, there is circumstantial evidence pointing to much earlier Christian involvement. According to Bede, missionaries were sent from Rome by Eleutherius at the request of the chieftain Lucius of Britain in AD 180 to settle controverted points of differences as to Eastern and Western ceremonials which were disturbing the church. Tradition speaks of 28 British bishops, one for each of the greater British cities, over whom presided the Archbishops of London, York and Caerleon-on-Usk.
The first recorded church on the site was a wooden structure built hurriedly in 627 to provide a place to baptise Edwin, King of Northumbria. Moves toward a more substantial building began in the decade of the 630s. A stone structure was completed in 637 by Oswald and was dedicated to Saint Peter. The church soon fell into disrepair and was dilapidated by 670 when Saint Wilfrid ascended to the See of York. He repaired and renewed the structure. The attached school and library were established and by the 8th century were some of the most substantial in Northern Europe.[citation needed][3]
In 741 the church was destroyed in a fire. It was rebuilt as a more impressive structure containing thirty altars. The church and the entire area then passed through the hands of numerous invaders, and its history is obscure until the 10th century. There was a series of Benedictine archbishops, including Saint Oswald of Worcester, Wulfstan and Ealdred, who travelled to Westminster to crown William in 1066. Ealdred died in 1069 and was buried in the church.[4]
The church was damaged in 1069 during William the Conqueror's harrying of the North, but the first Norman archbishop, Thomas of Bayeux, arriving in 1070, organised repairs. The Danes destroyed the church in 1075, but it was again rebuilt from 1080. Built in the Norman style, it was 111 m (364.173 ft) long and rendered in white and red lines. The new structure was damaged by fire in 1137 but was soon repaired. The choir and crypt were remodelled in 1154, and a new chapel was built, all in the Norman style.
The Gothic style in cathedrals had arrived in the mid 12th century. Walter de Gray was made archbishop in 1215 and ordered the construction of a Gothic structure to compare to Canterbury; building began in 1220. The north and south transepts were the first new structures; completed in the 1250s, both were built in the Early English Gothic style but had markedly different wall elevations. A substantial central tower was also completed, with a wooden spire. Building continued into the 15th century.
The Chapter House was begun in the 1260s and was completed before 1296. The wide nave was constructed from the 1280s on the Norman foundations. The outer roof was completed in the 1330s, but the vaulting was not finished until 1360. Construction then moved on to the eastern arm and chapels, with the last Norman structure, the choir, being demolished in the 1390s. Work here finished around 1405. In 1407 the central tower collapsed; the piers were then reinforced, and a new tower was built from 1420. The western towers were added between 1433 and 1472. The cathedral was declared complete and consecrated in 1472.[5]
The nave of York Minster
The English Reformation led to the looting of much of the cathedral's treasures and the loss of much of the church lands. Under Elizabeth I there was a concerted effort to remove all traces of Roman Catholicism from the cathedral; there was much destruction of tombs, windows and altars. In the English Civil War the city was besieged and fell to the forces of Cromwell in 1644, but Thomas Fairfax prevented any further damage to the cathedral.
Following the easing of religious tensions there was some work to restore the cathedral. From 1730 to 1736 the whole floor of the minster was relaid in patterned marble and from 1802 there was a major restoration. However, on 2 February 1829, an arson attack by a non-conformist, Jonathan Martin,[6] inflicted heavy damage on the east arm. An accidental fire in 1840 left the nave, south west tower and south aisle roofless and blackened shells. The cathedral slumped deeply into debt and in the 1850s services were suspended. From 1858 Augustus Duncombe worked successfully to revive the cathedral.
During the 20th century there was more concerted preservation work, especially following a 1967 survey that revealed the building, in particular the central tower, was close to collapse. £2,000,000 was raised and spent by 1972 to reinforce and strengthen the building foundations and roof. During the excavations that were carried out, remains of the north corner of the Roman Principia (headquarters of the Roman fort, Eboracum) were found under the south transept. This area, as well as remains of the Norman cathedral, re-opened to the public in spring 2013 as part of the new exhibition exploring the history of the building of York Minster.[7]
On 9 July 1984, a fire believed to have been caused by a lightning strike[8] destroyed the roof in the south transept, and around £2.5 million was spent on repairs. The fire was photographed from just south of the minster in the early hours by Bettison photographers. This picture was subsequently published showing the South transept alight with a list of North Yorkshire firefighters attending. The stations attending ranged from Scarborough to Harrogate. Huge amounts of water were needed to provide jets at great height to hit the roof timbers and protect the Rose Window. Most of the water was pumped from the Ouse nearby because the water supplies around the minster were inadequate. Fire crews from the main York fire station in Clifford Street worked hard to protect the Rose Window and stop the fire spreading into the tower and organ. Many crews worked for hours and some were on high levels of the minster at the time when the South transept roof fell in. Luckily, those few firefighters inside when the roof crashed down were not directly beneath. But what they saw after the ventilation released the smoke, was a pile of timber covering the whole of the south transept floor to a height of at least six feet. When daylight came the whole scene was occupied by media. At about 8am an officer was approached by two ladies looking for information. "Have you an account for The Times"? They said. The officer replied, "Actually, I spoke to the London and New York Times at about four thirty" The ladies then announced that they were from the Church Times. Reports of the fire travelled across both hemispheres. The Restoration work was completed in 1988, and included new roof bosses to designs which had won a competition organised by BBC Television's Blue Peter programme. In 2007 renovation began on the east front, including the Great East Window, at an estimated cost of £23 million.[9][10]
In 2000, the Dean and Chapter allowed the York Mystery Plays to be performed for the first time inside the Minster, directed by Greg Doran.[11]
Architecture of the present building
York Minster is the second largest Gothic cathedral of Northern Europe and clearly charts the development of English Gothic architecture from Early English through to the Perpendicular Period. The present building was begun in about 1230 and completed in 1472. It has a cruciform plan with an octagonal chapter house attached to the north transept, a central tower and two towers at the west front. The stone used for the building is magnesian limestone, a creamy-white coloured rock that was quarried in nearby Tadcaster. The Minster is 173 yards (158 m) long[citation needed] and the central tower has a height of 230 feet (70 m) high.[citation needed] The choir has an interior height of 102 feet (31 m).[citation needed]
The north and south transepts were the first parts of the new church to be built. They have simple lancet windows, including the Five Sisters in the north transept. These are five lancets, each 52 feet (16 m) high[citation needed] and glazed with grey (grisaille) glass, rather than narrative scenes or symbolic motifs that are usually seen in medieval stained glass windows. In the south transept is a rose window whose glass dates from about 1500 and commemorates the union of the royal houses of York and Lancaster. The roofs of the transepts are of wood, that of the south transept was burnt in the fire of 1984 and was replaced in the restoration work which was completed in 1988. New designs were used for the bosses, five of which were designed by winners of a competition organised by the BBC's Blue Peter television programme.
The chapter house.
Work began on the chapter house and its vestibule that links it to the north transept after the transepts were completed. The style of the chapter house is of the early Decorated Period where geometric patterns were used in the tracery of the windows, which were wider than those of early styles. However, the work was completed before the appearance of the ogee curve, an S-shaped double curve which was extensively used at the end of this period. The windows cover almost all of the upper wall space, filling the chapter house with light. The chapter house is octagonal, as is the case in many cathedrals, but is notable in that it has no central column supporting the roof. The wooden roof, which was of an innovative design, is light enough to be able to be supported by the buttressed walls. The chapter house has many sculptured heads above the canopies, representing some of the finest Gothic sculpture in the country. There are human heads, no two alike, and some pulling faces; angels; animals and grotesques. Unique to the transepts and chapter house is the use of Purbeck marble to adorn the piers, adding to the richness of decoration.
The Kings Screen and organ.
The nave was built between 1291 and c. 1350 and is also in the decorated Gothic style. It is the widest Gothic nave in England and has a wooden roof (painted so as to appear like stone) and the aisles have vaulted stone roofs. At its west end is the Great West Window, known as the 'Heart of Yorkshire' which features flowing tracery of the later decorated gothic period.
The east end of the Minster was built between 1361 and 1405 in the Perpendicular Gothic style. Despite the change in style, noticeable in details such as the tracery and capitals, the eastern arm preserves the pattern of the nave. The east end contains a four bay choir; a second set of transepts, projecting only above half-height; and the Lady Chapel. The transepts are in line with the high altar and serve to throw light onto it. Behind the high altar is the Great East Window, the largest expanse of medieval stained glass in the world, which is currently undergoing a massive conservation project, due to be completed in 2015–16. Below the Great East Window currently sits the Orb, a stainless steel dome which opened at the end of October 2012, containing five of the conserved panels from the window, one of which is changed each month. The Orb enables visitors to see the work of renowned medieval artist, John Thornton, up close, revealing the remarkable detail in each panel.
The sparsely decorated Central Tower was built between 1407 and 1472 and is also in the Perpendicular style. Below this, separating the choir from the crossing and nave is the striking 15th century choir screen. It contains sculptures of the kings of England from William the Conqueror to Henry VI with stone and gilded canopies set against a red background. Above the screen is the organ, which dates from 1832. The West Towers, in contrast with the Central Tower, are heavily decorated and are topped with battlements and eight pinnacles each, again in the Perpendicular style.
English Heritage has recently made publicly available a monograph[12] on the architectural history of York Minster. The book charts the construction and development of the minster based on the architectural recording of the building from the 1970s. The full report can be downloaded from the Archaeology Data Service website.
Stained glass
York as a whole, and particularly the minster, have a long tradition of creating beautiful stained glass. Some of the stained glass in York Minster dates back to the 12th century. The Minster's records show that much of the glass (white or coloured) came from Germany.[13] Upon arrival at York, it was intricately painted, fired, then glazed together with lead strips into the windows. The 76-foot (23 m)[citation needed] tall Great East Window, created by John Thornton in the early 15th century, is the largest expanse of medieval stained glass in the world. Other windows in the minster include an ornate rose window and the 50-foot (15 m)[citation needed] tall Five Sisters window. Because of the extended time periods during which the glass was installed, different types of glazing and painting techniques which evolved over hundreds of years are visible in the different windows. Approximately two million individual pieces of glass make up the cathedral's 128 stained glass windows. Much of the glass was removed before and pieced back together after the First and Second World Wars, and the windows are constantly being cleaned and conserved to keep their beauty intact.
In 2008 a major conservation project of the Great East Window commenced, involving the removal, repainting and re-leading of each individual panel.[14] While the window was in storage in the minster's stonemasons' yard, a fire broke out in some adjoining offices, due to an electrical fault, on 30 December 2009.[15] The window's 311 panes, stored in a neighbouring room, were undamaged and were successfully moved to safety.[16][17] In September 2015 Phase One of the renovation project of the East Front of the Minster was completed.[18]
Towers and bells
The two west towers of the minster hold bells, clock chimes and a concert carillon. The north-west tower contains Great Peter (216 cwt or 10.8 tons) and the six clock bells (the largest weighing just over 60 cwt or 3 tons). The south-west tower holds 14 bells (tenor 59 cwt or 3 tons) hung and rung for change ringing and 22 carillon bells (tenor 23 cwt or 1.2 tons) which are played from a baton keyboard in the ringing chamber (all together 35 bells.)
The clock bells ring every quarter of an hour during the daytime and Great Peter strikes the hour. The change ringing bells are rung regularly on Sundays before church services and at other occasions, the ringers practise on Tuesday evenings. York Minster became the first cathedral in England to have a carillon of bells with the arrival of a further twenty-four small bells on 4 April 2008. These are added to the existing "Nelson Chime" which is chimed to announce Evensong around 5.00 pm each day, giving a carillon of 35 bells in total (three chromatic octaves). The new bells were cast at the Loughborough Bell Foundry of Taylors, Eayre & Smith, where all of the existing minster bells were cast. The new carillon is a gift to the minster. It will be the first new carillon in the British Isles for 40 years and first hand played carillon in an English cathedral. Before Evensong each evening, hymn tunes are played on a baton keyboard connected with the bells, but occasionally anything from Beethoven to the Beatles may be heard.[19]
Shrines
When Thomas Becket was murdered and subsequently enshrined at Canterbury, York found itself with a rival major draw for pilgrims. More specifically, pilgrims spent money and would leave gifts for the support of the cathedral. Hence Walter de Gray, supported by the King, petitioned the Pope. On 18 March 1226, Pope Honorius issued a letter to the effect that the name of William (Fitzherbert), formerly Archbishop of York, was "inscribed in the catalogue of the Saints of the Church Militant." Thus there was now St William of York (whose name is perhaps more often associated with the adjacent St William's College). York had its saint but it took until 1279, when William de Wickwane (William de Wykewayne) was elected archbishop, for the remains of the canonised William to be transferred to a shrine prepared for them behind the high altar.[20] This was placed on a platform raised upon the arches of the crypt removed to this position for that purpose. On 29 December King Edward I himself, together with the bishops who were present, carried on their shoulder the chest or feretory containing the relics to their new resting-place and Anthony Beck, consecrated the same day as Bishop of Durham, paid all the expenses.
The tomb of Walter de Gray was erected in the south transept. His remains were interred on "the vigil of Pentecost, 1255"[20] under his effigy "in full canonicals" carved in Purbeck marble under a canopy resting on ten light pillars. It was subsequently somewhat hidden behind a screen of ironwork erected by Archbishop William Markham in the early 19th century.
Organ
The choir
The fire of 1829 destroyed the organ and the basis of the present organ dates from 1832, when Elliot and Hill constructed a new instrument. This organ was reconstructed in 1859 by William Hill and Sons. The case remained intact, but the organ was mechanically new, retaining the largest pipes of the former instrument.
In 1903, J.W. Walker and Sons built a new instrument in the same case. They retained several registers from the previous instrument.
Some work was undertaken in 1918 by Harrison & Harrison when the Tuba Mirabilis was added and the Great chorus revised. The same firm rebuilt this Walker-Harrison instrument in 1931 when a new console and electro-pneumatic action were added together with four new stops. The smaller solo tubas were enclosed in the solo box. In 1960, J.W. Walker & Sons restored the actions, lowered wind pressures and introduced mutations and higher chorus work in the spirit of the neo-classical movement. They cleaned the organ in 1982.
The fire of 1984 affected the organ but not irreparably; the damage hastened the time for a major restoration, which was begun in 1991 and finished two years later by Principal Pipe Organs of York, under the direction of their founder, Geoffrey Coffin, who had at one time been assistant organist at the Minster.[21]
Organists
The organists of York Minster have had several official titles, the job description roughly equates to that of Organist and Master of the Choristers. The current Organist and Director of Music of the minster is Robert Sharpe. There is also an assistant director of music, David Pipe, and an organ scholar.
Among the notable organists of York Minster are four members of the Camidge family, who served as the cathedral's organists for over 100 years, and a number of composers including John Naylor, T. Tertius Noble, Edward Bairstow, Francis Jackson, and Philip Moore.
Dean and chapter
Dean: The Very Revd Vivienne Faull (since 1 December 2012 installation[22])
Precentor: The Revd Canon Peter Moger (since 12 September 2010 installation[23])
Pastor: The Reverend Michael Smith
Chancellor: The Reverend Canon Christopher Collingwood
Archdeacon: The Reverend Canon David Butterfield
Burials
Bosa of York, Bishop of York and Saint (died c. 705)
Eanbald I, Archbishop (780–796)
Osbald, King of Northumbria (died 799)
Ealdred (archbishop of York) (1061–1069)
Thomas of Bayeux, Archbishop (1070–1100)
Gerard, Archbishop (1100–1108)
Thomas II of York, Archbishop (1108–1114)
William of York, Archbishop (1141–1147, 1153–1154)
Henry Murdac, Archbishop (1147–1153)
Roger de Pont L'Eveque, Archbishop {1154–1181}
Walter de Gray, Archbishop (1216–1255)
Sewal de Bovil, Dean and Archbishop (1256–1258)
Godfrey Ludham, Archbishop (1258–1265)
William Langton, Archbishop (1265)
Walter Giffard, Archbishop (1266–1279)
John le Romeyn, Archbishop (1286–1296)
Henry of Newark, Archbishop (1296–1299)
William Greenfield, Archbishop (1306–1315)
Prince William of Hatfield, Infant son of Edward III (1337)
William Melton, Archbishop (1317–1340)
William Zouche, Archbishop (1342–1352)
Henry Percy, soldier (1364–1403)
Richard le Scrope, Archbishop (1398–1405)
Henry Bowet, Archbishop (1407–1423)
Thomas Savage, Archbishop (1501–1507)
Hugh Ashton, Archdeacon of York (died 1522)
John Piers, Archbishop (1589–1594)
George Meriton, Dean of York (1579–1624)
Charles Watson-Wentworth, 2nd Marquess of Rockingham, (1730-1782)
John Farr Abbott, barrister (1756–1794)
Astronomical clock
The astronomical clock was installed in the North Transept of York Minster in 1955. The clock is a memorial to the airmen operating from bases in Yorkshire, County Durham and Northumberland who were killed in action during the Second World War.[24]
Illuminations
In November 2002, York Minster was illuminated in colour, devised by York-born Mark Brayshaw, for the first time in its history. The occasion was televised live on the BBC1 Look North programme. Similar illuminations have been projected over the Christmas period in subsequent years.
York Minster was also artistically illuminated on 5 November 2005, celebrating the 400th anniversary of the foiling of York-born Guy Fawkes' gunpowder plot. This was done by Patrice Warrener using his unique "chromolithe" technique with which he 'paints' with light, picking out sculpted architectural details.
In October 2010, York Minster's south transept was selected for "Rose", a son et lumiere created by international artists Ross Ashton and Karen Monid which lit up the entire exterior of the south transept of the minster and illuminated the Rose Window. There were also satellite illuminate events in Dean's Park.
This stunning image shows off the results of faults in Granicus and Tinjar Valles. Our goal is to look for changes over time of the walls of the faults. Granicus Valles are a network of valleys, probably outflow channels, that are 750 kilometers in length and located west of Elysium Mons. Both water and lava may have played a role in its formation.
This cutout is less than 5 km (3 mi) across and the spacecraft altitude was 289 km (180 mi) and north is to the left. For full images including scale bars, visit the source link.
www.uahirise.org/ESP_057042_2075
NASA/JPL-Caltech/UArizona
I won't let you choke on the noose around your neck.
26/52
Officially half-way done with this project!
Kay Kay and I went to breakfast and then went and froze our butts off at the beach. I almost fell through ice and Kay Kay almost had a heart attack.
Happy St. Patrick's Day from us both!
James Rogers
Part of the Olympus (Australia) Digital Pen competition. Voting is done... View the set.
The Overhang Fault is a major structure south of Cloncurry that separates the Overhang Jaspilite (from the Quilalar-Corella Intra-continental Sea) on the west, from the younger Staveley Formation (from the Calvert Superbasin) on the east.
The Overhang Jaspilite is a charismatic but enigmatic unit forming stark black outcrops. Jaspilite is a chemical rock precipitated from sea water like chert, which is generally iron rich and typically a banded accumulation of reddish hematite-rich layers and grey to white quartz. It is deposited under quiet conditions. Although it is a characteristic component there is actually not much jaspilite in the unit, which is mainly siltstone, but the name has stuck.
Mining in the Overhang Fault was worked from 1959 - 1962 when 7270 tonnes of manganese ore were used as an oxidant in the acid leach plant at the Mary Kathleen mine. It contains a concentration of various manganese oxides including manganite, pyrolusite, and psilomelane.
Source: Rocks and Landscapes of Northwest Queensland by Laurie Hutton & Ian Withnall.
Another from Saturday morning's misty sunrise at Cresswell. For this one I used a little bit more in the way of filtering to bring out the colours in the sky and used the interesting rock faults as a lead in.
From my one visit here, this looks like a cracking spot at pretty much any tide, which is good, as I always struggle for high tide locations.
No flashing invites / banners please
EOS 1000D / Sigma 10-20MM / Hitech 0.6 Hard & Soft grads
Foto por Jon Jacobsen
Asistente Miguel
Produccion de vestuario: YO!!!! :)
Revisen la nota de Jon en el Lun
www.lun.com/Pages/NewsDetail.aspx?dt=2009-10-26&Pagin...
Y no olviden visitar su exposición en galería Moro :)
pd:Vote por mi foto en el concurso de Garnier, busque por Camila, encuentre esta foto y regaleme un voto :)