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Hodor is a motor yacht with a length of 66.2m. The yacht's builder is Astilleros Armon from Spain who delivered superyacht Hodor in 2019. The superyacht has a beam of 14.0m, a draft of 3.1m and a volume of 1,582 GT.
The support yacht yacht features exterior design by Incat Crowther, while her interior was penned by Oliver Design , with naval architecture by Incat Crowther. Up to 20 crew members including the captain of Hodor are accommodated on board the superyacht Hodor, The yacht Hodor has a aluminium hull and aluminium superstructure. She is powered by 2 MTU engines, which give her a cruising speed of 14.0 kn and a top speed of 22.5 kn. The yacht has a range of 142.0/5000 n/m nautical miles at a speed of 14.0 kn. The yacht carries 16,000 liters of fuel on board, and 20,000 liters of water.
On the ranking of the largest yachts in the world, Hodor superyacht is listed as number 336th. She is the 3rd-largest yacht built by Astilleros Armon. The owner of yacht Hodor is shown in SYT iQ and is exclusively available to subscribers. On SuperYacht Times we have 12 photos of yacht Hodor, and she is featured in 9 yacht news articles. Refit market data from SYT iQ show that the yacht was last refitted in 2020.
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:
When searching for traditional kitchen decorating concepts, take into consideration which classic kitchen remodeling suggestions inspire you. Classic kitchen design still sports sophisticated additions that define it as a classic style. You do not have to have an all-white kitchen just to have a...
The Goodwood Revival takes place every September and is a classic car-based event that transports visitors back to 1940s-1960s period. Adding to the period feel, the shuttle bus 902 service from Chichester to the event features a number of vintage buses as well as modern examples.
I visited the shuttle terminals on a glorious Friday (13/09/2019) and enjoyed the atmosphere throughout the day. Buses in use on the various shuttle services / private hires included:
HAP985 1953 Brighton Hove & District Bristol KSW;
LRV992 1956 Devon General Leyland PD2 (new to Portsmouth);
2722CD 1961 Southdown Leyland Leopard;
406DCD 1964 Southdown Leyland PD3 'Queen Mary';
409DCD 1964 Southdown Leyland PD3 'Queen Mary';
BUF260C 1965 Southdown Leyland PD3 'Queen Mary';
BUF272C 1965 Southdown Leyland PD3 'Queen Mary';
DEK3D 1966 Wigan Leyland PD2;
JAH553D 1966 Eastern Counties Bristol FLF;
JJD565D 1966 Stratford Blue AEC Routemaster;
JRJ281E 1967 Salford Leyland PD2;
KPM91E 1967 Bristol FLF;
OKO816G 1968 Maidstone & District Leyland Leopard;
BFX666T 1979 Wilts & Dorset Bristol VRT;
J501GCD 1991 Stagecoach Dennis Dart;
KX06LYU 2006 Stagecoach Alexander Dennis Trident;
404DCD 2006 Stagecoach Alexander Dennis Enviro400 'The Pink Lady II';
GX11AKK 2011 Stagecoach Alexander Dennis Enviro400;
LX12DFV 2012 Stagecoach Alexander Dennis Enviro400;
LX12DHA/C/D/F 2012 Stagecoach Alexander Dennis Enviro400.
Headland is a civil parish in the Borough of Hartlepool, County Durham, England. The parish covers the old part of Hartlepool and nearby villages.
History
The Heugh Battery, one of three constructed to protect the port of Hartlepool in 1860, is located in the area along with a museum.
The area made national headlines in July 1994 in connection with the murder of Rosie Palmer, a local toddler.
On 19 March 2002 the Time Team searched for an Anglo-Saxon monastery.
Dominating the skyline is the impressive architectural structure that is St Hilda’s Church. Remnant of Hartlepool’s Saxon heritage and undoubtedly the crowning glory of the Headland, this church is a must-see attraction. After her stay in Hartlepool, the Abbess of the church progressed along the coast to Whitby and this spiritual journey can be explored through ‘The Way of St Hild’ walking trail.
A great way to explore the historic Headland is by finding and following the Headland Story Trail. The trail features 18 different information boards, each telling a story of the areas fascinating heritage from tales of shipwreck to the legend of the Hartlepool monkey. A truly interactive and fun walking experience!
Other landmarks of note include the impressive Town Wall, dating from the 14th century. This grade I listed, scheduled ancient monument still guards the Headland, and was originally built to keep out the twin threats of raiding Scots and the rigours of the North Sea.
The Borough Hall is another striking building and dates back to 1865. This gorgeous entertainment venue hosts an action-packed events programme so be sure to keep an eye out for all upcoming events here.
Dive into the town’s military history at The Heugh Battery Museum – this restored coastal defence battery protected the town throughout both World Wars. An enchanting historical sight with the original barrack room, underground magazines, coastal artillery and observation tower, the exhibits tell the story of those who lost their lives and the brave men who defended the area. Refresh with a light bite or sweet treat at the Poppy Café, located within the museum.
Visit the Headland War Memorial to see the magnificent ‘Winged Victory’ – a stunning statue that tributes those who lost their lives during the two world wars.
At the very north of the Headland you will find Spion Kop Cemetery – this historic cemetery supports a species-rich dune grassland and offers fantastic views of the coastline.
Every summer Headland Carnival attracts lively visitors to the area. Packed with thrilling rides, amusing games and live entertainment this week of jam-packed fun is great for all the family.
Hartlepool is a seaside and port town in County Durham, England. It is governed by a unitary authority borough named after the town. The borough is part of the devolved Tees Valley area. With an estimated population of 87,995, it is the second-largest settlement (after Darlington) in County Durham.
The old town was founded in the 7th century, around the monastery of Hartlepool Abbey on a headland. As the village grew into a town in the Middle Ages, its harbour served as the County Palatine of Durham's official port. The new town of West Hartlepool was created in 1835 after a new port was built and railway links from the South Durham coal fields (to the west) and from Stockton-on-Tees (to the south) were created. A parliamentary constituency covering both the old town and West Hartlepool was created in 1867 called The Hartlepools. The two towns were formally merged into a single borough called Hartlepool in 1967. Following the merger, the name of the constituency was changed from The Hartlepools to just Hartlepool in 1974. The modern town centre and main railway station are both at what was West Hartlepool; the old town is now generally known as the Headland.
Industrialisation in northern England and the start of a shipbuilding industry in the later part of the 19th century meant it was a target for the Imperial German Navy at the beginning of the First World War. A bombardment of 1,150 shells on 16 December 1914 resulted in the death of 117 people in the town. A severe decline in heavy industries and shipbuilding following the Second World War caused periods of high unemployment until the 1990s when major investment projects and the redevelopment of the docks area into a marina saw a rise in the town's prospects. The town also has a seaside resort called Seaton Carew.
History
The place name derives from Old English heort ("hart"), referring to stags seen, and pōl (pool), a pool of drinking water which they were known to use. Records of the place-name from early sources confirm this:
649: Heretu, or Hereteu.
1017: Herterpol, or Hertelpolle.
1182: Hierdepol.
Town on the heugh
A Northumbrian settlement developed in the 7th century around an abbey founded in 640 by Saint Aidan (an Irish and Christian priest) upon a headland overlooking a natural harbour and the North Sea. The monastery became powerful under St Hilda, who served as its abbess from 649 to 657. The 8th-century Northumbrian chronicler Bede referred to the spot on which today's town is sited as "the place where deer come to drink", and in this period the Headland was named by the Angles as Heruteu (Stag Island). Archaeological evidence has been found below the current high tide mark that indicates that an ancient post-glacial forest by the sea existed in the area at the time.
The Abbey fell into decline in the early 8th century, and it was probably destroyed during a sea raid by Vikings on the settlement in the 9th century. In March 2000, the archaeological investigation television programme Time Team located the foundations of the lost monastery in the grounds of St Hilda's Church. In the early 11th century, the name had evolved into Herterpol.
Hartness
Normans and for centuries known as the Jewel of Herterpol.
During the Norman Conquest, the De Brus family gained over-lordship of the land surrounding Hartlepool. William the Conqueror subsequently ordered the construction of Durham Castle, and the villages under their rule were mentioned in records in 1153 when Robert de Brus, 1st Lord of Annandale became Lord of Hartness. The town's first charter was received before 1185, for which it gained its first mayor, an annual two-week fair and a weekly market. The Norman Conquest affected the settlement's name to form the Middle English Hart-le-pool ("The Pool of the Stags").
By the Middle Ages, Hartlepool was growing into an important (though still small) market town. One of the reasons for its escalating wealth was that its harbour was serving as the official port of the County Palatine of Durham. The main industry of the town at this time was fishing, and Hartlepool in this period established itself as one of the primary ports upon England's Eastern coast.
In 1306, Robert the Bruce was crowned King of Scotland, and became the last Lord of Hartness. Angered, King Edward I confiscated the title to Hartlepool, and began to improve the town's military defences in expectation of war. In 1315, before they were completed, a Scottish army under Sir James Douglas attacked, captured and looted the town.
In the late 15th century, a pier was constructed to assist in the harbour's workload.
Garrison
Hartlepool was once again militarily occupied by a Scottish incursion, this time in alliance with the Parliamentary Army during the English Civil War, which after 18 months was relieved by an English Parliamentarian garrison.
In 1795, Hartlepool artillery emplacements and defences were constructed in the town as a defensive measure against the threat of French attack from seaborne Napoleonic forces. During the Crimean War, two coastal batteries were constructed close together in the town to guard against the threat of seaborne attacks from the Imperial Russian Navy. They were entitled the Lighthouse Battery (1855) and the Heugh Battery (1859).
Hartlepool in the 18th century became known as a town with medicinal springs, particularly the Chalybeate Spa near the Westgate. The poet Thomas Gray visited the town in July 1765 to "take the waters", and wrote to his friend William Mason:
I have been for two days to taste the water, and do assure you that nothing could be salter and bitterer and nastier and better for you... I am delighted with the place; there are the finest walks and rocks and caverns.
A few weeks later, he wrote in greater detail to James Brown:
The rocks, the sea and the weather there more than made up to me the want of bread and the want of water, two capital defects, but of which I learned from the inhabitants not to be sensible. They live on the refuse of their own fish-market, with a few potatoes, and a reasonable quantity of Geneva [gin] six days in the week, and I have nowhere seen a taller, more robust or healthy race: every house full of ruddy broad-faced children. Nobody dies but of drowning or old-age: nobody poor but from drunkenness or mere laziness.
Town by the strand
By the early nineteenth century, Hartlepool was still a small town of around 900 people, with a declining port. In 1823, the council and Board of Trade decided that the town needed new industry, so the decision was made to propose a new railway to make Hartlepool a coal port, shipping out minerals from the Durham coalfield. It was in this endeavour that Isambard Kingdom Brunel visited the town in December 1831, and wrote: "A curiously isolated old fishing town – a remarkably fine race of men. Went to the top of the church tower for a view."
But the plan faced local competition from new docks. 25 kilometres (16 mi) to the north, the Marquis of Londonderry had approved the creation of the new Seaham Harbour (opened 31 July 1831), while to the south the Clarence Railway connected Stockton-on-Tees and Billingham to a new port at Port Clarence (opened 1833). Further south again, in 1831 the Stockton and Darlington Railway had extended into the new port of Middlesbrough.
The council agreed the formation of the Hartlepool Dock and Railway Company (HD&RCo) to extend the existing port by developing new docks, and link to both local collieries and the developing railway network in the south. In 1833, it was agreed that Christopher Tennant of Yarm establish the HD&RCo, having previously opened the Clarence Railway (CR). Tennant's plan was that the HD&RCo would fund the creation of a new railway, the Stockton and Hartlepool Railway, which would take over the loss-making CR and extended it north to the new dock, thereby linking to the Durham coalfield.
After Tennant died, in 1839, the running of the HD&RCo was taken over by Stockton-on-Tees solicitor, Ralph Ward Jackson. But Jackson became frustrated at the planning restrictions placed on the old Hartlepool dock and surrounding area for access, so bought land which was mainly sand dunes to the south-west, and established West Hartlepool. Because Jackson was so successful at shipping coal from West Hartlepool through his West Hartlepool Dock and Railway Company and, as technology developed, ships grew in size and scale, the new town would eventually dwarf the old town.
The 8-acre (3.2-hectare) West Hartlepool Harbour and Dock opened on 1 June 1847. On 1 June 1852, the 14-acre (5.7-hectare) Jackson Dock opened on the same day that a railway opened connecting West Hartlepool to Leeds, Manchester and Liverpool. This allowed the shipping of coal and wool products eastwards, and the shipping of fresh fish and raw fleeces westwards, enabling another growth spurt in the town. This in turn resulted in the opening of the Swainson Dock on 3 June 1856, named after Ward Jackson's father-in-law. In 1878, the William Gray & Co shipyard in West Hartlepool achieved the distinction of launching the largest tonnage of any shipyard in the world, a feat to be repeated on a number of occasions. By 1881, old Hartlepool's population had grown from 993 to 12,361, but West Hartlepool had a population of 28,000.
Ward Jackson Park
Ward Jackson helped to plan the layout of West Hartlepool and was responsible for the first public buildings. He was also involved in the education and the welfare of the inhabitants. In the end, he was a victim of his own ambition to promote the town: accusations of shady financial dealings, and years of legal battles, left him in near-poverty. He spent the last few years of his life in London, far away from the town he had created.
World Wars
In Hartlepool near Heugh Battery, a plaque in Redheugh Gardens War Memorial "marks the place where the first ...(German shell) struck... (and) the first soldier was killed on British soil by enemy action in the Great War 1914–1918."
The area became heavily industrialised with an ironworks (established in 1838) and shipyards in the docks (established in the 1870s). By 1913, no fewer than 43 ship-owning companies were located in the town, with the responsibility for 236 ships. This made it a key target for Germany in the First World War. One of the first German offensives against Britain was a raid and bombardment by the Imperial German Navy on the morning of 16 December 1914,
Hartlepool was hit with a total of 1150 shells, killing 117 people. Two coastal defence batteries at Hartlepool returned fire, launching 143 shells, and damaging three German ships: SMS Seydlitz, SMS Moltke and SMS Blücher. The Hartlepool engagement lasted roughly 50 minutes, and the coastal artillery defence was supported by the Royal Navy in the form of four destroyers, two light cruisers and a submarine, none of which had any significant impact on the German attackers.
Private Theophilus Jones of the 18th Battalion Durham Light Infantry, who fell as a result of this bombardment, is sometimes described as the first military casualty on British soil by enemy fire. This event (the death of the first soldiers on British soil) is commemorated by the 1921 Redheugh Gardens War Memorial together with a plaque unveiled on the same day (seven years and one day after the East Coast Raid) at the spot on the Headland (the memorial by Philip Bennison illustrates four soldiers on one of four cartouches and the plaque, donated by a member of the public, refers to the 'first soldier' but gives no name). A living history group, the Hartlepool Military Heritage Memorial Society, portray men of that unit for educational and memorial purposes.
Hartlepudlians voluntarily subscribed more money per head to the war effort than any other town in Britain.
On 4 January 1922, a fire starting in a timber yard left 80 people homeless and caused over £1,000,000 of damage. Hartlepool suffered badly in the Great Depression of the 1930s and endured high unemployment.
Unemployment decreased during the Second World War, with shipbuilding and steel-making industries enjoying a renaissance. Most of its output for the war effort were "Empire Ships". German bombers raided the town 43 times, though, compared to the previous war, civilian losses were lighter with 26 deaths recorded by Hartlepool Municipal Borough[19] and 49 by West Hartlepool Borough. During the Second World War, RAF Greatham (also known as RAF West Hartlepool) was located on the South British Steel Corporation Works.
The merge
In 1891, the two towns had a combined population of 64,000. By 1900, the two Hartlepools were, together, one of the three busiest ports in England.
The modern town represents a joining of "Old Hartlepool", locally known as the "Headland", and West Hartlepool. As already mentioned, what was West Hartlepool became the larger town and both were formally unified in 1967. Today the term "West Hartlepool" is rarely heard outside the context of sport, but one of the town's Rugby Union teams still retains the name.
The name of the town's professional football club reflected both boroughs; when it was formed in 1908, following the success of West Hartlepool in winning the FA Amateur Cup in 1905, it was called "Hartlepools United" in the hope of attracting support from both towns. When the boroughs combined in 1967, the club renamed itself "Hartlepool" before re-renaming itself Hartlepool United in the 1970s. Many fans of the club still refer to the team as "Pools"
Fall out
After the war, industry went into a severe decline. Blanchland, the last ship to be constructed in Hartlepool, left the slips in 1961. In 1967, Betty James wrote how "if I had the luck to live anywhere in the North East [of England]...I would live near Hartlepool. If I had the luck". There was a boost to the retail sector in 1970 when Middleton Grange Shopping Centre was opened by Princess Anne, with over 130 new shops including Marks & Spencer and Woolworths.
Before the shopping centre was opened, the old town centre was located around Lynn Street, but most of the shops and the market had moved to a new shopping centre by 1974. Most of Lynn Street had by then been demolished to make way for a new housing estate. Only the north end of the street remains, now called Lynn Street North. This is where the Hartlepool Borough Council depot was based (alongside the Focus DIY store) until it moved to the marina in August 2006.
In 1977, the British Steel Corporation announced the closure of its Hartlepool steelworks with the loss of 1500 jobs. In the 1980s, the area was afflicted with extremely high levels of unemployment, at its peak consisting of 30 per cent of the town's working-age population, the highest in the United Kingdom. 630 jobs at British Steel were lost in 1983, and a total of 10,000 jobs were lost from the town in the economic de-industrialization of England's former Northern manufacturing heartlands. Between 1983 and 1999, the town lacked a cinema and areas of it became afflicted with the societal hallmarks of endemic economic poverty: urban decay, high crime levels, drug and alcohol dependency being prevalent.
Rise and the future
Docks near the centre were redeveloped and reopened by Queen Elizabeth II in 1993 as a marina with the accompanying National Museum of the Royal Navy opened in 1994, then known as the Hartlepool Historic Quay.
A development corporation is under consultation until August 2022 to organise projects, with the town's fund given to the town and other funds. Plans would be (if the corporation is formed) focused on the railway station, waterfront (including the Royal Navy Museum and a new leisure centre) and Church Street. Northern School of Art also has funds for a TV and film studios.
Governance
There is one main tier of local government covering Hartlepool, at unitary authority level: Hartlepool Borough Council. There is a civil parish covering Headland, which forms an additional tier of local government for that area; most of the rest of the urban area is an unparished area. The borough council is a constituent member of the Tees Valley Combined Authority, led by the directly elected Tees Valley Mayor. The borough council is based at the Civic Centre on Victoria Road.
Hartlepool was historically a township in the ancient parish of Hart. Hartlepool was also an ancient borough, having been granted a charter by King John in 1200. The borough was reformed to become a municipal borough in 1850. The council built Hartlepool Borough Hall to serve as its headquarters, being completed in 1866.
West Hartlepool was laid out on land outside Hartlepool's historic borough boundaries, in the neighbouring parish of Stranton. A body of improvement commissioners was established to administer the new town in 1854. The commissioners were superseded in 1887, when West Hartlepool was also incorporated as a municipal borough. The new borough council built itself a headquarters at the Municipal Buildings on Church Square, which was completed in 1889. An events venue and public hall on Raby Road called West Hartlepool Town Hall was subsequently completed in 1897. In 1902 West Hartlepool was elevated to become a county borough, making it independent from Durham County Council. The old Hartlepool Borough Council amalgamated with West Hartlepool Borough Council in 1967 to form a county borough called Hartlepool.
In 1974 the borough was enlarged to take in eight neighbouring parishes, and was transferred to the new county of Cleveland. Cleveland was abolished in 1996 following the Banham Review, which gave unitary authority status to its four districts, including Hartlepool. The borough was restored to County Durham for ceremonial purposes under the Lieutenancies Act 1997, but as a unitary authority it is independent from Durham County Council.
Emergency services
Hartlepool falls within the jurisdiction of Cleveland Fire Brigade and Cleveland Police. Before 1974, it was under the jurisdiction of the Durham Constabulary and Durham Fire Brigade. Hartlepool has two fire stations: a full-time station at Stranton and a retained station on the Headland.
Economy
Hartlepool's economy has historically been linked with the maritime industry, something which is still at the heart of local business. Hartlepool Dock is owned and run by PD Ports. Engineering related jobs employ around 1700 people. Tata Steel Europe employ around 350 people in the manufacture of steel tubes, predominantly for the oil industry. South of the town on the banks of the Tees, Able UK operates the Teesside Environmental Reclamation and Recycling Centre (TERRC), a large scale marine recycling facility and dry dock. Adjacent to the east of TERRC is the Hartlepool nuclear power station, an advanced gas-cooled reactor (AGR) type nuclear power plant opened in the 1980s. It is the single largest employer in the town, employing 1 per cent of the town's working age people.
The chemicals industry is important to the local economy. Companies include Huntsman Corporation, who produce titanium dioxide for use in paints, Omya, Baker Hughes and Frutarom.
Tourism was worth £48 million to the town in 2009; this figure excludes the impact of the Tall Ships 2010. Hartlepool's historic links to the maritime industry are centred on the Maritime Experience, and the supporting exhibits PS Wingfield Castle and HMS Trincomalee.
Camerons Brewery was founded in 1852 and currently employs around 145 people. It is one of the largest breweries in the UK. Following a series of take-overs, it came under the control of the Castle Eden Brewery in 2001 who merged the two breweries, closing down the Castle Eden plant. It brews a range of cask and bottled beers, including Strongarm, a 4% abv bitter. The brewery is heavily engaged in contract brewing such beers as Kronenbourg 1664, John Smith's and Foster's.
Orchid Drinks of Hartlepool were formed in 1992 after a management buy out of the soft drinks arm of Camerons. They manufactured Purdey's and Amé. Following a £67 million takeover by Britvic, the site was closed down in 2009.
Middleton Grange Shopping Centre is the main shopping location. 2800 people are employed in retail. The ten major retail companies in the town are Tesco, Morrisons, Asda, Next, Argos, Marks & Spencer, Aldi, Boots and Matalan. Aside from the local sports clubs, other local entertainment venues include a VUE Cinema and Mecca Bingo.
Companies that have moved operations to the town for the offshore wind farm include Siemens and Van Oord.
Culture and community
Festivals and Fairs
Since November 2014 the Headland has hosted the annual Wintertide Festival, which is a weekend long event that starts with a community parade on the Friday and culminating in a finale performance and fireworks display on the Sunday.
Tall Ships' Races
On 28 June 2006 Hartlepool celebrated after winning its bid to host The Tall Ships' Races. The town welcomed up to 125 tall ships in 2010, after being chosen by race organiser Sail Training International to be the finishing point for the race. Hartlepool greeted the ships, which sailed from Kristiansand in Norway on the second and final leg of the race. Hartlepool also hosted the race in July 2023.
Museums, art galleries and libraries
Hartlepool Art Gallery is located in Church Square within Christ Church, a restored Victorian church, built in 1854 and designed by the architect Edward Buckton Lamb (1806–1869). The gallery's temporary exhibitions change frequently and feature works from local artists and the permanent Fine Art Collection, which was established by Sir William Gray. The gallery also houses the Hartlepool tourist information centre.
The Heugh Battery Museum is located on the Headland. It was one of three batteries erected to protect Hartlepool's port in 1860. The battery was closed in 1956 and is now in the care of the Heugh Gun Battery Trust and home to an artillery collection.
Hartlepool is home to a National Museum of the Royal Navy (more specifically the NMRN Hartlepool). Previously known simply as The Historic Quay and Hartlepool's Maritime Experience, the museum is a re-creation of an 18th-century seaport with the exhibition centre-piece being a sailing frigate, HMS Trincomalee. The complex also includes the Museum of Hartlepool.
Willows was the Hartlepool mansion of the influential Sir William Gray of William Gray & Company and he gifted it to the town in 1920, after which it was converted to be the town's first museum and art gallery. Fondly known locally as "The Gray" it was closed as a museum in 1994 and now houses the local authority's culture department.
There are six libraries in Hartlepool, the primary one being the Community Hub Central Library. Others are Throston Grange Library, Community Hub North Library, Seaton Carew Library, Owton Manor Library and Headland Branch Library.
Sea
Hartlepool has been a major seaport virtually since it was founded, and has a long fishing heritage. During the industrial revolution massive new docks were created on the southern side of the channel running below the Headland, which gave rise to the town of West Hartlepool.
Now owned by PD Ports, the docks are still in use today and still capable of handling large vessels. However, a large portion of the former dockland was converted into a marina capable of berthing 500 vessels. Hartlepool Marina is home to a wide variety of pleasure and working craft, with passage to and from the sea through a lock.
Hartlepool also has a permanent RNLI lifeboat station.
Education
Secondary
Hartlepool has five secondary schools:
Dyke House Academy
English Martyrs School and Sixth Form College
High Tunstall College of Science
Manor Community Academy
St Hild's Church of England School
The town had planned to receive funding from central government to improve school buildings and facilities as a part of the Building Schools for the Future programme, but this was cancelled because of government spending cuts.
College
Hartlepool College of Further Education is an educational establishment located in the centre of the town, and existed in various forms for over a century. Its former 1960s campus was replaced by a £52million custom-designed building, it was approved in principle in July 2008, opened in September 2011.
Hartlepool also has Hartlepool Sixth Form College. It was a former grammar and comprehensive school, the college provides a number of AS and A2 Level student courses. The English Martyrs School and Sixth Form College also offers AS, A2 and other BTEC qualification to 16- to 18-year-olds from Hartlepool and beyond.
A campus of The Northern School of Art is a specialist art and design college and higher education, located adjacent to the art gallery on Church Square. The college has a further site in Middlesbrough that facilitates further education.
Territorial Army
Situated in the New Armoury Centre, Easington Road are the following units.
Royal Marines Reserve
90 (North Riding) Signal Squadron
Religion
They are multiple Church of England and Roman Catholic Churches in the town. St Hilda's Church is a notable church of the town, it was built on Hartlepool Abbey and sits upon a high point of the Headland. The churches of the Church of England's St Paul and Roman Catholic's St Joseph are next to each other on St Paul's Road. Nasir Mosque on Brougham Terrace is the sole purpose-built mosque in the town.
Sport
Football
Hartlepool United is the town's professional football club and they play at Victoria Park. The club's most notable moment was in 2005 when, with 8 minutes left in the 2005 Football League One play-off final, the team conceded a penalty, allowing Sheffield Wednesday to equalise and eventually beat Hartlepool to a place in the Championship. The club currently play in the National League.
Supporters of the club bear the nickname of Monkey Hangers. This is based upon a legend that during the Napoleonic wars a monkey, which had been a ship's mascot, was taken for a French spy and hanged. Hartlepool has also produced football presenter Jeff Stelling, who has a renowned partnership with Chris Kamara who was born in nearby Middlesbrough. Jeff Stelling is a keen supporter of Hartlepool and often refers to them when presenting Sky Sports News. It is also the birthplace and childhood home of Pete Donaldson, one of the co-hosts of the Football Ramble podcast as well as co-host of the Abroad in Japan podcast, and a prominent radio DJ.
The town also has a semi-professional football club called FC Hartlepool who play in Northern League Division Two.
Rugby union
Hartlepool is something of an anomaly in England having historically maintained a disproportionate number of clubs in a town of only c.90,000 inhabitants. These include(d) West Hartlepool, Hartlepool Rovers, Hartlepool Athletic RFC, Hartlepool Boys Brigade Old Boys RFC (BBOB), Seaton Carew RUFC (formerly Hartlepool Grammar School Old Boys), West Hartlepool Technical Day School Old Boys RUFC (TDSOB or Tech) and Hartlepool Old Boys' RFC (Hartlepool). Starting in 1904 clubs within eight miles (thirteen kilometres) of the headland were eligible to compete for the Pyman Cup which has been contested regularly since and that the Hartlepool & District Union continue to organise.
Perhaps the best known club outside the town is West Hartlepool R.F.C. who in 1992 achieved promotion to what is now the Premiership competing in 1992–93, 1994–95, 1995–96 and 1996–97 seasons. This success came at a price as soon after West was then hit by bankruptcy and controversially sold their Brierton Lane stadium and pitch to former sponsor Yuills Homes. There then followed a succession of relegations before the club stabilised in the Durham/Northumberland leagues. West and Rovers continue to play one another in a popular Boxing Day fixture which traditionally draws a large crowd.
Hartlepool Rovers, formed in 1879, who played at the Old Friarage in the Headland area of Hartlepool before moving to West View Road. In the 1890s Rovers supplied numerous county, divisional and international players. The club itself hosted many high-profile matches including the inaugural Barbarians F.C. match in 1890, the New Zealand Maoris in 1888 and the legendary All Blacks who played against a combined Hartlepool Club team in 1905. In the 1911–12 season, Hartlepool Rovers broke the world record for the number of points scored in a season racking up 860 points including 122 tries, 87 conversions, five penalties and eleven drop goals.
Although they ceased competing in the RFU leagues in 2008–09, West Hartlepool TDSOB (Tech) continues to support town and County rugby with several of the town's other clubs having played at Grayfields when their own pitches were unavailable. Grayfields has also hosted a number of Durham County cup finals as well as County Under 16, Under 18 and Under 20 age group games.
Olympics
Boxing
At the 2012 Summer Olympics, 21-year-old Savannah Marshall, who attended English Martyrs School and Sixth Form College in the town of Hartlepool, competed in the Women's boxing tournament of the 2012 Olympic Games. She was defeated 12–6 by Marina Volnova of Kazakhstan in her opening, quarter-final bout. Savannah Marshall is now a professional boxer, currently unbeaten as a pro and on 31 October 2020 in her 9th professional fight Marshall became the WBO female middleweight champion with a TKO victory over opponent Hannah Rankin at Wembley Arena.
Swimming
In August 2012 Jemma Lowe, a British record holder who attended High Tunstall College of Science in the town of Hartlepool, competed in the 2012 Olympic Games. She finished sixth in the 200-metre butterfly final with a time of 58.06 seconds. She was also a member of the eighth-place British team in the 400m Medley relay.
Monkeys
Hartlepool is known for allegedly executing a monkey during the Napoleonic Wars. According to legend, fishermen from Hartlepool watched a French warship founder off the coast, and the only survivor was a monkey, which was dressed in French military uniform, presumably to amuse the officers on the ship. The fishermen assumed that this must be what Frenchmen looked like and, after a brief trial, summarily executed the monkey.
Historians have pointed to the prior existence of a Scottish folk song called "And the Boddamers hung the Monkey-O". It describes how a monkey survived a shipwreck off the village of Boddam near Peterhead in Aberdeenshire. Because the villagers could only claim salvage rights if there were no survivors from the wreck, they allegedly hanged the monkey. There is also an English folk song detailing the later event called, appropriately enough, "The Hartlepool Monkey". In the English version the monkey is hanged as a French spy.
"Monkey hanger" and Chimp Choker are common terms of (semi-friendly) abuse aimed at "Poolies", often from footballing rivals Darlington. The mascot of Hartlepool United F.C. is H'Angus the monkey. The man in the monkey costume, Stuart Drummond, stood for the post of mayor in 2002 as H'angus the monkey, and campaigned on a platform which included free bananas for schoolchildren. To widespread surprise, he won, becoming the first directly elected mayor of Hartlepool, winning 7,400 votes with a 52% share of the vote and a turnout of 30%. He was re-elected by a landslide in 2005, winning 16,912 on a turnout of 51% – 10,000 votes more than his nearest rival, the Labour Party candidate.
The monkey legend is also linked with two of the town's sports clubs, Hartlepool Rovers RFC, which uses the hanging monkey as the club logo. Hartlepool (Old Boys) RFC use a hanging monkey kicking a rugby ball as their tie crest.
Notable residents
Michael Brown, former Premier League footballer
Edward Clarke, artist
Brian Clough, football manager who lived in the Fens estate in town while manager of Hartlepools United
John Darwin, convicted fraudster who faked his own death
Pete Donaldson, London radio DJ and podcast host
Janick Gers, guitarist from British heavy metal band Iron Maiden
Courtney Hadwin, singer
Jack Howe, former England international footballer
Liam Howe, music producer and songwriter for several artists and member of the band Sneaker Pimps
Saxon Huxley, WWE NXT UK wrestler
Andy Linighan, former Arsenal footballer who scored the winning goal in the 1993 FA Cup Final
Savannah Marshall, professional boxer
Stephanie Aird, comedian and television personality
Jim Parker, composer
Guy Pearce, film actor who lived in the town when he was younger as his mother was from the town
Narbi Price, artist
Jack Rowell, coached the England international rugby team and led them to the semi-final of the 1995 Rugby World Cup
Wayne Sleep, dancer and actor who spent his childhood in the town.
Reg Smythe, cartoonist who created Andy Capp
Jeremy Spencer, guitarist who was in the original Fleetwood Mac line-up
Jeff Stelling, TV presenter, famous for hosting Gillette Soccer Saturday
David Eagle, Folk singer and stand-up comedian,
Local media
Hartlepool Life - local free newspaper
Hartlepool Mail – local newspaper
BBC Radio Tees – BBC local radio station
Radio Hartlepool – Community radio station serving the town
Hartlepool Post – on-line publication
Local television news programmes are BBC Look North and ITV News Tyne Tees.
Town twinning
Hartlepool is twinned with:
France Sète, France
Germany Hückelhoven, Germany (since 1973)
United States Muskegon, Michigan
Malta Sliema, Malta
Features from a bound volume of Australian Women's Budget Magazine, dated July-December 1913. Read more on the blog: chronicallysiobhan.wordpress.com/2016/12/07/a-glimpse-int...
REYKJAVIK, ICELAND - APRIL 7: Tomoaki "crow" Maruoka of team ZETA DIVISION poses for the VALORANT Masters Features Day on April 7, 2022 in Reykjavik, Iceland. (Photo by Lance Skundrich/Riot Games)
The Sea Rabbit (Monafluffchus americanus) of Coney Island, Brooklyn, New York – This unique sea-dwelling rabbit, which is actually a close relative of the sea lion, was officially discovered and investigated by Henry Hudson when he first visited this land to colonize the area by order of the Dutch government. It was named New Amsterdam -- today’s New York City. This island was named after he saw the beach covered with strange swimming wild rabbits. The word “Coney Island” means “wild rabbit island” in Dutch (originally Conyne Eylandt, or Konijneneiland in modern Dutch spelling). Sea rabbits were also referred mermaid rabbit, merrabbit, rabbit fish or seal rabbit in the natural history documents in the 17th century. The current conservation status, or risk of extinction, of the sea rabbit is Extinct in the Wild.
This website features two species of sea rabbits, which have been taken care of by Dr. Takeshi Yamada (山田武司) at the Coney Island Sea Rabbit Repopulation Center, which is a part of the Marine biology department of the Coney Island University in Brooklyn, New York. They are – Coney Island Sea Rabbit (Monafluffchus americanus) called “Seara” and Coney Island Tiger-striped Sea Rabbit (Monafluffchus konjinicus) called “Stripes”.
The photographs and videos featured in this website chronicle adventures of the Coney Island sea rabbits and the world as seen by them. This article also documented efforts of Dr. Takeshi Yamada for bringing back the nearly extinct sea rabbits to Coney Island in the City of New York and beyond. Dr. Yamada produced a series of public lectures, workshops, original public live interactive fine art performances and fine art exhibitions about sea rabbits at a variety of occasions and institutions in the City of New York and beyond. Dr. Yamada is an internationally active educator, book author, wildlife conservationist and high profile artist, who lives and works in Brooklyn, New York.
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Sea Rabbit
Other Common Names: Coney Island Sea Rabbit, Beach Rabbit, Seal Rabbit, mer-rabbit, merrabbit, Atlantic Sea Rabbit.
Latin Name: Monafluffchus americanus
Origin: Atlantic coast of the United States
Description of the specimen: In the early 17th century’s European fur craze drove the fleet of Dutch ships to the eastern costal area of America. Then Holland was the center of the world just like the Italy was in the previous century. New York City was once called New Amsterdam when Dutch merchants landed and established colonies. Among them, Henry Hudson is probably the most recognized individual in the history of New York City today. “This small island is inhabited by two major creatures which we do not have in our homeland. The one creature is a large arthropod made of three body segments: the frontal segment resembles a horseshoe, the middle segment resembles a spiny crab and its tail resembles a sharp sword. Although they gather beaches here in great numbers, they are not edible due to their extremely offensive odor. Another creature which is abundant here, has the head of wild rabbit. This animal of great swimming ability has frontal legs resemble the webbed feet of a duck. The bottom half of the body resembles that of a seal. This docile rabbit of the sea is easy to catch as it does not fear people. The larger male sea rabbits control harems of 20 to 25 females. The meat of the sea rabbit is very tender and tasty.” This is what Hadson wrote in his personal journal in 1609 about the horseshoe crab and the sea rabbit in today’s Coney Island area of Brooklyn, New York. Sadly, just like the Dodo bird and the Thylacine, the sea rabbit was driven to extinction by the European settlers’ greed. When Dutch merchants and traders arrived here, sea rabbits were one of the first animals they hunted down to bring their furs to homeland to satisfy the fur craze of the time. To increase the shipment volume of furs of sea rabbit and beavers from New Amsterdam, Dutch merchants also started using wampum (beads made of special clam shells) as the first official currency of this country.
At the North Eastern shores of the United States, two species of sea rabbits were commonly found. They are Coney Island Sea Rabbit (Monafluffchus americanus) and Coney Island Tiger-striped Sea Rabbit (Monafluffchus konjinicus). Sadly, due to their over harvesting in the previous centuries, their conservation status became “Extinct in the Wild” (ET) in the Red List Endangered species by the International Union for Conservation of Nature (IUCN). Currently, these sea rabbits are only found at breeding centers at selected zoos and universities such as Coney Island Aquarium and Coney Island University in Brooklyn, New York. The one shown in this photograph was named "Seara" and has been cared by Dr. Takeshi Yamada at Coney Island University.
The sea rabbit is one of the families of the Pinniped order. Pinnipeds (from Latin penna = flat and pes/pedis = foot) are sea-mammals: they are homeothermic (i.e having high and regulated inner temperature), lung-breathing (i.e dependant on atmospheric oxygen) animals having come back to semi aquatic life. As soon as they arrive ashore, females are caught by the nearest adult male. Males can maintain harems of about 20 females on average. Several hours to several days after arriving ashore, pregnant females give birth to eight to ten pups with a dark brown fur. As soon as birth occurs, the mother’s special smell and calls help her pups bond specifically to her. The mother stays ashore with her pup for about one week during which the pup gains weight. During the first week spent with her newborn, the mother becomes receptive. She will be impregnated by the bull, which control the harem. Implantation of the embryo will occur 3 months later, in March-April. During the reproductive period, the best males copulate with several tens females. To do so, males have to stay ashore without feeding in order to keep their territory and their harem. In mid-January, when the last females have been fecundated, males leave at sea to feed. Some of them will come back later in March-April for the moult. The other ones will stay at sea and will come back on Coney Island only in next November. After fecundation, the mother goes at sea for her first meal. At sea, mothers feed on clams, crabs, shrimps, fish (herring, anchovy, Pollock, capelin etc.) and squids. When she is back, the mother recovers her pups at the beach she left them. Suckling occurs after auditive and olfactory recognition had occured. In March-April, the dark brown fur is totally replaced by an adult-like light brownish grey fur during the moult that lasts 1-2 months. This new fur is composed by 2 layers. Externally, the guard fur is composed by flat hairs that recover themselves when wet. By doing so, they make a water-proof barrier for the under fur. The underfur retains air when the seal is dry. Because of isolating properties of the air, the underfur is the insulating system of the fur. In March-April, the fur of adults is partially replaced. First reproduction occurs at 1-yr old in females. Males are physiologically matures at 1 year old but socially matures at +2 years old.
NOTE: The name of Coney Island is commonly thought to be derived from the Dutch Konijn Eylandt or Rabbit Island as apparently the 17th century European settlers noted many rabbits running amuck on the island.
www.takeshiyamada.weebly.com/performances.html
www.takeshiyamada.weebly.com/sea-rabbit-center.html
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www.flickr.com/photos/searabbit24/
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www.flickr.com/photos/diningwithsearabbits03
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www.flickr.com/photos/yamadaimmortalized2/
www.flickr.com/photos/takeshiyamadaimmortalized/
www.flickr.com/photos/yamadabellhouse2014/
www.flickr.com/photos/museumofworldwonders3/
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www.flickr.com/photos/museumofworldwonders/
www.flickr.com/photos/takeshiyamadapaintings/
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For any questions, please email contact Takeshi Yamada, Art & Rogue Taxidermy, Museum of World Wonders, official website. www.takeshiyamada.weebly.com/
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For any questions, please contact Dr. Takeshi Yamada. His email address is posted in the chapter page (the last page or the first page).
(Updated May 25, 2015)
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.
Taken around 2004 on a Minolta DimargeX compact camera.
This is the form work I made to create the circular "brickwork".
Pembroke is a town and community in Pembrokeshire, Wales, with a population of 7,552. The names of both the town and the county (of which the county town is Haverfordwest) have a common origin; both are derived from the Cantref of Penfro: Pen, "head" or "end", and bro, "region", "country", "land", which has been interpreted to mean either "Land's End" or "headland".
Pembroke features a number of historic buildings, town walls, complexes and Pembroke Castle which was the birthplace of Henry Tudor, who became Henry VII of England.
Pembroke Castle, the substantial remains of a stone medieval fortress founded by the Normans in 1093, stands at the western tip of a peninsula surrounded by water on three sides. The castle was the seat of the powerful Earls of Pembroke and the birthplace of King Henry VII of England. Gerald de Windsor was the first recorded Constable of Pembroke. Pembroke town and castle and its surroundings are linked with the early Christian church. Following the final extension of the castle about 1254 the town was extended and defensive perimeter walls erected around the edge of the town. The walls survive on their medieval foundations, although much rebuilt over the centuries. A great many of the town's original medieval burgage plots survive and are divided by early stone walls that are of significant national importance.
Monkton Priory, sited on a hill across the river from the castle, founded in 1098 by Arnulf de Montgomery and granted by him to the Benedictine order, has very early foundations and retains much of the Norman walls of the nave. The choir and sanctuary were renovated in the nineteenth century. Monkton Hall, close by the Priory church, is regarded as the oldest domestic building in Pembrokeshire and possibly Wales and is thought to have been the guesthouse for visitors to the Priory.
The first stone building in the town was a defensive tower, now known as the Medieval Chapel, at 69a Main Street and built on a cliff edge. There are the remains of a great hall to the north and recently filled-in arched cellars. The building was thought to have been later used as an early church as the layout is the same as St. Govan's Chapel and was used by John Wesley in 1764 to preach Methodism. In 1866 it became the brewery for the York Tavern which was briefly Oliver Cromwell's headquarters at the end of the Siege of Pembroke during the English Civil War.
The town's main bridge across the River Pembroke, which also acts as a dam, crosses and constrains the millpond. The first bridge was constructed to house a tide mill, originally granted to the Knight's Templar in 1199. The last mill building was destroyed by fire in 1956.
On both banks of the Pembroke River to the west of the castle are many remains of early activities. The North Shore Quarries are relatively complete as are the remains of medieval and Elizabethan slipways where wooden vessels were built before the industrial dockyard and admiralty town was built on the grid pattern of Pembroke Dock. There is a very early complete graving dock in what was Hancock's Yard.
During the English Civil War, the strategic maritime shire was primarily in the control of the parliamentary forces which aspired to prevent communication to Ireland.
At Pennar Flats there was an early submarine base used for experiments in submarine warfare. Three of the houses on the then foreshore, part of the shipyard before the Admiralty Dock Yard was built, are still standing but are heavily altered.[citation needed]
The ferry port of Pembroke Dock is 3 miles (4.8 km) to the northwest of Pembroke. It was established in 1814.
Pembroke town stands on the South Pembrokeshire limestone peninsula by the estuary of the River Cleddau, flanked on all sides by woodland and arable farmland. The town is 8 miles (13 km) south of the county town of Haverfordwest.
The town is centred on Main Street, which is the only street that is inside the original Pembroke town walls. Outside the walls, residential estates have been built to the north towards Pembroke Dock, to the east towards Lamphey, and to the south. To the west of the town lies the village of Monkton, which is included as part of the community of Pembroke. At the 2001 census, the community had a population of 7,214.
The conurbation of Pembroke Dock and Pembroke has a combined population of 15,890 and as such is one of the major population centres of West Wales.
There are two tiers of local government covering Pembroke, at community (town) and county level: Pembroke Town Council and Pembrokeshire County Council. Pembroke Town Council is based at Pembroke Town Hall. The community of Pembroke covers an area of 4.58 square miles (1,190 ha) and includes the Pembroke St Mary North, St Mary South, St Michael and Monkton wards.
For representation on the county council, the four wards comprising Pembroke community each elect one councillor.
Pembroke is part of the Carmarthen West and South Pembrokeshire Senedd constituency and UK Parliamentary constituency.
The local Member of Parliament (MP) is Simon Hart, a Conservative.
Pembroke was an ancient borough, with evidence of borough charters dating back to at least 1168. The borough covered the two parishes of Pembroke St Mary and Pembroke St Michael plus part of the parish of Monkton (also known as Pembroke St Nicholas). The borough was reformed to become a municipal borough in 1836. The borough included a sizeable rural area within its boundaries as well as the built up area of Pembroke itself. The town of Pembroke Dock, which developed from the early nineteenth century as a separate urban area was nevertheless within the borough boundaries of Pembroke, falling within the parish of Pembroke St Mary. The part of the parish of Monkton outside the borough boundaries became a separate parish called Hundleton in 1894.
As Pembroke Dock grew through the nineteenth century it began to rival the old town of Pembroke for position as the main settlement within the borough. By 1895 Pembroke Borough Council had adopted the practice of holding its meetings alternately at Pembroke Town Hall and at Pembroke Dock, where the council had established its main administrative offices at 37 Bush Street (renumbered 71 Bush Street in 1906). The council remained based at 71 Bush Street (and later also expanded into neighbouring 73 Bush Street) until the early 1970s when it acquired Llanion Park, part of the Llanion Barracks at Pembroke Dock, to serve as its headquarters.
Pembroke Borough Council was abolished under the Local Government Act 1972, with the area becoming part of the new district of South Pembrokeshire within the county of Dyfed on 1 April 1974. A community was established to cover the area of the former borough, with its council taking the name Pembroke Town Council. South Pembrokeshire District Council took over Llanion Park at Pembroke Dock to serve as its headquarters.
On 1 April 1986 the community of Pembroke was split into a Pembroke Dock community and a reduced Pembroke community, with Pembroke Town Council thereafter just covering the old town of Pembroke itself.
South Pembrokeshire was abolished in 1996, with the area becoming part of a re-established Pembrokeshire.
Primary and pre-school (ages 3–11) education in Pembroke is served by two state schools. In Pembroke town, Golden Grove CP School is a dual stream school established in 2002 following the amalgamation of Golden Manor Infants School and Grove Junior School. In Monkton, pupils can attend Monkton Priory CP School.
Secondary education is provided by Pembroke School (in Welsh: Ysgol Benfro), a mixed 11–18 comprehensive school of 1,600 pupils with a sixth form of about 200. The school was formed in 1972 as a result of the amalgamation of the former grammar school and secondary modern school. The school takes pupils from the Pembroke family of schools, which as well as Golden Grove and Monkton Priory includes community primary schools in Lamphey, Orielton, Pennar and Pembroke Dock, voluntary controlled primary schools in Angle, Cosheston and Stackpole, and St. Mary's Catholic Primary School in Pembroke Dock.
Pembroke 21C community association was founded in 2004, and is based out of the Foundry House building on the Commons, which they operate as a community centre. Activities carried out by 21C include organising the annual Pembroke Festival, running the town's fortnightly farmers' market and producing a quarterly newsletter which is distributed to all households in the town. Pembroke Rugby Club organises the town's annual carnival, which is usually held in June. Pembroke Library shares a building with the Tourist Information Centre on Commons Road and offers a full lending service and internet access.
Pembroke has been twinned with the towns of Bergen, Lower Saxony, Germany, since 1977 and Pembroke, Malta, since 2002.
Notable people
King Henry VII (1457–1509), King of England, born in Pembroke Castle.
William Lort Mansel (1753–1820), an English churchman and Cambridge fellow.
Frank Goodden (1889–1917), a pioneering British aviator and test pilot
Mervyn Johns (1899–1992), a Welsh stage, film and TV character actor.
W. F. Grimes CBE (1905–1988), a Welsh archaeologist, studied the prehistory of Wales.
Daniel Jones, OBE (1912–1993), a Welsh composer of classical music.
John Cooke CB, OBE (1922–2011), a British doctor and senior Royal Air force officer.
Peter Bishop (1953–2022), an English painter of mountain landscape of north Wales and an art historian.
Sport
William Bowen (1862–1925), a Welsh international rugby union player, capped 13 times for Wales.
Henry Davies (1865–1934), a Welsh horse racing jockey and first-class cricketer.
W. J. A. Davies OBE (1890–1967), a Welsh rugby union footballer, capped 22 times for England
Reg Thomas (1907–1946), a Welsh middle-distance runner, he competed at the 1928 and 1932 Summer Olympics
David Gwynne-James (1937−2011), a Welsh first-class cricketer, British Army officer and military historian.
Scott Gammer (born 1976), a Welsh former professional boxer, British heavyweight title-holder from 2006 to 2007
Jonathan Thomas (born 1982), a Welsh rugby union coach and former player, capped 67 times for Wales.
Pembroke Rugby Club is on Upper Lamphey Road. The ground is called Crickmarren. The club plays in WRU Division Five West. Pembroke's main game of the season is often the local derby with rivals the Pembroke Dock Harlequins. Pembroke produced Ospreys and Welsh international Jonathan Thomas, Welsh international Dominic Day and Scotland international Luke Hamilton.
Other sporting clubs in the area include the football team Monkton Swifts.
The town is home to Pembroke Cricket Club. The cricket club plays its home games at its Treleet ground on Upper Lamphey Road, opposite the rugby club. The club currently has a 1st and a 2nd team playing in divisions 2 and 4 of the Pembrokeshire league. The club colours are green and gold.
In February 2012, it was revealed that Pembroke was the UK's second-slowest broadband town. The average internet download speed in Pembroke was just over 1.6 Mbit/s (1600 kbit/s) compared to the UK average of 12.0 Mbit/s (12000 kbit/s) at the time.
BT's telephone exchange, which serves Pembroke and Pembroke Dock, was upgraded in 2014 under the Superfast Cymru programme and new cabinets were built to provide FTTC technology. Additional exchanges across Pembrokeshire are also being upgraded under the programme, with a goal of bringing superfast broadband to 96% of Wales by spring 2016.
Pembrokeshire is a county in the south-west of Wales. It is bordered by Carmarthenshire to the east, Ceredigion to the northeast, and is otherwise surrounded by the sea. Haverfordwest is the largest town and administrative headquarters of Pembrokeshire County Council.
The county is generally sparsely populated and rural, with an area of 200 square miles (520 km2) and a population of 123,400. After Haverfordwest, the largest settlements are Milford Haven (13,907), Pembroke Dock (9,753), and Pembroke (7,552). St Davids (1,841) is a city, the smallest by population in the UK. Welsh is spoken by 17.2 percent of the population, and for historic reasons is more widely spoken in the north of the county than in the south.
Pembrokeshire's coast is its most dramatic geographic feature, created by the complex geology of the area. It is a varied landscape which includes high sea cliffs, wide sandy beaches, the large natural harbour of Milford Haven, and several offshore islands which are home to seabird colonies. Most of it is protected by Pembrokeshire Coast National Park, and can be hiked on the 190-mile (310 km) Pembrokeshire Coast Path. The interior of Pembrokeshire is relatively flat and gently undulating, with the exception of the Preseli Mountains in the north.
There are many prehistoric sites in Pembrokeshire, particularly in the Preseli Mountains. During the Middle Ages several castles were built by the Normans, such as Pembroke and Cilgerran, and St David's Cathedral became an important pilgrimage site. During the Industrial Revolution the county remained relatively rural, with the exception of Milford Haven, which was developed as a port and Royal Navy dockyard. It is now the UK's third-largest port, primarily because of its two liquefied natural gas terminals. The economy of the county is now focused on agriculture, oil and gas, and tourism.
Human habitation of the region that is now Pembrokeshire extends back to between 125,000 and 70,000 years and there are numerous prehistoric sites such as Pentre Ifan, and neolithic remains (12,000 to 6,500 years ago), more of which were revealed in an aerial survey during the 2018 heatwave; in the same year, a 1st-century Celtic chariot burial was discovered, the first such find in Wales. There may have been dairy farming in Neolithic times.
There is little evidence of Roman occupation in what is now Pembrokeshire. Ptolemy's Geography, written c. 150, mentioned some coastal places, two of which have been identified as the River Teifi and what is now St Davids Head, but most Roman writers did not mention the area; there may have been a Roman settlement near St Davids and a road from Bath, but this comes from a 14th-century writer. Any evidence for villas or Roman building materials reported by mediaeval or later writers has not been verified, though some remains near Dale were tentatively identified as Roman in character by topographer Richard Fenton in his Historical Tour of 1810. Fenton stated that he had "...reason to be of opinion that they had not colonized Pembrokeshire till near the decline of their empire in Britain".
Part of a possible Roman road is noted by CADW near Llanddewi Velfrey, and another near Wiston. Wiston is also the location of the first Roman fort discovered in Pembrokeshire, investigated in 2013.
Some artefacts, including coins and weapons, have been found, but it is not clear whether these belonged to Romans or to a Romanised population. Welsh tradition has it that Magnus Maximus founded Haverfordwest, and took a large force of local men on campaign in Gaul in 383 which, together with the reduction of Roman forces in south Wales, left a defensive vacuum which was filled by incomers from Ireland.
Between 350 and 400, an Irish tribe known as the Déisi settled in the region known to the Romans as Demetae. The Déisi merged with the local Welsh, with the regional name underlying Demetae evolving into Dyfed, which existed as an independent petty kingdom from the 5th century. In 904, Hywel Dda married Elen (died 943), daughter of the king of Dyfed Llywarch ap Hyfaidd, and merged Dyfed with his own maternal inheritance of Seisyllwg, forming the new realm of Deheubarth ("southern district"). Between the Roman and Norman periods, the region was subjected to raids from Vikings, who established settlements and trading posts at Haverfordwest, Fishguard, Caldey Island and elsewhere.
Dyfed remained an integral province of Deheubarth, but this was contested by invading Normans and Flemings who arrived between 1067 and 1111. The region became known as Pembroke (sometimes archaic "Penbroke":), after the Norman castle built in the cantref of Penfro. In 1136, Prince Owain Gwynedd at Crug Mawr near Cardigan met and destroyed a 3,000-strong Norman/Flemish army and incorporated Deheubarth into Gwynedd. Norman/Flemish influence never fully recovered in West Wales. In 1138, the county of Pembrokeshire was named as a county palatine. Rhys ap Gruffydd, the son of Owain Gwynedd's daughter Gwenllian, re-established Welsh control over much of the region and threatened to retake all of Pembrokeshire, but died in 1197. After Deheubarth was split by a dynastic feud, Llywelyn the Great almost succeeded in retaking the region of Pembroke between 1216 and his death in 1240. In 1284 the Statute of Rhuddlan was enacted to introduce the English common law system to Wales, heralding 100 years of peace, but had little effect on those areas already established under the Marcher Lords, such as Cemais in the north of the county.
Henry Tudor, born at Pembroke Castle in 1457, landed an army in Pembrokeshire in 1485 and marched to Cardigan. Rallying support, he continued to Leicestershire and defeated the larger army of Richard III at the Battle of Bosworth Field. As Henry VII, he became the first monarch of the House of Tudor, which ruled England until 1603.
The Laws in Wales Act 1535 effectively abolished the powers of the Marcher Lords and divided the county into seven hundreds, roughly corresponding to the seven pre-Norman cantrefi of Dyfed. The hundreds were (clockwise from the northeast): Cilgerran, Cemais, Dewisland, Roose, Castlemartin, Narberth and Dungleddy and each was divided into civil parishes; a 1578 map in the British Library is the earliest known to show parishes and chapelries in Pembrokeshire. The Elizabethan era brought renewed prosperity to the county through an opening up of rural industries, including agriculture, mining and fishing, with exports to England and Ireland, though the formerly staple woollen industry had all but disappeared.
During the First English Civil War (1642–1646) the county gave strong support to the Roundheads (Parliamentarians), in contrast to the rest of Wales, which was staunchly Royalist. In spite of this, an incident in Pembrokeshire triggered the opening shots of the Second English Civil War when local units of the New Model Army mutinied. Oliver Cromwell defeated the uprising at the Siege of Pembroke in July 1648. On 13 August 1649, the Cromwellian conquest of Ireland began when New Model Army forces sailed from Milford Haven.
In 1720, Emmanuel Bowen described Pembrokeshire as having five market towns, 45 parishes and about 4,329 houses, with an area of 420,000 acres (1,700 km2). In 1791 a petition was presented to the House of Commons concerning the poor state of many of the county's roads, pointing out that repairs could not be made compulsory by the law as it stood. The petition was referred to committee. People applying for poor relief were often put to work mending roads. Workhouses were poorly documented. Under the Poor Laws, costs and provisions were kept to a minimum, but the emphasis was often on helping people to be self-employed. While the Poor Laws provided a significant means of support, there were many charitable and benefit societies. After the Battle of Fishguard, the failed French invasion of 1797, 500 French prisoners were held at Golden Hill Farm, Pembroke. From 1820 to 1878 one of the county's prisons, with a capacity of 86, was in the grounds of Haverfordwest Castle. In 1831, the area of the county was calculated to be 345,600 acres (1,399 km2) with a population of 81,424.
It was not until nearly the end of the 19th century that mains water was provided to rural south Pembrokeshire by means of a reservoir at Rosebush and cast iron water pipes throughout the district.
Throughout much of the 20th century (1911 to 1961) the population density in the county remained stable while it rose in England and Wales as a whole. There was considerable military activity in Pembrokeshire and offshore in the 20th century: a naval base at Milford Haven because German U-boats were active off the coast in World War I and, in World War II, military exercises in the Preseli Mountains and a number of military airfields. The wartime increase in air activity saw a number of aircraft accidents and fatalities, often due to unfamiliarity with the terrain. From 1943 to 1944, 5,000 soldiers from the United States Army's 110th Infantry Regiment were based in the county, preparing for D-Day. Military and industrial targets in the county were subjected to bombing during World War II. After the end of the war, German prisoners of war were accommodated in Pembrokeshire, the largest prison being at Haverfordwest, housing 600. The County of Pembroke War Memorial in Haverfordwest carries the names of 1,200 of those that perished in World War I.
In 1972, a second reservoir for south Pembrokeshire, at Llys y Fran, was completed.
Pembrokeshire's tourism portal is Visit Pembrokeshire, run by Pembrokeshire County Council. In 2015 4.3 million tourists visited the county, staying for an average of 5.24 days, spending £585 million; the tourism industry supported 11,834 jobs. Many of Pembrokeshire's beaches have won awards, including Poppit Sands and Newport Sands. In 2018, Pembrokeshire received the most coast awards in Wales, with 56 Blue Flag, Green Coast or Seaside Awards. In the 2019 Wales Coast Awards, 39 Pembrokeshire beaches were recognised, including 11 awarded Blue Flag status.
The Pembrokeshire coastline is a major draw to tourists; in 2011 National Geographic Traveller magazine voted the Pembrokeshire Coast the second best in the world and in 2015 the Pembrokeshire Coast National Park was listed among the top five parks in the world by a travel writer for the Huffington Post. Countryfile Magazine readers voted the Pembrokeshire Coast the top UK holiday destination in 2018, and in 2019 Consumers' Association members placed Tenby and St Davids in the top three best value beach destinations in Britain. With few large urban areas, Pembrokeshire is a "dark sky" destination. The many wrecks off the Pembrokeshire coast attract divers. The decade from 2012 saw significant, increasing numbers of Atlantic bluefin tuna, not seen since the 1960s, and now seen by some as an opportunity to encourage tourist sport fishing.
The county has a number of theme and animal parks (examples are Folly Farm Adventure Park and Zoo, Manor House Wildlife Park, Blue Lagoon Water Park and Oakwood Theme Park), museums and other visitor attractions including Castell Henllys reconstructed Iron Age fort, Tenby Lifeboat Station and Milford Haven's Torch Theatre. There are 21 marked cycle trails around the county.
Pembrokeshire Destination Management Plan for 2020 to 2025 sets out the scope and priorities to grow tourism in Pembrokeshire by increasing its value by 10 per cent in the five years, and to make Pembrokeshire a top five UK destination.
As the national sport of Wales, rugby union is widely played throughout the county at both town and village level. Haverfordwest RFC, founded in 1875, is a feeder club for Llanelli Scarlets. Village team Crymych RFC in 2014 plays in WRU Division One West. There are numerous football clubs in the county, playing in five leagues with Haverfordwest County A.F.C. competing in the Cymru Premier.
Triathlon event Ironman Wales has been held in Pembrokeshire since 2011, contributing £3.7 million to the local economy, and the county committed in 2017 to host the event for a further five years. Ras Beca, a mixed road, fell and cross country race attracting UK-wide competitors, has been held in the Preselis annually since 1977. The record of 32 minutes 5 seconds has stood since 1995. Pembrokeshire Harriers athletics club was formed in 2001 by the amalgamation of Cleddau Athletic Club (established 1970) and Preseli Harriers (1989) and is based in Haverfordwest.
The annual Tour of Pembrokeshire road-cycling event takes place over routes of optional length. The 4th Tour, in April 2015, attracted 1,600 riders including Olympic gold medallist Chris Boardman and there were 1,500 entrants to the 2016 event. Part of Route 47 of the Celtic Trail cycle route is in Pembrokeshire. The Llys y Fran Hillclimb is an annual event run by Swansea Motor Club, and there are several other county motoring events held each year.
Abereiddy's Blue Lagoon was the venue for a round of the Red Bull Cliff Diving World Series in 2012, 2013, and 2016; the Welsh Surfing Federation has held the Welsh National Surfing Championships at Freshwater West for several years, and Llys y Fran Country Park hosted the Welsh Dragonboat Championships from 2014 to 2017.
While not at major league level, cricket is played throughout the county and many villages such as Lamphey, Creselly, Llangwm, Llechryd and Crymych field teams in minor leagues under the umbrella of the Cricket Board of Wales.
Notable people
From mediaeval times, Rhys ap Gruffydd (c. 1132-1197), ruler of the kingdom of Deheubarth, was buried in St Davids Cathedral. and Gerald of Wales was born c. 1146 at Manorbier Castle. Henry Tudor (later Henry VII) was born in 1457 at Pembroke Castle.
The pirate Bartholomew Roberts (Black Bart) (Welsh: Barti Ddu) was born in Casnewydd Bach, between Fishguard and Haverfordwest in 1682.
In later military history, Jemima Nicholas, heroine of the so-called "last invasion of Britain" in 1797, was from Fishguard, Lieutenant General Sir Thomas Picton GCB, born in Haverfordwest, was killed at the Battle of Waterloo in 1815 and Private Thomas Collins is believed to be the only Pembrokeshire man that fought in the Battle of Rorke's Drift in 1879.
In the arts, siblings Gwen and Augustus John were both born in Pembrokeshire, as was the novelist Sarah Waters; singer Connie Fisher grew up in Pembrokeshire. The actor Christian Bale was born in Haverfordwest.
Stephen Crabb, a former Secretary of State for Work and Pensions and Secretary of State for Wales, was brought up in Pembrokeshire and is one of the county's two Members of Parliament, the other being Simon Hart,[90] who served as Secretary of State for Wales from 2019 to 2022.
Qing features the new third generation athletic Inamorata doll body, Chie head sculpt and Caramel resin tone. I've done three photoshoots with this versatile girl: A 30's Retro Shanghai, modern girl in Taipei and a exotic look in Tokyo. This little globetrotter is on her way to her new home, but I did enjoy her company.
The de Havilland DH.88 Comet was a twin-engined British aircraft designed for the 1934 MacRobertson Air Race. Three examples took part in the race and one of them won it. The type set many aviation records during the race and afterwards, as a pioneer mail plane. The modern features and clean lines of the DH.88, especially in the striking colours of Grosvenor House (shown here), the race winner, make it a true design classic.
Three orders were indeed received, and de Havilland set to work. The airframe consisted of a wooden skeleton clad with spruce plywood, with a final fabric covering on the wings. A long streamlined nose held the main fuel tanks, with the low-set and fully glazed central two-seat cockpit faired into an unbroken line to the tail. The wings were of a thin cantilever monoplane design for high-speed flight, and as such would require stressed-skin construction to achieve sufficient strength. While other designers were turning to metal to provide this extra strength, de Havilland took the unusual approach of increasing the strength of all-wood construction. De Havilland achieved the skin profile using many thin, shaped pieces set side by side, and then overlaid in the manner of plywood. This was made possible only by the recent discovery of high-strength synthetic bonding resins and its success took many in the industry by surprise.
The engines were uprated versions of the standard Gipsy Six, being tuned for best performance with a higher compression ratio. The DH.88 could maintain altitude up to 4,000 ft (1,200 m) on one engine. The propellers were two-position variable pitch, manually set to fine before takeoff using a bicycle pump and changed automatically to coarse by a pressure sensor. The main undercarriage retracted upwards and backwards into the engine nacelles, while the tailskid did not retract. Later examples and rebuilds would feature a castoring tail wheel.
The DH.88 might have been the only wooden British high-performance monoplane, but for a shortage of metal for aircraft construction during the Second World War. Experience with the DH.88 would later be put to use in designing the DH.98 Mosquito, also a twin-engined monoplane of wooden construction. The Mosquito was not simply the 1935 proposal revisited but was a much bigger and more powerful aircraft powered by two Rolls-Royce Merlin engines delivering over twice the power of the Gipsy Sixes.
Grosvenor House:-
The scarlet G-ACSS was the property of Mr A.O.Edwards and was named Grosvenor House after the hotel which he managed. The crew were C. W. A. Scott and Tom Campbell Black. When the Mollisons ran into problems at Karachi, Scott and Campbell Black took over the lead and were first into Allahabad. Despite a severe storm over the Bay of Bengal they reached Singapore safely, eight hours ahead of the DC-2.
They took off for Darwin, but over the Timor Sea lost power in the port engine when the oil pressure dropped to zero. Repairs at Darwin got them going again, although continuing oil warnings caused them to fly the last two legs with one engine throttled back. Their lead was unassailable despite this, and after the final mandatory stop and more engine work at Charleville they flew on to cross the finish line at Flemington Racecourse (in Melbourne) at 3.33 p.m. (local time) on 23 October. Their official time was 71 hours 18 seconds.
Also named 'Comet' was the Ford Motor Company's 'Intermediate' model under the Mercury marque. Though considered an intermediate, the Comet was in many ways, just a long wheelbase compact, based on the Falcon. The 1964 model update was enlarged from the first generation 1960-63 model, and replaced the unsuccessful Mercury Meteor (based on the Ford Fairlane) in the intermediate segment.
The performance model sub-series was known as 'Cylone', and was equipped with the V8 engine. A small number of 50 light-weight Cyclones fitted with the 427 race motor were built, and fielded in the A/FX category in Stock Car Racing.
The Comet model would remain on as Mercury's intermediate until the end of 1969. The name was reused for the Mercury twin of the compact Ford Maverick in 1971 through to 1977.
The de Havilland DH88 Comet (1934) and Mercury Comet Cyclone Hardtop Coupe (1964) featured here are modelled in Lego miniland-scale for Flickr LUGNuts 79th Build Challenge, - "LUGNuts goes Wingnuts", - featuring automotive vehicles named after, inspired by, or related to aircraft.
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.
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
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NEW YORK, NEW YORK - OCTOBER 05: (L-R) Seo "deokdam" Dae-gil, Heo “ShowMaker” Su and Kim "Canyon" Geon-bu of DAMWON KIA pose at the League of Legends World Championship Groups Features Day on October 5, 2022 in New York City. (Photo by Colin Young-Wolff/Riot Games)
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.
NEW YORK, NEW YORK - OCTOBER 05: Son "Lehends" Si-woo (L) and Jeong "Chovy" Ji-hoon of Gen.G pose at the League of Legends World Championship Groups Features Day on October 5, 2022 in New York City. (Photo by Colin Young-Wolff/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.
Hạ Long Bay (Vietnamese: Vịnh Hạ Long, About this sound listen, literally: "descending dragon bay") is a UNESCO World Heritage Site, and a popular travel destination, in Quảng Ninh Province, Vietnam. Administratively, the bay belongs to Hạ Long City, Cẩm Phả town, and the part of Vân Đồn District. The bay features thousands of limestone karsts and isles in various sizes and shapes. Hạ Long Bay is a center of a larger zone which includes Bái Tử Long bay to the northeast, and Cát Bà islands to the southwest. These larger zones share similar geological, geographical, geomorphological, climate, and cultural characters.
Hạ Long Bay has an area of around 1,553 km2, including 1,960–2,000 islets, most of which are limestone. The core of the bay has an area of 334 km2 with a high density of 775 islets. The limestone in this bay has gone through 500 million years of formation in different conditions and environments. The evolution of the karst in this bay has taken 20 million years under the impact of the tropical wet climate. The geo-diversity of the environment in the area has created biodiversity, including a tropical evergreen biosystem, oceanic and sea shore biosystem. Hạ Long Bay is home to 14 endemic floral species and 60 endemic faunal species.
Historical research surveys have shown the presence of prehistorical human beings in this area tens of thousands years ago. The successive ancient cultures are the Soi Nhụ culture around 18,000–7000 BC, the Cái Bèo culture 7000–5000 BC and the Hạ Long culture 5,000–3,500 years ago. Hạ Long Bay also marked important events in the history of Vietnam with many artifacts found in Bài Thơ Mount, Đầu Gỗ Cave, Bãi Cháy.
500 years ago, Nguyễn Trãi praised the beauty of Hạ Long Bay in his verse Lộ nhập Vân Đồn, in which he called it "rock wonder in the sky".[8] In 1962, the Ministry of Culture, Sports and Tourism of North Vietnam listed Hạ Long Bay in the National Relics and Landscapes publication. In 1994, the core zone of Hạ Long Bay was listed by UNESCO as a World Heritage Site according to criterion vii, and listed for a second time according to criterion viii.
ETYMOLOGY
The name Hạ Long is derived from the Sino-Vietnamese 下龍, meaning "descending dragon".
Before 19th century, the name Halong Bay had not been recorded in the old books of our country. It has been called An Bang, Luc Thuy, Van Don... Late 19th century, the name Halong Bay has appeared on the Maritime map of France. "Haiphong News" published in French, has reported: " Dragon appears on Halong Bay". The story can be summarized as follows: In 1898, lieutenant Lagoredin captain of Avalangso met a couple of giant sea snake on Halong Bay three times. Not only the lieutenant but also many other sailors saw those species. The European thought that those animals looked like Asian dragon. Maybe the appearance of strange animals led to the name of Quang Ninh sea area today: Halong Bay
According to local legend, when Vietnam had just started to develop into a country, they had to fight against invaders. To assist the Vietnamese in defending their country, the gods sent a family of dragons as protectors. This family of dragons began spitting out jewels and jade. These jewels turned into the islands and islets dotting the bay, linking together to form a great wall against the invaders. Under magics, numerous rock mountains abruptly appeared on the sea, ahead of invaders' ships; the forward ships struck the rocks and each other. After winning the battle, the dragons were interested in peaceful sightseeing of the Earth, and then decided to live in this bay. The place where the mother dragon descended was named Hạ Long, the place where the dragon's children attended upon their mother was called Bái Tử Long island (Bái: attend upon, Tử: children, Long: dragon), and the place where the dragon's children wriggled their tails violently was called Bạch Long Vỹ island (Bạch: white-color of the foam made when Dragon's children wriggled, Long: dragon, Vỹ: tail), present day Trà Cổ peninsula, Móng Cái.
OVERVIEW
The bay consists of a dense cluster of some 1,600 limestone monolithic islands each topped with thick jungle vegetation, rising spectacularly from the ocean. Several of the islands are hollow, with enormous caves. Hang Đầu Gỗ (Wooden stakes cave) is the largest grotto in the Hạ Long area. French tourists visited in the late 19th century, and named the cave Grotte des Merveilles. Its three large chambers contain large numerous stalactites and stalagmites (as well as 19th century French graffiti). There are two bigger islands, Tuần Châu and Cát Bà, that have permanent inhabitants, as well as tourist facilities including hotels and beaches. There are a number of beautiful beaches on the smaller islands.
A community of around 1,600 people live on Hạ Long Bay in four fishing villages: Cửa Vạn, Ba Hang, Cống Tàu and Vông Viêng in Hùng Thắng commune, Hạ Long city. They live on floating houses and are sustained through fishing and marine aquaculture (cultivating marine biota), plying the shallow waters for 200 species of fish and 450 different kinds of mollusks. Many of the islands have acquired their names as a result of interpretation of their unusual shapes. Such names include Voi Islet (elephant), Ga Choi Islet (fighting cock), Khi Islet (monkey), and Mai Nha Islet (roof). 989 of the islands have been given names. Birds and animals including bantams, antelopes, monkeys, and lizard also live on some of the islands.
Almost all these islands are as individual towers in a classic fenglin landscape with heights from 50m to 100m, and height/width ratios of up to about six.
Another specific feature of Halong Bay is the abundance of lakes inside the limestone islands. For example, Dau Be island has six enclosed lakes. All these island lakes occupy drowned dolines within fengcong karst.
LOCATION
Hạ Long Bay is located in northeastern Vietnam, from E106°56' to E107°37' and from N20°43' to N21°09'. The bay stretches from Yên Hưng district, past Hạ Long city, Cẩm Phả town to Vân Đồn District, bordered on the south and southeast by the Gulf of Tonkin, on the north by China, and on the west and southwest by Cát Bà Island. The bay has a 120 km long coastline and is approximately 1,553 km² in size with about 2,000 islets. The area designated by UNESCO as the World Natural Heritage Site incorporates 434 km² with 775 islets, of which the core zone is delimited by 69 points: Đầu Gỗ island on the west, Ba Hầm lake on the south and Cống Tây island on the east. The protected area is from the Cái Dăm petrol store to Quang Hanh commune, Cẩm Phả town and the surrounding zone.
CLIMATE
The climate of the bay is tropical, wet, sea islands, with two seasons: hot and moist summer, and dry and cold winter. The average temperature is from 15 °C- 25 °C, and annual rainfall is between 2 meters and 2.2 meters. Hạ Long Bay has the typical diurnal tide system (tide amplitude ranges from 3.5-4m). The salinity is from 31 to 34.5MT in the dry season and lower in the rainy season.
HISTORY
SOI NHU CULTURE (16,000–5000 BC)
Located in Hạ Long and Bái Tử Long are archaeological sites such as Mê Cung and Thiên Long. There are remains from mounds of mountain shellfish (Cyclophorus), spring shellfish (Melania), some fresh water mollusc and some rudimentary labour tools. The main way of life of Soi Nhụ's inhabitants included catching fish and shellfish, collecting fruits and digging for bulbs and roots. Their living environment was a coastal area unlike other Vietnamese cultures, for example, like those found in Hòa Bình and Bắc Sơn.
CAI BEO CULTURE (5000–3000 BC)
Located in Hạ Long and Cát Bà island, its inhabitants developed to the level of sea exploitation. Cái Bèo culture is a link between Soi Nhụ culture and Hạ Long culture.
FEUDAL PERIOD
History shows that Hạ Long Bay was the setting for local naval battles against Vietnam's coastal neighbors. On three occasions, in the labyrinth of channels in Bạch Đằng River near the islands, the Vietnamese army stopped the Chinese from landing. In 1288, General Trần Hưng Đạo stopped Mongol ships from sailing up the nearby Bạch Đằng River by placing steel-tipped wooden stakes at high tide, sinking the Mongol Kublai Khan's fleet.
During the Vietnam War, many of the channels between the islands were heavily mined by the United States navy, some of which pose a threat to shipping to this day.
GEOLOGY AND GEOMORPHOLOGY
In 2000, the UNESCO’s World Heritage Committee has inscribed the Hạ Long Bay in the World Heritage List according to its outstanding examples representing major stages of the Earth’s history and its original limestone karstic geomorphologic features. The Hạ Long Bay and its adjacent areas consist of a part of the Sino-Vietnamese composite terrane having its development history from pre-Cambrian up to present day. During Phanerozoic, terrigenous, volcanogenic and cherty-carbonate sediments containing in abundance graptolites, brachiopods, fishes, corals, foraminiferas, radiolarias, bivalves and flora, separated one from another by 10 stratigraphic gaps, but the boundary between Devonian and Carboniferous has been considered as continuous. The limestone karstic geomorphology of the bay was developed since Miocene, especially the cone-shaped hills (fengcong), or isolated high limestone karst towers (fenglin) with many remnants of old phreatic caves, old karstic foot caves, marine notch caves form magnificent limestone karst landforms as unique on the world. The Quaternary geology was developed through 5 cycles with the intercalation of marine and continental environments. The present Hạ Long Bay, in fact, appeared after the Middle Holocene maximum transgression, leaving ultimate zone of lateral undercutting in the limestone cliffs bearing many shells of oysters, having the 14C age as 2280 to >40,000 y. BP. Geological resources are abundant: anthracite, lignite, oil shale, petroleum, phosphate, limestone and cement additives, kaolin, silica sand, dolomite, quartzite of exogenous origin, and antimony, mercury of hydrothermal origin. Besides, there still are surface water, groundwater and thermal mineral water on the shore of the Hạ Long - Bái Tử Long Bays and other environmental resources.
In terms of marine geology, this area is recorded as an especially coastal sedimentary environment. In the alkaline seawater environment, the chemical denudation process of calcium carbonate proceeds rapidly, creating wide, strangely shaped marine notches.
The bottom surface sediments are various from clay mud to sand, however, silty mud and clay mud are dominated in distribution. Especially, the carbonate materials originated from organisms make up from 60-65% sedimentary content. The surface sediments of coral reefs are mainly sand and pebbles of which the carbonate materials occupy for more than 90%. The intertidal zone sediments are various from clay mud to sand and gravel depending to distinguished sedimentary environments such as mangrove marshes, tidal flats, beaches etc. At the small, but wonderfully beautiful beaches, the sand sediments may be dominated quartz or carbonate materials.
The sediment layers of intertidal zone, the upper sea bed with a plain surface conserving ancient rivers, systems of caves and it's sediments, traces of ancient marine action forming distinctive notches, beaches and marine terraces, mangrove swamps are important evidence of geological events and processes taking place during Quaternary.
HISTORY OF TECTONICS
Hạ Long Bay has experienced at least 500 million years in various geological states of orogeny, marine transgression and marine regression. During the Ordovician and Silurian periods (500-410 million years ago), Hạ Long Bay was deep sea. During the Carboniferous and Permian periods (340-250 million years ago), Hạ Long Bay was at shallow sea level.
The dominated uplift movement of neotectonic and recent tectonic influenced deeply on topography of this area, and the present landscape of sea-islands was formed around 7 or 8 thousand years ago by the sea invasion during Holocene transgression begun at about 17-18 thousand years ago. Particularly from the Holocene time, from about 11,000 years ago Cat Ba - Hạ Long area has much archaeological evidence connecting variations in sea levels with the development of ancient cultures such as the Soi Nhu and Ha Long cultures.
KARST GEOMORPHOLOGY VALUE
Due to a simultaneous combination of ideal factors such as thick, pale, grey, and strong limestone layers, which are formed by fine-grained materials; hot and moist climate and slow tectonic process as a whole; Hạ Long Bay has had a complete karst evolution for 20 million years. There are many types of karst topography in the bay, such as karst field.
Hạ Long Bay is a mature karst landscape developed during a warm, wet, tropical climate. The sequence of stages in the evolution of a karst landscape over a period of 20 million years requires a combination of several distinct elements including a massive thickness of limestone, a hot wet climate and slow overall tectonic up lift. The process of karst formation is divided into five stage is the formation of the distinctive do line karst. This is followed by the development of fengcong karst can be seen in the groups of hills on Bo Hon and Dau Be Inland. These cones with sloping side average 100m in height with the tallest exceeding 200m. Fenglin karst is characterised by steep separate towers. The hundreds of rocky islands with form the beautiful and famous landscape of the Bay are the individual towers of a classic Fenglin landscape where the intervening plains have been submerged by the sea. Most towers reach a height of between 50 and 100m with a height to width ratio of about 6. The karst dolines were flooded by the sea becoming the abundance of lakes that lie within the limestone islands. For example, Dau Be island at the mouth of the Bay has six enclosed lakes including those of the Ba Ham lakes lying within its fencong karst. The Bay contains examples of the landscape elements of fengcong, fenglin and karst plain. These are not separate evolutionary stages but the result of natural non – uniform processes in the denudation of a large mass of limestone. Marine erosion created the notches which in some places have been enlarged into caves. The marine notch is a feature of limestone coastline but, in Ha Long Bay, it has created the mature landscape.
Within Ha Long Bay, the main accessible caves are the older passages that survive from the time when the karst was evolving though its various stages of fengcong and fenglin. Three main types of caves can be recognized in the limestone islands (Waltham, T. 1998):
Remnants of old phreatic caves
Old karstic foot caves
Marine notch caves
The first group of caves is old phreatic caves which include Sung Sot, Tam Cung, Lau Dai, Thien Cung, Dau Go, Hoang Long, Thien Long. Nowadays, these caves lie at various high levels. Sung Sot cave is on Bo Hon island. From its truncated entrance chambers on allege high on the cliff, a passage of more that 10m high and wide descends to the south. Tam Cung is a large phreatic fissure cave that developed in the bedding planes of the limestone dividing the fissure cave into three chambers. Lau Dai is a cave with a complex of passages extending over 300m opening on the south side of Con Ngua island. Thien Cung and Dau Go are remnants of the same old cave system. They both survive in the northern part of Dau Go island at between 20 and 50m above sea level. Thien Cung has one large chamber more that 100m long, blocked at its ends and almost subdivided into smaller chambers by massive wall of stalactites and stalagmites. Dau Go is a single large tunnel descending along a major set of fractures to a massive choke.
The second group of caves is the old karstic foot caves which include Trinh Lu, Bo Nau, Tien Ong and Trong caves. Foot caves are a ubiquitous feature of karst landscapes which have reached a stage of widespread lateral undercutting at base level. They may extend back into maze caves of stream caves draining from larger cave systems within the limestone. They are distinguished by the main elements of their passages being close to the horizontal and are commonly related to denuded or accumulated terraces at the old base levels. Trinh Nu, which is one of the larger foot caves in Ha Long Bay with its ceiling at about 12m above sea level and about 80m in length, was developed in multiple stages. Bo Nau, a horizontal cave containing old stalactite deposits, cuts across the 25o dip of the bedding plane.
The third group is the marine notch caves that are a special feature of the karst of Ha Long Bay. The dissolution process of sea water acting on the limestone and erosion by wave action crates notches at the base of the cliffs. In advantageous conditions, dissolution of the limestone allows the cliff notches to be steadily deepened and extended into caves. Many of these at sea level extend right though the limestone hills into drowned dolines which are now tidal lakes.
A distinguishing feature of marine notch caves is an absolutely smooth and horizontal ceiling cut through the limestone. Some marine notch caves had been not formed at present sea level, but old sea levels related to sea level changes in Holocene transgression, event to Pleistocene sea levels. Some of them passed preserved the development of old karstic foot cave in mainland environment or preserved the remnants of older phreatic caves. One of the most unusual features of Ha Long Bay is the Bo Ham lake group of hidden lakes and their connecting tunnel – notch caves in Dau Be island. From the island’s perimeter cliff a cave, 10m wide at water level and curving so that it is almost completely dark, extends about 150m to Lake 1. Luon cave is on Bo Hon island and extends 50m though to an enclosed tidal lake. It has a massive stalactite hanging 2m down and truncated at the modern tidal level. It has passed though many stages in its formation.
The karst landscape of Ha Long Bay is of international significance and of fundamental importance to the science of geomorphology. The fenglin tower karst, which is the type present in much of Ha Long Bay, is the most extreme form of limestone landscape development. If these karst landscapes are broadly compared in terms of their height, steepness and number of their limestone towers, Ha Long Bay is probably second in the entire world only to Yangshou, in China. However, Ha Long Bay ha also been invaded by the sea so that the geomorphology of its limestone is lands are, at least in part, the consequence of marine erosion. The marine invasion distinguishes Ha Long Bay and makes it unique in the world. There are other areas of submerged karst towers which were invaded by the sea, but none is as extensive as Ha Long Bay.
TIMELINE OF GEOLOGIC EVOLUTION
Some of the most remarkable geological events in Hạ Long Bay's history have occurred in the last 1,000 years, include the advance of the sea, the raising of the bay area, strong erosion that has formed coral, and, pure blue and heavily salted water. This process of erosion by seawater has deeply engraved the stone, contributing to its fantastic beauty. Present-day Hạ Long Bay is the result of this long process of geological evolution that has been influenced by so many factors.
Due to all these factors, tourists visiting Hạ Long Bay are not only treated to one of the natural wonders of the world, but also to a precious geological museum that has been naturally preserved in the open air for the last 300 million years.
ECOLOGY
Halong Bay is host to two ecosystems: a tropical, moist, evergreen rainforest ecosystem; and a marine and coastal ecosystem. The bay is home to seven endemic species: Livistona halongensis, Impatiens halongensis, Chirita halongensis, Chirita hiepii, Chirita modesta, Paraboea halongensis and Alpinia calcicola.
The many islands that dot the bay are home to a great many other species, including (but likely not limited to): 477 magnoliales, 12 pteris, 20 salt marsh flora; and 4 amphibia, 10 reptilia, 40 aves, and 4 mammalia.
Common aquatic species found in the bay include: cuttlefish (mực); oyster (hào); cyclinae (ngán); prawns (penaeidea (tôm he), panulirus (tôm hùm), parapenaeopsis (tôm sắt), etc.); sipunculoideas (sá sùng); nerita (ốc đĩa); charonia tritonis (ốc tù và); and cà sáy.
ENVIRONMENTAL DAAGE
With an increasing tourist trade, mangroves and seagrass beds have been cleared and jetties and wharves have been built for tourist boats.
Game fishing, often near coral reefs, is threatening many endangered species of fish.
Local government and businesses are aware of problems and many measures have been taken to minimize tourism affect to the bay environment for sustainable economic growth like introducing eco friendly tours and introducing tight waste control on resorts.
AWARDS AND DESIGNATIONS
In 1962, the Vietnam Ministry of Culture, Sport and Tourism designated Hạ Long Bay a 'Renowned National Landscape Monument'.
Hạ Long Bay was first listed as a UNESCO World Heritage Site in 1994, in recognition of its outstanding, universal aesthetic value. In 2000 the World Heritage Committee additionally recognised Hạ Long Bay for its outstanding geological and geomorphological value, and its World Heritage Listing was updated.
In October 2011, World Monuments Fund included the bay on the 2012 World Monuments Watch, citing tourism pressures and associated development as threats to the site that must be addressed. The goal of Watch-listing is to promote strategies of responsible heritage-driven development for a sustainable future.
In 2012, New 7 Wonders Foundation officially named Halong Bay as one of New Seven Natural Wonders of the world.
Hạ Long Bay is also a member of the Club of the Most Beautiful Bays of the World.
IN LITERATURE
In writings about Hạ Long Bay, the following Vietnamese writers said:
Nguyễn Trãi: "This wonder is ground raising up into the middle of the high sky".
Xuân Diệu: "Here is the unfinished works of the Beings...Here is the stones which the Giant played and threw away".
Nguyên Ngọc: "...to form this first- rate wonder, nature only uses: Stone and Water...There are just only two materials themselves chosen from as much as materials, in order to write, to draw, to sculpture, to create everything...It is quite possible that here is the image of the future world".
Ho Chi Minh: "It is the wonder that one cannot impart to others".
Phạm Văn Đồng: "Is it one scenery or many sceneries? Is it the scenery in the world or somewhere?".
Nguyễn Tuân: "Only mountains accept to be old, but Hạ Long sea and wave are young for ever".
Huy Cận: "Night breathes, stars wave Hạ Long's water".
Chế Lan Viên:
"Hạ Long, Bái Tử Long- Dragons were hidden, only stones still remain
On the moonlight nights, stones meditate as men do..."
Lord Trịnh Cương overflowed with emotion: "Mountains are glistened by water shadow, water spills all over the sky".
ANCIENT TALES
Hạ Long bay's inhabitants have developed numerous tales explaining names given to various isles and caves in the bay.
Đầu Gỗ cave (literally: "the end of wooden bars" cave): these wooden bars in this cave are the remnants of sharped wooden columns built under the water level by the order of Trần Hưng Đạo commander in order to sink Mongolian invaders' ships in the 13th century.
Kim Quy cave (literally: "Golden Turtle" cave): it is told that the Golden Turtle swam toward the Eastern Sea (international name: South China Sea) after returning the holy sword which had assisted King Lê Thái Tổ in the combat against Ming invaders from China. Next, with the approval of the Sea King, Golden Turtle continued to fight against monsters in this marine area. The turtle became exhausted and died in a cave. Consequently, the cave was named after the Golden Turtle.
Con Cóc isle (literally: Frog isle): is a frog- like isle. According to ancient tales, in a year of severe drought, a frog directed all animals to the Heaven and protested against the God. They demonstrated in favour of making rain. As a result, the God must accept the frog as his uncle. Since then, whenever frogs grind their teeth, the God has to pour water down the ground.
WIKIPEDIA
Canisbay Parish Church is a Church of Scotland church in Canisbay, Scotland, that dates back to the early 1600s and is the most northernly church on mainland Britain. It is a Category A listed building. It is surrounded by a large cemetery, which is split into two sections, the new and old. It features a square bell tower, nave and a porch. The porch was added in 1891, when the other extensions and work was completed to the church building.
The church was rebuilt in the 17th century, and ancient remains were discovered after a wall collapsed in the cemetery. Jan De Groot, the man who founded John o' Groats, is buried in Canisbay cemetery; his tombstone sits in the church building and is a popular tourist attraction when the building is open for visitors every summer. The book Lest We Forget: The Parish of Canisbay (1996) is a "miscellany of memories written by parishioners and friends so that future generations can know what made Canisbay a very special place".
Between 1959 and 2001 Queen Elizabeth the Queen Mother was a regular worshipper at the church during her periods of residence, usually in late summer each year, at the nearby Castle of Mey, which she owned.
Canisbay is a rural hamlet located about one mile (1.5 kilometres) southwest of Huna and two and a half miles (four kilometres) southwest of John o' Groats in Caithness, Scottish Highlands, and is in the Scottish council area of Highland. It lies on the A836 coast road, which bypasses the hamlet to the north.
It is home to Canisbay Primary School, a Village Hall, Medical Practice, and two Churches, one of which was the church used by Charles III. The Church is also the burial place of Jean De Groot, the ferryman after which John o' Groats is named.
The Parish of Canisbay includes John o' Groats, Upper and Lower Gills, Huna and Freswick.
Canisbay Juniors are the "feeder" team to John o' Groats FC with many of the key first team players having played for the side at one time. They play in the youth development leagues in Caithness where they enter teams at all age groups. It is also home to Canisbay Rifle club, who regularly compete in the Caithness Rifle Leagues.
The Canisbay Show is the local agricultural and crafts show held mid-June each year in the park behind the village hall, with the JCB competition, the karate display and mainly the Beer Tent being the big attractions.
The Highlands is a historical region of Scotland. Culturally, the Highlands and the Lowlands diverged from the Late Middle Ages into the modern period, when Lowland Scots language replaced Scottish Gaelic throughout most of the Lowlands. The term is also used for the area north and west of the Highland Boundary Fault, although the exact boundaries are not clearly defined, particularly to the east. The Great Glen divides the Grampian Mountains to the southeast from the Northwest Highlands. The Scottish Gaelic name of A' Ghàidhealtachd literally means "the place of the Gaels" and traditionally, from a Gaelic-speaking point of view, includes both the Western Isles and the Highlands.
The area is very sparsely populated, with many mountain ranges dominating the region, and includes the highest mountain in the British Isles, Ben Nevis. During the 18th and early 19th centuries the population of the Highlands rose to around 300,000, but from c. 1841 and for the next 160 years, the natural increase in population was exceeded by emigration (mostly to Canada, the United States, Australia and New Zealand, and migration to the industrial cities of Scotland and England.) and passim The area is now one of the most sparsely populated in Europe. At 9.1/km2 (24/sq mi) in 2012, the population density in the Highlands and Islands is less than one seventh of Scotland's as a whole.
The Highland Council is the administrative body for much of the Highlands, with its administrative centre at Inverness. However, the Highlands also includes parts of the council areas of Aberdeenshire, Angus, Argyll and Bute, Moray, North Ayrshire, Perth and Kinross, Stirling and West Dunbartonshire.
The Scottish Highlands is the only area in the British Isles to have the taiga biome as it features concentrated populations of Scots pine forest: see Caledonian Forest. It is the most mountainous part of the United Kingdom.
Between the 15th century and the mid-20th century, the area differed from most of the Lowlands in terms of language. In Scottish Gaelic, the region is known as the Gàidhealtachd, because it was traditionally the Gaelic-speaking part of Scotland, although the language is now largely confined to The Hebrides. The terms are sometimes used interchangeably but have different meanings in their respective languages. Scottish English (in its Highland form) is the predominant language of the area today, though Highland English has been influenced by Gaelic speech to a significant extent. Historically, the "Highland line" distinguished the two Scottish cultures. While the Highland line broadly followed the geography of the Grampians in the south, it continued in the north, cutting off the north-eastern areas, that is Eastern Caithness, Orkney and Shetland, from the more Gaelic Highlands and Hebrides.
Historically, the major social unit of the Highlands was the clan. Scottish kings, particularly James VI, saw clans as a challenge to their authority; the Highlands was seen by many as a lawless region. The Scots of the Lowlands viewed the Highlanders as backward and more "Irish". The Highlands were seen as the overspill of Gaelic Ireland. They made this distinction by separating Germanic "Scots" English and the Gaelic by renaming it "Erse" a play on Eire. Following the Union of the Crowns, James VI had the military strength to back up any attempts to impose some control. The result was, in 1609, the Statutes of Iona which started the process of integrating clan leaders into Scottish society. The gradual changes continued into the 19th century, as clan chiefs thought of themselves less as patriarchal leaders of their people and more as commercial landlords. The first effect on the clansmen who were their tenants was the change to rents being payable in money rather than in kind. Later, rents were increased as Highland landowners sought to increase their income. This was followed, mostly in the period 1760–1850, by agricultural improvement that often (particularly in the Western Highlands) involved clearance of the population to make way for large scale sheep farms. Displaced tenants were set up in crofting communities in the process. The crofts were intended not to provide all the needs of their occupiers; they were expected to work in other industries such as kelping and fishing. Crofters came to rely substantially on seasonal migrant work, particularly in the Lowlands. This gave impetus to the learning of English, which was seen by many rural Gaelic speakers to be the essential "language of work".
Older historiography attributes the collapse of the clan system to the aftermath of the Jacobite risings. This is now thought less influential by historians. Following the Jacobite rising of 1745 the British government enacted a series of laws to try to suppress the clan system, including bans on the bearing of arms and the wearing of tartan, and limitations on the activities of the Scottish Episcopal Church. Most of this legislation was repealed by the end of the 18th century as the Jacobite threat subsided. There was soon a rehabilitation of Highland culture. Tartan was adopted for Highland regiments in the British Army, which poor Highlanders joined in large numbers in the era of the Revolutionary and Napoleonic Wars (1790–1815). Tartan had largely been abandoned by the ordinary people of the region, but in the 1820s, tartan and the kilt were adopted by members of the social elite, not just in Scotland, but across Europe. The international craze for tartan, and for idealising a romanticised Highlands, was set off by the Ossian cycle, and further popularised by the works of Walter Scott. His "staging" of the visit of King George IV to Scotland in 1822 and the king's wearing of tartan resulted in a massive upsurge in demand for kilts and tartans that could not be met by the Scottish woollen industry. Individual clan tartans were largely designated in this period and they became a major symbol of Scottish identity. This "Highlandism", by which all of Scotland was identified with the culture of the Highlands, was cemented by Queen Victoria's interest in the country, her adoption of Balmoral as a major royal retreat, and her interest in "tartenry".
Recurrent famine affected the Highlands for much of its history, with significant instances as late as 1817 in the Eastern Highlands and the early 1850s in the West. Over the 18th century, the region had developed a trade of black cattle into Lowland markets, and this was balanced by imports of meal into the area. There was a critical reliance on this trade to provide sufficient food, and it is seen as an essential prerequisite for the population growth that started in the 18th century. Most of the Highlands, particularly in the North and West was short of the arable land that was essential for the mixed, run rig based, communal farming that existed before agricultural improvement was introduced into the region.[a] Between the 1760s and the 1830s there was a substantial trade in unlicensed whisky that had been distilled in the Highlands. Lowland distillers (who were not able to avoid the heavy taxation of this product) complained that Highland whisky made up more than half the market. The development of the cattle trade is taken as evidence that the pre-improvement Highlands was not an immutable system, but did exploit the economic opportunities that came its way. The illicit whisky trade demonstrates the entrepreneurial ability of the peasant classes.
Agricultural improvement reached the Highlands mostly over the period 1760 to 1850. Agricultural advisors, factors, land surveyors and others educated in the thinking of Adam Smith were keen to put into practice the new ideas taught in Scottish universities. Highland landowners, many of whom were burdened with chronic debts, were generally receptive to the advice they offered and keen to increase the income from their land. In the East and South the resulting change was similar to that in the Lowlands, with the creation of larger farms with single tenants, enclosure of the old run rig fields, introduction of new crops (such as turnips), land drainage and, as a consequence of all this, eviction, as part of the Highland clearances, of many tenants and cottars. Some of those cleared found employment on the new, larger farms, others moved to the accessible towns of the Lowlands.
In the West and North, evicted tenants were usually given tenancies in newly created crofting communities, while their former holdings were converted into large sheep farms. Sheep farmers could pay substantially higher rents than the run rig farmers and were much less prone to falling into arrears. Each croft was limited in size so that the tenants would have to find work elsewhere. The major alternatives were fishing and the kelp industry. Landlords took control of the kelp shores, deducting the wages earned by their tenants from the rent due and retaining the large profits that could be earned at the high prices paid for the processed product during the Napoleonic wars.
When the Napoleonic wars finished in 1815, the Highland industries were affected by the return to a peacetime economy. The price of black cattle fell, nearly halving between 1810 and the 1830s. Kelp prices had peaked in 1810, but reduced from £9 a ton in 1823 to £3 13s 4d a ton in 1828. Wool prices were also badly affected. This worsened the financial problems of debt-encumbered landlords. Then, in 1846, potato blight arrived in the Highlands, wiping out the essential subsistence crop for the overcrowded crofting communities. As the famine struck, the government made clear to landlords that it was their responsibility to provide famine relief for their tenants. The result of the economic downturn had been that a large proportion of Highland estates were sold in the first half of the 19th century. T M Devine points out that in the region most affected by the potato famine, by 1846, 70 per cent of the landowners were new purchasers who had not owned Highland property before 1800. More landlords were obliged to sell due to the cost of famine relief. Those who were protected from the worst of the crisis were those with extensive rental income from sheep farms. Government loans were made available for drainage works, road building and other improvements and many crofters became temporary migrants – taking work in the Lowlands. When the potato famine ceased in 1856, this established a pattern of more extensive working away from the Highlands.
The unequal concentration of land ownership remained an emotional and controversial subject, of enormous importance to the Highland economy, and eventually became a cornerstone of liberal radicalism. The poor crofters were politically powerless, and many of them turned to religion. They embraced the popularly oriented, fervently evangelical Presbyterian revival after 1800. Most joined the breakaway "Free Church" after 1843. This evangelical movement was led by lay preachers who themselves came from the lower strata, and whose preaching was implicitly critical of the established order. The religious change energised the crofters and separated them from the landlords; it helped prepare them for their successful and violent challenge to the landlords in the 1880s through the Highland Land League. Violence erupted, starting on the Isle of Skye, when Highland landlords cleared their lands for sheep and deer parks. It was quietened when the government stepped in, passing the Crofters' Holdings (Scotland) Act, 1886 to reduce rents, guarantee fixity of tenure, and break up large estates to provide crofts for the homeless. This contrasted with the Irish Land War underway at the same time, where the Irish were intensely politicised through roots in Irish nationalism, while political dimensions were limited. In 1885 three Independent Crofter candidates were elected to Parliament, which listened to their pleas. The results included explicit security for the Scottish smallholders in the "crofting counties"; the legal right to bequeath tenancies to descendants; and the creation of a Crofting Commission. The Crofters as a political movement faded away by 1892, and the Liberal Party gained their votes.
Today, the Highlands are the largest of Scotland's whisky producing regions; the relevant area runs from Orkney to the Isle of Arran in the south and includes the northern isles and much of Inner and Outer Hebrides, Argyll, Stirlingshire, Arran, as well as sections of Perthshire and Aberdeenshire. (Other sources treat The Islands, except Islay, as a separate whisky producing region.) This massive area has over 30 distilleries, or 47 when the Islands sub-region is included in the count. According to one source, the top five are The Macallan, Glenfiddich, Aberlour, Glenfarclas and Balvenie. While Speyside is geographically within the Highlands, that region is specified as distinct in terms of whisky productions. Speyside single malt whiskies are produced by about 50 distilleries.
According to Visit Scotland, Highlands whisky is "fruity, sweet, spicy, malty". Another review states that Northern Highlands single malt is "sweet and full-bodied", the Eastern Highlands and Southern Highlands whiskies tend to be "lighter in texture" while the distilleries in the Western Highlands produce single malts with a "much peatier influence".
The Scottish Reformation achieved partial success in the Highlands. Roman Catholicism remained strong in some areas, owing to remote locations and the efforts of Franciscan missionaries from Ireland, who regularly came to celebrate Mass. There remain significant Catholic strongholds within the Highlands and Islands such as Moidart and Morar on the mainland and South Uist and Barra in the southern Outer Hebrides. The remoteness of the region and the lack of a Gaelic-speaking clergy undermined the missionary efforts of the established church. The later 18th century saw somewhat greater success, owing to the efforts of the SSPCK missionaries and to the disruption of traditional society after the Battle of Culloden in 1746. In the 19th century, the evangelical Free Churches, which were more accepting of Gaelic language and culture, grew rapidly, appealing much more strongly than did the established church.
For the most part, however, the Highlands are considered predominantly Protestant, belonging to the Church of Scotland. In contrast to the Catholic southern islands, the northern Outer Hebrides islands (Lewis, Harris and North Uist) have an exceptionally high proportion of their population belonging to the Protestant Free Church of Scotland or the Free Presbyterian Church of Scotland. The Outer Hebrides have been described as the last bastion of Calvinism in Britain and the Sabbath remains widely observed. Inverness and the surrounding area has a majority Protestant population, with most locals belonging to either The Kirk or the Free Church of Scotland. The church maintains a noticeable presence within the area, with church attendance notably higher than in other parts of Scotland. Religion continues to play an important role in Highland culture, with Sabbath observance still widely practised, particularly in the Hebrides.
In traditional Scottish geography, the Highlands refers to that part of Scotland north-west of the Highland Boundary Fault, which crosses mainland Scotland in a near-straight line from Helensburgh to Stonehaven. However the flat coastal lands that occupy parts of the counties of Nairnshire, Morayshire, Banffshire and Aberdeenshire are often excluded as they do not share the distinctive geographical and cultural features of the rest of the Highlands. The north-east of Caithness, as well as Orkney and Shetland, are also often excluded from the Highlands, although the Hebrides are usually included. The Highland area, as so defined, differed from the Lowlands in language and tradition, having preserved Gaelic speech and customs centuries after the anglicisation of the latter; this led to a growing perception of a divide, with the cultural distinction between Highlander and Lowlander first noted towards the end of the 14th century. In Aberdeenshire, the boundary between the Highlands and the Lowlands is not well defined. There is a stone beside the A93 road near the village of Dinnet on Royal Deeside which states 'You are now in the Highlands', although there are areas of Highland character to the east of this point.
A much wider definition of the Highlands is that used by the Scotch whisky industry. Highland single malts are produced at distilleries north of an imaginary line between Dundee and Greenock, thus including all of Aberdeenshire and Angus.
Inverness is regarded as the Capital of the Highlands, although less so in the Highland parts of Aberdeenshire, Angus, Perthshire and Stirlingshire which look more to Aberdeen, Dundee, Perth, and Stirling as their commercial centres.
The Highland Council area, created as one of the local government regions of Scotland, has been a unitary council area since 1996. The council area excludes a large area of the southern and eastern Highlands, and the Western Isles, but includes Caithness. Highlands is sometimes used, however, as a name for the council area, as in the former Highlands and Islands Fire and Rescue Service. Northern is also used to refer to the area, as in the former Northern Constabulary. These former bodies both covered the Highland council area and the island council areas of Orkney, Shetland and the Western Isles.
Much of the Highlands area overlaps the Highlands and Islands area. An electoral region called Highlands and Islands is used in elections to the Scottish Parliament: this area includes Orkney and Shetland, as well as the Highland Council local government area, the Western Isles and most of the Argyll and Bute and Moray local government areas. Highlands and Islands has, however, different meanings in different contexts. It means Highland (the local government area), Orkney, Shetland, and the Western Isles in Highlands and Islands Fire and Rescue Service. Northern, as in Northern Constabulary, refers to the same area as that covered by the fire and rescue service.
There have been trackways from the Lowlands to the Highlands since prehistoric times. Many traverse the Mounth, a spur of mountainous land that extends from the higher inland range to the North Sea slightly north of Stonehaven. The most well-known and historically important trackways are the Causey Mounth, Elsick Mounth, Cryne Corse Mounth and Cairnamounth.
Although most of the Highlands is geographically on the British mainland, it is somewhat less accessible than the rest of Britain; thus most UK couriers categorise it separately, alongside Northern Ireland, the Isle of Man, and other offshore islands. They thus charge additional fees for delivery to the Highlands, or exclude the area entirely. While the physical remoteness from the largest population centres inevitably leads to higher transit cost, there is confusion and consternation over the scale of the fees charged and the effectiveness of their communication, and the use of the word Mainland in their justification. Since the charges are often based on postcode areas, many far less remote areas, including some which are traditionally considered part of the lowlands, are also subject to these charges. Royal Mail is the only delivery network bound by a Universal Service Obligation to charge a uniform tariff across the UK. This, however, applies only to mail items and not larger packages which are dealt with by its Parcelforce division.
The Highlands lie to the north and west of the Highland Boundary Fault, which runs from Arran to Stonehaven. This part of Scotland is largely composed of ancient rocks from the Cambrian and Precambrian periods which were uplifted during the later Caledonian Orogeny. Smaller formations of Lewisian gneiss in the northwest are up to 3 billion years old. The overlying rocks of the Torridon Sandstone form mountains in the Torridon Hills such as Liathach and Beinn Eighe in Wester Ross.
These foundations are interspersed with many igneous intrusions of a more recent age, the remnants of which have formed mountain massifs such as the Cairngorms and the Cuillin of Skye. A significant exception to the above are the fossil-bearing beds of Old Red Sandstone found principally along the Moray Firth coast and partially down the Highland Boundary Fault. The Jurassic beds found in isolated locations on Skye and Applecross reflect the complex underlying geology. They are the original source of much North Sea oil. The Great Glen is formed along a transform fault which divides the Grampian Mountains to the southeast from the Northwest Highlands.
The entire region was covered by ice sheets during the Pleistocene ice ages, save perhaps for a few nunataks. The complex geomorphology includes incised valleys and lochs carved by the action of mountain streams and ice, and a topography of irregularly distributed mountains whose summits have similar heights above sea-level, but whose bases depend upon the amount of denudation to which the plateau has been subjected in various places.
Climate
The region is much warmer than other areas at similar latitudes (such as Kamchatka in Russia, or Labrador in Canada) because of the Gulf Stream making it cool, damp and temperate. The Köppen climate classification is "Cfb" at low altitudes, then becoming "Cfc", "Dfc" and "ET" at higher altitudes.
Places of interest
An Teallach
Aonach Mòr (Nevis Range ski centre)
Arrochar Alps
Balmoral Castle
Balquhidder
Battlefield of Culloden
Beinn Alligin
Beinn Eighe
Ben Cruachan hydro-electric power station
Ben Lomond
Ben Macdui (second highest mountain in Scotland and UK)
Ben Nevis (highest mountain in Scotland and UK)
Cairngorms National Park
Cairngorm Ski centre near Aviemore
Cairngorm Mountains
Caledonian Canal
Cape Wrath
Carrick Castle
Castle Stalker
Castle Tioram
Chanonry Point
Conic Hill
Culloden Moor
Dunadd
Duart Castle
Durness
Eilean Donan
Fingal's Cave (Staffa)
Fort George
Glen Coe
Glen Etive
Glen Kinglas
Glen Lyon
Glen Orchy
Glenshee Ski Centre
Glen Shiel
Glen Spean
Glenfinnan (and its railway station and viaduct)
Grampian Mountains
Hebrides
Highland Folk Museum – The first open-air museum in the UK.
Highland Wildlife Park
Inveraray Castle
Inveraray Jail
Inverness Castle
Inverewe Garden
Iona Abbey
Isle of Staffa
Kilchurn Castle
Kilmartin Glen
Liathach
Lecht Ski Centre
Loch Alsh
Loch Ard
Loch Awe
Loch Assynt
Loch Earn
Loch Etive
Loch Fyne
Loch Goil
Loch Katrine
Loch Leven
Loch Linnhe
Loch Lochy
Loch Lomond
Loch Lomond and the Trossachs National Park
Loch Lubnaig
Loch Maree
Loch Morar
Loch Morlich
Loch Ness
Loch Nevis
Loch Rannoch
Loch Tay
Lochranza
Luss
Meall a' Bhuiridh (Glencoe Ski Centre)
Scottish Sea Life Sanctuary at Loch Creran
Rannoch Moor
Red Cuillin
Rest and Be Thankful stretch of A83
River Carron, Wester Ross
River Spey
River Tay
Ross and Cromarty
Smoo Cave
Stob Coire a' Chàirn
Stac Polly
Strathspey Railway
Sutherland
Tor Castle
Torridon Hills
Urquhart Castle
West Highland Line (scenic railway)
West Highland Way (Long-distance footpath)
Wester Ross
This photo features a large statue of Buddha carved into the side of a mountain. The statue is prominently displayed, with the mountain serving as a stunning backdrop. A group of people is gathered around the statue, admiring the impressive artwork. There are at least 13 people visible in the scene, standing at various distances from the statue, some closer to the foreground and others further back.
In addition to the people, there are several handbags scattered throughout the scene, likely belonging to the visitors. Some of the handbags are placed near the people, while others are located closer to the statue. The overall atmosphere of the scene is one of awe and appreciation for the magnificent artwork and the breathtaking natural setting.
Summit goers arrive at the International Transport Forum's 2023 Summit on "Transport Enabling Sustainable Economies" in Leipzig, Germany on 24 May 2023.
The Firehydrant..chapter one..Busted..an excerpt from a story set in 1973/74
After that first court appearance in the Windsor courthouse I was sitting in the back of the paddy wagon being transported along with a few other criminals to the county bucket a five minute or so ride from the courthouse. I was still pretty high, if you look at it from a different perspective, I’d been high for about four or five years. Once, years earlier at the Don Gaol in Toronto, I was serving a four day weekend when these two cool hip looking Yankee dudes asked me what the prices were on the streets for weed and hash, shit like that. They had all the hippie trappings, long hair, hawk like features from looking over their shoulders too often. Briefly I thought maybe they were cops, plants, but they were Americans and had just left the O.R. in Guelph where they knew my buddy Coop de Grasser who was the head of the inmate committee at that time. I knew the difference in body language and voices from that of common pigs, they gave me that term, “we’ve been high for seven years, then we got busted” they had a Cheech and Chong quality about them especially in the eyes, they were crazies too, coming from California I could grasp their earlier introduction to the Herb.
Sitting in that wagon, (nic nac paddy whack, paddy wagon gonna take ya back, lock ya up and thro away the keys) handcuffed to some murderer or child molester, it just didn’t feel right, or seem right. I was not in the same criminal category as “those” criminals. They were bad, I just sold recreational drugs, which made people happy. I looked out the unmarked vans wired windows at some familiar sights. There was the Ambassador Bridge the Hippies at school had marched on the year before protesting for an end to the war in Vietnam while the Simon and Garfunkel song A Bridge Over Troubled Water played over loudspeakers. It was the same bridge Pete Kalci and self used to score the Hookers, buy the case of Ripple Wine, cross over to attend the Ravi Shankar and Traffic concerts. The very same bridge that took you to Ann Arbour and all the hip people living near those Michigan campuses. I was feeling greasy, very dirty, sweat was stinking up my armpits, my new blue leisure jacket was all wrinkled from being used as a pillow in the police station cell the night before where I once again carved the initials CTuna into the institutional paint.
Prison is a very sobering experience. That morning in the courtroom a man in his thirties, a violent robber, he threatened the people he robbed, gave them a smack with a gun to get their attention, you’d think this guy was rock solid, wouldn’t crack, no matter what. He started to ball when they gave him eight years in Federal Penitentiary, His lawyer had pleaded for leniency as he had a wife and a new baby on the way. You could tell the judge wasn’t swayed by this plea bargaining, he had to protect society from this monster repeat offender. Downstairs in the dungeon like remand cells I stayed away from him he was so emotionally distraught he might of lashed out at me.
You don’t get to pick your company in jail. At the county prison where I would be held for six weeks waiting for my trial and sentencing I was put through the usual routines, fingerprinted, again as I had already been fingerprinted at the police station the night before when I was arrested. At the county jail your clothes are taken from you and put in a bag with your name on them. The intake officer instructs you to have a shower in this big stall that was doorless. Afterwards you are instructed to stand there while a another officer sprays you for lice with a pressure mister that resembles a brass plant and weed sprayer similar to one you would use in your garden to kill bugs. All loose things like lighters, smokes, pills, cough candies, change, had been put into a manila envelope with your name on it at the police station downtown. This included my teacher/friends Don and Carol’s car keys to their car which I had parked on one of the upper floors at the Toronto Airport before taking the flight to Windsor. The paddy wagon driver another pink faced anglo saxon refugee handed that manila envelope over to the guard on duty when we arrived through the heavy steel gates and through a small brick lined tunnel into the courtyard of the very old county jail, the steel gates clanked shut automatically.
The desk guard had each of us answer some rudimentary questions, sex, race, age, education, religion, he looked startled and upset when he heard I was Taoist (pronounced Daoist). This was my spiritual flavour of the month, a Chinese faith based on the worship of Nature.
My bed for the next six weeks was located on the second tier of the three tiered old thick stone building built I would think in the last century. On this tier there were three other wards each ward holding a dozen cages/cells/cribs, each cell comprised of a steel bed a dull once stainless steel washbasin and a similar steel toilet without a seat, a piece of four inch square stainless steel was mounted above the sink, the mirror. The tier was designed to allow a single guard to patrol all four wards on the floor from the command centre located in the centre of the unit. There were always two guards on each floor one in the booth, the other always roaming. A roll of toilet paper had been issued to me as well as a cheap toothbrush and some tooth powder a threadbare facecloth and a towel big enough to dry your face and hands. A twenty five watt bulb glowed in the ceiling above, it would be on from six in the morning, till lights out at ten.
Home Sweet Home. My roommates were of various criminal backgrounds, there was a tall skinny biker with greasy yellow hair like the kind a worker at a wrecking yard might have, he was in for rape, his partner slept in the next set of cells, a portly unshaven fellow possibly related to a black bear or Kentucky mountain person, he was also in for rape, the two of them belonged to the Loners M.C, the local biker club. Next to me in the adjoining cell was a guy named Bill Hoskins who was quiet, had a scared look on his face, hadn’t shaved in a while, slightly receding, looked a bit like Garth Hudson of the Band, he was in on a smuggling marijuana charge and was not pleased with his circumstances. Little Mikey was the ward comic, shit disturber, go between, who was the one who bridged social classes and intermingled with all types, a chatterbox. There were a few quiet chaps and there was a young likeable guy all tattooed with crudely tattooed LOVE and HATE on his knuckles who it seemed had spent most of his young life in jail. He was just hoping to get sent to a prison in the area The Burtch Institution, he spoke of Burtch the way we would usually talk about home. Besides this motley crew there was one guy who everyone liked, I don’t recall his name, it might have been Jim he was coming down from using junk, he was dark haired and sort of reminded me of the Veteres from my youth, my neighbourhood Mt.Dennis, this Jim, he was street wise, quick to talk, he’d been around for his young twenty something age.
In very quick fashion a new person is sized up by the powers on the ward of any prison in any country, and it isn’t very long before the new prisoners place in the prison pack is established. For some reason my popularity irritated the power and after a few days I was asked to give the bad guys smokes while we were out in the small yard strolling around getting fresh air, I gave this some thought and passed out a few TMs as tailor made cigarettes were called but not without some resistance, the bikers weren’t very pleased to have a smart ass comparatively wealthy guy like myself around who might wrestle the minds of the weaker members of the pack from them.
As usual I became quite popular, my ability to tell stories and write stories about the fabled life in Toronto, the apartment building full of drugs (Rochdale) had every ones eyes bulging out. By this time two black brothers from Detroit were in the same ward with a minor infraction, they passed themselves off as bona fide black 'gangstas', I bought their story, they needed a connection to some crystal meth in TO and I turned them on to a pair of bikers who were living in the west end and whom I thought might appreciate the referral. As it was I had a list of phone numbers hidden in my shoes under the lining which along with some of my street clothes I was allowed to wear after they had been fumigated and cleaned since I was on remand and not yet officially a ward of the government. The black guys got bail fast, I never saw them again. Later in life the guys I referred them to paid me a visit as I worked the day shift at the Queensbury Arms, they weren’t pleased with my introduction. It could have been curtains for me, had I not been able to think on my feet. They thought the black guys may have been cops..
There was a crooked screw (guard) on the floor who for a price would smuggle in drugs and other contraband for those who had money and cravings. His name was Sidney and he was very tight with the diverse criminal element. In every prison man ever created there have been bent guards. Up to this time in life I had only known the soft side of Windsor, the niceties of the University scene, this was a much different perspective as the other folk I was now incarcerated with thought this situation as one of their schools of higher learning, a step in the ladder of criminality.
To help make time pass we played cards at the larger than picnic table sized metal tables that were bolted to the floor along with metal benches that were also bolted I suppose so no one would use them to hit each other with. A box shaped colour TV set sat in one corner of the ward. It was hung on one of those hospital style adjustable mounts and it was only put on at certain times, in the evenings from 7 to 10 or a bit later if something that was important was being shown. On weekends that TV might be on all day, starting with cartoons in the morning, which I recall quite a few of the people enjoying, then sports, and then hockey at night. There wasn’t much to do on weekends everybody’s routines ground to a halt.
The news story of the day was Richard Nixon’s impeachment from office. The previous year it seemed as if I had lost touch with events in the world. On reflection it may have been a lack of interest in the news that television and other media fed you. Lacking very many options at this time I began to join the herd and watched and laughed at All in The Family. The dreaded hockey games were on Saturday nights. Hockey is a Canadian staple and there were fierce conversations about various teams. Being so close to Detroit made for a lively rivalry, there weren’t as many teams in the league, it was an easier sport to appreciate.
Besides these time fillers I wrote pages and pages of short stories, some lyrical, like poems or songs. One in particular was a rhyming story about a “Gypsy Caravan” that parked under the full moon and where my lost love wept for me as I’d been sent to war. There were numerous verses and choruses, it was in my eyes a grand work. Several of the inmates would gather around the table as I would recite these stories, I recall Jim the Junkie giving the story his blessing and that was quite important for me as his sense of beauty and appreciation was different than the others. The other prisoners on remand held him in awe for some reason, he was like a Robin Hood type, a criminal All Star born and raised in Windsor. He got out on bail and a short while later word filtered back that he had died of an overdose of heroin and I always felt good that I had painted this nice scene for him of gypsies and love along a riverbank in golden days, like a Van Morrison lyric and his praise still ranks with the praise of others given me over the years.
Perhaps that is where my new nickname came from, that story about the gypsies. Around then someone tagged me with the title ‘Gypsy’ and it stuck right through my prison life. It took a while at first to get used to the new title, after all, nicknames were nothing new to me, as a kid I had been called Brooks by Bud Walford after Brooks Robinson the ballplayer with the Baltimore Orioles, Barb Sue Kevin and Shane often called me Weaver “Hey Weave” when we were younger playing cards on Victoria Blvd, then early on I used to carve my initials into the poured concrete sidewalks all over our area called Mount Dinky. C Tuna I would carve, using a stick or a piece of rock. Around this time there was a cartoon character called Charlie Tuna who was seen in tv advertisements for the Starkist Tuna company, there was a jingle with the ads and the ads were based on the premise that only the finest Tunas were good enough for Starkist customers and old Charlie a suave, Jackie Gleason type of Tuna with slicked back hair was always thrown back in to the sea. C Tuna was scraped also in the odd prison cell of Toronto’s #12, #31 and #52 Divisions as well as the gritty Don Gaol and now Windsor. One time, in Toronto I woke up from a drunken stupor and a police man at the #52 Divison asked me, “are you Charles Gregory aka C Tuna?” I replied I was, and was curtly charged with being drunk in a public place. I went back to sleep and was released in the morning, I couldn’t have been much more than sixteen.
My long relationship with the drink started around fifteen or so. While hanging out at Nick’s Pool Hall on Weston Road near Eglinton I met guys who were a bit older and liked to drink, especially on the weekends. An older guy named Bud a good pool player would go to the beer store and buy us a box of beer, I had developed a taste for it. Today, when I reflect on this behavior I have difficulty in recalling why I drank so much to the point often of blacking out as the consumption of beer became mixed with that of hard alcohol, whiskey, scotch etcetera. A common Saturday night would find me drinking a dozen beers with a mickey of Johnny Walker red as a chaser. At one time, I had been arrested six weekends in a row for drinking under age, drinking in a public place, drunk and disorderly…My mom was fed up bailing me out on Sunday mornings at the local police holding cells, located in the police stations, 31 division and 12 division. The fine for such behavior was usually $25 or $35 dollars or three days in jail. Not once do I recall anyone saying, this boy needs counseling. I may have been such a ‘tough nut’ that they felt it would have been a waste of time.
My friend George Holmes loved shouting out “here comes Tuna Fish” up at the corner of Keele and Eglinton during my greaseball period. This period took place between frat days and hippy days. Around town in my greaseball days that name C Tuna was recognizable up in the Junction, over on St Clair at Blackthorn and as well at Lansdowne and St Clair, also farther west towards Jane and Wilson and in Weston proper. I suppose the greasers up at Dufferin and Eglinton like Kenny Tanaka and Danny MacDonald had also known my AKA. It wasn’t that I was a prize fighter or anything a moniker was more a Title like that of a knight or a duke, sort of a right of passing, like a coming of age. Lots of guys had nick names just like the TV gangsters of the day, or the good guy bad guys in cowboy films. Names that quickly come to mind are, Hook, Coop de Grassser, Gooch, Scarecrow, Mars, Jake the Snake, Crazy Ivan, Fat Jack Hamilton, Mod, Vern the Tern, Dump, Butler, The Kid, Toot, Count, one guy, my friend Dave Wellwood had several nick names, The Goat, News, The General, Pee Wee and on and on.
Chassly Gangbusters was a favourite of the Hook and Coop years, Herbie used to like calling me Storch it was his invention he’d say it ‘Storch’ then back off a few steps in case I’d give him a smack, I always gave him a nasty sneer when he called me that. Charlie, Chuck, Chas, but almost never Charles. My name comes from a friend of my dads, Charles Bishop who died in the second war. Lately Schmiddy has been calling me the Kaliph of Keene which I really like. In the tradition of moms father Leon Yamel, actually Noel Lemay I’ve often tagged myself as Selrahc Yrogerg, this dates back to my saying words backwards while I waited to get on the field at the Smythe Park baseball league.
After a few days in the ward I could almost feel the drugs leaving my system and after two or three weeks I’d never been so clean, voluntarily. Even when I had the Hepatitis at Rochdale earlier that winter I was toking the finest hash and bud available. I must admit there was a new clarity to my mental comprehension, I could not adjust myself with other substances, alcohol included.
The food was awful, repetitive, I smoked like a chimney, there was a few hundred dollars in my pocket when I was picked up, I don’t recall the figure exactly. These funds in prison buy a lot of tobacco! To keep the peace I gave out as many smokes as required to avoid the bad guys wanting to shank me. We played cards night and day to pass the time, if anything I can remember that in particular, the time passing real slowly. That’s what more seasoned guys were saying that once you got where you were going, once you were sentenced you would find that your days took on structure and time was easier to do. This kind of time, waiting to be sentenced is called Dead Time and rightly so.
Michael Snyder the lawyer supplied free via the government legal aid program was a little lame in court during my first appearance. I took him aside and chewed him out. I wrote a letter to the court system, maybe the judge or the Attorney Generals Office, I’m not sure. The crooked screw Sidney read the letter and informed the lawyer of my dissatisfaction this got his attention and he did a fine job afterwards. I wonder if that letter ever made it out of that place.
Bill Hoskins as it turns out was in for a serious smuggling rap that he was not telling any of us about. He was on a sailing boat that had come up from the Bahamas area loaded with marijuana. The pot was hidden in false walls built into the customized ship, tons and tons of gange. As advisory counsel for my defense he nixed my hand written ten page dialogue about my historical accounting of the events leading up to my arrest, from the dysfunctional family situation with big Al at home which I used as my starting point in the dialogue, nixed the U.I.C. appeals process where I was cut off pogey for quitting my position without proper reason, nixed it all. He said to get a bunch of people to write letters who could speak for your good side, which in point of fact wasn’t so long ago, just the previous year I was bringing the teachers apples and cleaning the chalk off of the blackboards.
Turns out Sidney the crooked guard did me a favour by reading the mail that I had addressed to the law society and others regarding my lawyers lameness. When the lawyer caught wind of this he rushed in to appease me. Three weeks in the bucket passed and I was anxious to get on with things, when asked how I wished to plead it was a no brainer, I pled guilty. In court the judge found me guilty of all the charges, trafficking in narcotics, marijuana, hashish, peyote, acid, there was no blow left and I guess they didn’t bother to analyze the salt like crystal meth, there wasn’t much of it. I sat in the dock, again resolved, resolved not to break down and cry when sentenced like that other guy had done. I had to wait three more weeks for sentencing as the judge had asked for a pre-sentence report, which is like a record of your life, the details of your life, your failures and your successes if any. I recall finding this worrisome, although in my mind, having recently attended university under trying (at home) circumstances as a mature student, I felt I was on the right track, just jumped off the track momentarily.
That morning back in the court holding cells this big young Coloured man, I repeat, this was a big, strong athletic mean and angry twenty year old who wore those thick soled, tan coloured boots that motorcycle riders wore in the day, Fry Boots was their name. A diddler, a full grown twenty something farm kid from the sticks had just been returned to the holding cells in the basement of the court house, he walked with his head down, ashamed and afraid at the same time. As if in a movie the cell area was dimly lit an invitation for terror.
The farm kid went into a cell at the back of the block, none of the cell doors were locked. In court it came out that a couple of young girls had been molested the day before, quite young, under ten or so. You know how they say the jail system has its own way of getting folk, well this kid was in the wrong place at the wrong time. That big negro boy took his hatred out on that boy, he went into that cell and put the boots to the farm kids face, his gut, his balls, his legs, you name it, he got hit real hard. Nobody, no prisoner, no guard interfered I just watched stunned, I didn’t try to break it up, I just watched in my own kind of terror, that’s the way it can be in prison for diddlers they get no mercy, they are garbage. The guards very slowly came and broke it up, put the diddler in a solitary area, by this time his assailant had left the cell, he just brushed pass us all, me the other prisoners, the guards and took a seat in a cell holding his head in his hands, the screws never even bothered to ask what had happened, then we all went to the jailhouse in the paddy wagon, the diddler got separate transportation. Funny, I never saw that black guy again, he may have gone up to court and been given bail.
At the county bucket they put the diddler in a cell on my ward. That night we got him there as well but in a different way. Myself and others made a mixture of shit and piss, cold tea, spit and saliva, toilet water any vile substance we could find and poured it all over him as he lay in a back corner of the ward, not saying a word, afraid for his life, afraid to say anything, I mean we really humiliated him, I was a big part of this humiliation, this hazing, it was worse than a military blackballing. I’d been involved as a recipient in a mild fraternity hazing, I suppose that is where I got the idea. Over the years I’ve had a lot of remorse about this event but I still hold that this punishment, this prison tar and feathering was better than him losing his life, his balls or an eye or an ear.
They moved the big scared blonde haired blue eyed farm boy diddler from the ward that night put him into solitary confinement. In the visiting room the next day Frankie Herbert’s dad Frank Sr. came to visit, my first visit in nearly a month. Mr. Herbert worked as a travelling salesman for a big novelty company, he toured Ontario selling kitschy stuff like bingo markers, and roulette wheels and all sorts of things fundraising organizations use in their work and that large corporate stores stocked. At the same time Frank Sr. was visiting the diddler was visiting his dad, telling his dad through his pulverized face that I was one of his enemies, one of the perpetrators of his black eyes and bruises. That diddler, he don’t know how close he come to dying in that cell downtown. Frank Sr. he just looked at this farm kid with the shiners, looked at me, Frank Sr. he knew what the score was, he just shook his head, my father figure, surrogate dad visiting his son in gaol. Years earlier, Mr. Herbert had put up bail for me when the RCMP had placed a bag of pot in our groups car (actually a stretch Cadillac limo) as we tried to enter the Rockwood Festival. We had heard via the radio that everyone was getting busted that heading to the concert so we had stopped and stashed our goods in the woods, a ways from the entrance. The other five people were given bail but I was refused because of a previous minor offence. The charges were all thrown out in court later. I told the RCMP, this guy last name of Ryan, that if I saw him on the streets, I would kick the shit of him!
A couple of university school chums paid a visit one day after I had been sentenced, Tim, a bright musician type from the university showed up with my old baked and breaded sardine dinner girlfriend, Mary Lewis. That was kind of them to show up at that depressing place, it was the last time I ever saw or heard from them except when I contacted Mary Lewis and she sent me a year book from the university. A book I looked at maybe twice then mysteriously wrapped in several windings of masking tape for thirty years and hid in a milk crate with several old photo albums on top, securing its hiding place, was that my soul in that book? Who was that guy?
Bill the Smuggler had a birthday card sent in from someone on the outside, in the card, on the nose of the clown they had poured some liquid LSD and Bill did some, offered me a taste, I declined, felt the surroundings not conducive to a good trip. Bill laid some on the bikers to secure their loyalty. Now here you have these three or four biker types running around all looney, higher than kites, grooving to the little AM radio playing in the corner, digging the tunes, staring at hallucinations only they could see. In a way it was like the lawyer in Easy Rider getting turned on, except these were bad guys, getting all soft and mushy, I stayed in my crib that night until the party settled down. I think I was scared the bikers might be able (through the power of acid) be able to see my true feelings for them. Like many a night I read to sleep. Dostoyevsky offered imaginable experiences to escape to.
Next day in the yard the bikers were hovering together, conspiring, they were good at that, at joining forces, intimidation by numbers. At some point this middle aged black inmate took an epileptic fit, started shaking all over, fell to the ground, I thought he had been shot, the guards blew their stupid whistles they thought someone had beaten the guy up. We all had to stand at attention while the screws came and took the fellow away on a stretcher. It was a cool forty five degree F morning, the sun was shining. The heavy grey cloth winter coats we’d been issued had to be turned in when we went back inside, it felt so good being out in the yard, the fresh air, the bit of Spring green showing on the small lawn. Another inmate pointed out where they used to do the hangings, there remained a shuttered doorway a few levels up I was also shown where they used to bury the bodies they had hung, this was becoming a real adult experience.
Freddy is an old US Postal Service delivery truck that has been re-purposed as a Belgian Waffle Truck by my good friends at "Belgian Waffle Crafters". Their truck is serving original Belgian Liège Waffles around the Raleigh/Durham area in North Carolina.
Check out his full story here:
belgianwafflecrafters.com/meet-freddy/
This LEGO model features 2 sliding doors, an opening boot and hood with engine detailing. The engine can be accessed from the hood or from inside the truck by opening an access cover - just like in the real truck (I believe this was done to make the engine easier to access and service). The food truck equipment includes 3 waffle casts, 2 sinks and an opening fridge... and of course the side hatch that can opened/closed.
See the full album here.
An orange cat is lazily resting with its head down on a stack of red blankets. The background features a textured surface and blurred furniture.
The Ford Consul Capri was a two-door coupé version of the Classic saloon made by Ford of Britain.
The Capri Project was code named "Sunbird" and took design elements from the Ford Thunderbird and the Ford Galaxie Starliner. It was instigated by Sir Horace Denne, Ford's Sales Director. He wanted a "co-respondent's" car to add glamour to the product line. It was designed by Charles Thompson who worked under Neale and had sweeping lines, a large boot space and a pillarless coupé roof.
On its September announcement the Consul Capri was for export only but went on sale to the domestic British market in January 1962. The bodies were sub-assembled by Pressed Steel Company, with only final assembly of the drivetrain taking place at Dagenham and from February 1963 at Halewood. It was intended as part of the Ford Classic range of cars but the body was complex and expensive to produce. With new production methods, time demands from Dearborn and a need to match opposition manufacturers in price, the Ford Classic and Consul Capri were almost doomed from the start. The Ford Classic was made from 1961 to 1963, and replaced by the Cortina-derived Ford Corsair.
The Consul Capri included Ford Classic De-Luxe features, including four headlights, variable speed wipers, 9.5 in (241 mm) front disc brakes, dimming dashboard lights, and a cigar lighter. The four-speed transmission was available with either a column or floor change. It was proclaimed as "The First Personal car from Ford of Great Britain" (Ford of Great Britain, sales literature, December 1961)
Initially fitted with a 1340 cc 3 main bearing engine (model 109E), the early cars were considered underpowered and suffered from premature crankshaft failure. Engine capacity was increased in August 1962 to 1498 cc (model 116E) and this engine with its new 5 bearing crankshaft was a vast improvement. The first 200 Capris were left-hand-drive cars for export including Europe and North America. In Germany at the 1961 Frankfurt Auto Show, Ford sold 88 Capris.
The Sanctury of the St Kilda Presbyterian Church features three beautiful 1880s Ferguson and Urie stained glass windows; Faith on the left, Charity in the middle and Hope on the right. All are executed in iridescent reds, yellows, greens and blues, to reflect the colour palate used in other Ferguson and Urie windows elsewhere around the church.
Built on the crest of a hill in a prominent position overlooking St Kilda and the bay is the grand St Kilda Presbyterian Church.
The St Kilda Presbyterian Church's interior is cool, spacious and lofty, with high ceilings of tongue and groove boards laid diagonally, and a large apse whose ceiling was once painted with golden star stenciling. The bluestone walls are so thick that the sounds of the busy intersection of Barkley Street and Alma Road barely permeate the church's interior, and it is easy to forget that you are in such a noisy inner Melbourne suburb. The cedar pews of the church are divided by two grand aisles which feature tall cast iron columns with Corinthian capitals. At the rear of the building towards Alma Road there are twin porches and a narthex with a staircase that leads to the rear gallery where the choir sang from. It apparently once housed an organ by William Anderson, but the space today is used as an office and Bible study area. The current impressive Fincham and Hobday organ from 1892 sits in the north-east corner of the church. It cost £1030.00 to acquire and install. The church is flooded with light, even on an overcast day with a powerful thunder storm brewing (as the weather was on my visit). The reason for such light is because of the very large Gothic windows, many of which are filled with quarry glass by Ferguson and Urie featuring geometric tracery with coloured borders. The church also features stained glass windows designed by Ferguson and Urie, including the impressive rose window, British stained glass artist Ernest Richard Suffling, Brooks, Robinson and Company Glass Merchants, Mathieson and Gibson of Melbourne and one by Australian stained glass artist Napier Waller.
Opened in 1886, the St Kilda Presbyterian church was designed by the architects firm of Wilson and Beswicke, a business founded in 1881 by Ralph Wilson and John Beswicke (1847 - 1925) when they became partners for a short period. The church is constructed of bluestone with freestone dressings and designed in typical Victorian Gothic style. The foundation stone, which may be found on the Alma Road facade, was laid by the Governor of Victoria Sir Henry Barkly on 27 January. When it was built, the St Kilda Presbyterian Church was surrounded by large properties with grand mansions built upon them, so the congregation were largely very affluent and wished for a place of worship that reflected its stature not only in location atop a hill, but in size and grandeur.
The exterior facades of the church on Barkley Street and Alma Road are dominated by a magnificent tower topped by an imposing tower. The location of the church and the height of the tower made the spire a landmark for mariners sailing into Melbourne's port. The tower features corner pinnacles and round spaces for the insertion of a clock, which never took place. Common Victorian Gothic architectural features of the St Kilda Presbyterian Church include complex bar tracery over the windows, wall buttresses which identify structural bays, gabled roof vents, parapeted gables and excellent stone masonry across the entire structure.
I am very grateful to the Reverend Paul Lee for allowing me the opportunity to photograph the interior of the St Kilda Presbyterian Church so extensively.
The architects Wilson and Beswicke were also responsible for the Brighton, Dandenong, Essendon, Hawthorn and Malvern Town Halls and the Brisbane Wesleyan Church on the corner of Albert and Ann Streets. They also designed shops in the inner Melbourne suburbs of Auburn and Fitzroy. They also designed several individual houses, including "Tudor House" in Williamstown, "Tudor Lodge" in Hawthorn and "Rotha" in Hawthorn, the latter of which is where John Beswicke lived.
The stained glass firm of Ferguson and Urie was established by Scots James Ferguson (1818 – 1894), James Urie (1828 – 1890) and John Lamb Lyon (1836 – 1916). They were the first known makers of stained glass in Australia. Until the early 1860s, window glass in Melbourne had been clear or plain coloured, and nearly all was imported, but new churches and elaborate buildings created a demand for pictorial windows. The three Scotsmen set up Ferguson and Urie in 1862 and the business thrived until 1899, when it ceased operation, with only John Lamb Lyon left alive. Ferguson and Urie was the most successful Nineteenth Century Australian stained glass window making company. Among their earliest works were a Shakespeare window for the Haymarket Theatre in Bourke Street, a memorial window to Prince Albert in Holy Trinity, Kew, and a set of Apostles for the West Melbourne Presbyterian Church. Their palatial Gothic Revival office building stood at 283 Collins Street from 1875. Ironically, their last major commission, a window depicting “labour”, was installed in the old Melbourne Stock Exchange in Collins Street in 1893 on the eve of the bank crash. Their windows can be found throughout the older suburbs of Melbourne and across provincial Victoria.
Windows 10 Has Launched Read Its Features Before Install And Also Learn How To Upgrade It
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www.dcmot.com/windows-10-has-launched-read-its-features-b...
MEXICO CITY, MEXICO - SEPTEMBER 27: Kim "Deft" Hyuk-kyu of DRX poses at the League of Legends World Championship Play-Ins Features Day on September 27, 2022 in Mexico City, Mexico. (Photo by Colin Young-Wolff/Riot Games)
Installed in 1892, the George Wilson memorial stained glass window was designed by British stained glass artist Ernest Richard Suffling (1855 - 1911) of Edgware Road, London. Looking out onto Barkley Street, the stained glass window features Jesus walking on the water as he calms the storm for his disciples from the Book of Matthew. The window features an angel at the bottom of each pane holding a scroll. One says: "It is I, be not afraid" whilst the other says: "Lord save me, or I perish". The window's octofoil features two angels with a scroll bearing the words: "Be of good cheer" which is from the same section of the Book of Matthew as the calming of the storm by Jesus. The colours in this window are especially rich, not least the vivid red and gold robes of Jesus and the shades of the water upon which he stands.
Built on the crest of a hill in a prominent position overlooking St Kilda and the bay is the grand St Kilda Presbyterian Church.
The St Kilda Presbyterian Church's interior is cool, spacious and lofty, with high ceilings of tongue and groove boards laid diagonally, and a large apse whose ceiling was once painted with golden star stenciling. The bluestone walls are so thick that the sounds of the busy intersection of Barkley Street and Alma Road barely permeate the church's interior, and it is easy to forget that you are in such a noisy inner Melbourne suburb. The cedar pews of the church are divided by two grand aisles which feature tall cast iron columns with Corinthian capitals. At the rear of the building towards Alma Road there are twin porches and a narthex with a staircase that leads to the rear gallery where the choir sang from. It apparently once housed an organ by William Anderson, but the space today is used as an office and Bible study area. The current impressive Fincham and Hobday organ from 1892 sits in the north-east corner of the church. It cost £1030.00 to acquire and install. The church is flooded with light, even on an overcast day with a powerful thunder storm brewing (as the weather was on my visit). The reason for such light is because of the very large Gothic windows, many of which are filled with quarry glass by Ferguson and Urie featuring geometric tracery with coloured borders. The church also features stained glass windows designed by Ferguson and Urie, British stained glass artist Ernest Richard Suffling, Brooks, Robinson and Company Glass Merchants, Mathieson and Gibson of Melbourne and one by Australian stained glass artist Napier Waller.
Opened in 1886, the St Kilda Presbyterian church was designed by the architects firm of Wilson and Beswicke, a business founded in 1881 by Ralph Wilson and John Beswicke (1847 - 1925) when they became partners for a short period. The church is constructed of bluestone with freestone dressings and designed in typical Victorian Gothic style. The foundation stone, which may be found on the Alma Road facade, was laid by the Governor of Victoria Sir Henry Barkly on 27 January. When it was built, the St Kilda Presbyterian Church was surrounded by large properties with grand mansions built upon them, so the congregation were largely very affluent and wished for a place of worship that reflected its stature not only in location atop a hill, but in size and grandeur.
The exterior facades of the church on Barkley Street and Alma Road are dominated by a magnificent tower topped by an imposing tower. The location of the church and the height of the tower made the spire a landmark for mariners sailing into Melbourne's port. The tower features corner pinnacles and round spaces for the insertion of a clock, which never took place. Common Victorian Gothic architectural features of the St Kilda Presbyterian Church include complex bar tracery over the windows, wall buttresses which identify structural bays, gabled roof vents, parapeted gables and excellent stone masonry across the entire structure.
I am very grateful to the Reverend Paul Lee for allowing me the opportunity to photograph the interior of the St Kilda Presbyterian Church so extensively.
The architects Wilson and Beswicke were also responsible for the Brighton, Dandenong, Essendon, Hawthorn and Malvern Town Halls and the Brisbane Wesleyan Church on the corner of Albert and Ann Streets. They also designed shops in the inner Melbourne suburbs of Auburn and Fitzroy. They also designed several individual houses, including "Tudor House" in Williamstown, "Tudor Lodge" in Hawthorn and "Rotha" in Hawthorn, the latter of which is where John Beswicke lived.
Ernest Richard Suffling (1855 - 1911) was a stained glass artist based in London. He was also a prolific writer, publishing "The Art of Glass Painting" in 1902, as well as books on the Norfolk Broads and Epitaphs.
This Teeshirtales clip features my talented Nephew Ali Jerome who along with is partner Lamar Callaghan authored and illustrated "Kickin It Kids" Enter the Rapscallion a Hip-Hop Space Odyssey--about kids representing the four elements of hip-hop who inhabit super-powers. Of course Ali wears a tee he created with a pic from the book--available on Amazon, Barnes & Nobles.com and Kindle
#teeshirttales
Full Video can be seen on my Youtube channel:
www.youtube.com/channel/UCoWpDDCSGsn8MW9p3f5KzuQ
(animation & photos provided by Ali Jerome)
video Produced/directed & edited by JuliaO
Grotesque and gargoyle are architectural features that are very similar, but are different in a subtle way.
A grotesque is a carved animal or human attached to a building that is merely decorative and does not serve any other function.
Grotesques are found on churches and other buildings such as university halls. The word grotesque generally means something that is distorted to an appalling degree, a caricature.
Grotesque is derived from the Italian word grottegargoysco, which means of the cave. This refers to paintings found in Roman ruins.
A gargoyle is a carved animal or human attached to a building that acts as a water spout. Directing the water away from the walls of a building counteracts erosion.
Gargoyles are most often associated with medieval cathedrals.
The word gargoyle is derived from the Old French word gargouille, which means throat.
This refers to the water moving through the spout or throat of the figure.
So there you have it!
The Dunnock looks perfectly at home beside him eh? 😁
+++ DISCLAIMER +++
Nothing you see here is real, even though the conversion or the presented background story might be based on authentic facts. BEWARE!
Some background:
The VF-1 was developed by Stonewell/Bellcom/Shinnakasu for the U.N. Spacy by using alien Overtechnology obtained from the SDF-1 Macross alien spaceship. Its production was preceded by an aerodynamic proving version of its airframe, the VF-X. Unlike all later VF vehicles, the VF-X was strictly a jet aircraft, built to demonstrate that a jet fighter with the features necessary to convert to Battroid mode was aerodynamically feasible. After the VF-X's testing was finished, an advanced concept atmospheric-only prototype, the VF-0 Phoenix, was flight-tested from 2005 to 2007 and briefly served as an active-duty fighter from 2007 to the VF-1's rollout in late 2008, while the bugs were being worked out of the full-up VF-1 prototype (VF-X-1).
The space-capable VF-1's combat debut was on February 7, 2009, during the Battle of South Ataria Island - the first battle of Space War I - and remained the mainstay fighter of the U.N. Spacy for the entire conflict. Introduced in 2008, the VF-1 would be out of frontline service just five years later, though.
The VF-1 proved to be an extremely capable craft, successfully combating a variety of Zentraedi mecha even in most sorties which saw UN Spacy forces significantly outnumbered. The versatility of the Valkyrie design enabled the variable fighter to act as both large-scale infantry and as air/space superiority fighter. The signature skills of U.N. Spacy ace pilot Maximilian Jenius exemplified the effectiveness of the variable systems as he near-constantly transformed the Valkyrie in battle to seize advantages of each mode as combat conditions changed from moment to moment.
The basic VF-1 was deployed in four minor variants (designated A, D, J, and S) and its success was increased by continued development of various enhancements including the GBP-1S "Armored" Valkyrie, FAST Pack "Super" Valkyrie and the additional RÖ-X2 heavy cannon pack weapon system for the VF-1S for additional firepower.
The FAST Pack system was designed to enhance the VF-1 Valkyrie variable fighter, and the initial V1.0 came in the form of conformal pallets that could be attached to the fighter’s leg flanks for additional fuel – primarily for Long Range Interdiction tasks in atmospheric environment. Later FAST Packs were designed for space operations.
The following FAST Pack 2.0 system featured two 120.000 kg class P&W+EF-2001 booster thrusters (mounted on the dorsal section of the VF-1) and two CTB-04 conformal propellant/coolant tanks (mounted on the leg/engines), since the VF-1's internal tanks could not carry enough propellant to achieve a stable orbit from Earth bases and needed the help of a booster pack to reach Low Earth Orbit. Anyway, the FAST Pack 2.0 wasn't adapted for atmospheric use, due to its impact on a Valkyrie's aerodynamics and its weight; as such, it needed to be discarded before atmospheric entry.
Included in the FAST Pack boosters and conformal tanks were six high-maneuverability vernier thrusters and two low-thrust vernier thrusters beneath multipurpose hook/handles in two dorsal-mounted NP-BP-01, as well as ten more high-maneuverability vernier thrusters and two low-thrust vernier thrusters beneath multipurpose hook/handles in the two leg/engine-mounted NP-FB-01 systems.
Granting the VF-1 a significantly increased weapons payload as well as greater fuel and thrust, Shinnakasu Heavy Industry's FAST Pack system 2.0 was in every way a major success in space combat. The first VF-1 equipped with FAST Packs was deployed in January 2010 for an interception mission.
Following first operational deployment and its effectiveness, the FAST Pack system was embraced enthusiastically by the U.N. Spacy and found wide use. By February 2010, there were already over 300+ so-called "Super Valkyries" stationed onboard the SDF-1 Macross alone.
The FAST Pack went through constant further development, including upgraded versions for late production and updated VF-1s (V3.0 and V4.0). Another addition to the early V2.0 variant of 2010 was the so-called “S-FAST Pack”. The S-FAST pack was originally developed at the Apollo lunar base, for the locally based VF-1 interceptor squadrons that were tasked with the defense of this important production and habitat site on the Moon, but it also found its way to other orbital stations and carriers.
Officially designated FAST Pack V2.1, the S-FAST Pack consisted of the standard pair of dorsal rocket boosters plus the pallets with additional maneuvering jets, sensors and weapons. The S-FAST pack added another pair of P&W+EF-2001 boosters under the inner wings, having the duty to give to fighter the power necessary to exit easily from the gravity of moons or little planets without atmosphere, and improve acceleration during combat situations. Range was also further extended, together with additional life support systems for prolonged deep space operations, or the case of emergency.
In order to accept the S-FAST pack and exploit its potential, the VF-1’s wings and inner wing attachment points had to be strengthened due to the additional load and propulsion. The use of the S-FAST pack also precluded the fighter from transforming into Battroid or Gerwalk mode – the underwing packs had to be jettisoned beforehand. The other standard FAST Pack 2.0 elements could still be carried, though.
The modfied Valkyries capable of accepting the S-FAST Pack received an additional “S” to their type designation – more than 100 VF-1s were converted or built in this deep space configuration until late 2011. Initial deployment of the S-FAST Pack was conducted through SVF-24 “Moon Shadows” in early 2010, a unit that was quickly disbanded, though, but re-formed as SVF-124 “Moon Shooters”, tasked with the defense of the lunar Apollo Base and several special missions.
After the end of Space War I, the VF-1 continued to be manufactured both in the Sol system and throughout the UNG space colonies. Although the VF-1 would eventually be replaced as the primary Variable Fighter of the U.N. Spacy by the more capable, but also much bigger, VF-4 Lightning III in 2020, a long service record and continued production after the war proved the lasting worth of the design.
The VF-1 was without doubt the most recognizable variable fighter of Space War I and was seen as a vibrant symbol of the U.N. Spacy even into the first year of the New Era 0001 in 2013. At the end of 2015 the final rollout of the VF-1 was celebrated at a special ceremony, commemorating this most famous of variable fighters. The VF-1 Valkryie was built from 2006 to 2013 with a total production of 5,459 VF-1 variable fighters with several variants (VF-1A = 5,093, VF-1D = 85, VF-1J = 49, VF-1S = 30, VF-1G = 12, VE-1 = 122, VT-1 = 68)
However, the fighter remained active in many second line units and continued to show its worthiness years later, e. g. through Milia Jenius who would use her old VF-1 fighter in defense of the colonization fleet - 35 years after the type's service introduction!
General characteristics:
All-environment variable fighter and tactical combat Battroid,
used by U.N. Spacy, U.N. Navy, U.N. Space Air Force
Accommodation:
Pilot only in Marty & Beck Mk-7 zero/zero ejection seat
Dimensions:
Fighter Mode:
Length 14.23 meters
Wingspan 14.78 meters (at 20° minimum sweep)
Height 3.84 meters
Battroid Mode:
Height 12.68 meters
Width 7.3 meters
Length 4.0 meters
Empty weight: 13.25 metric tons;
Standard T-O mass: 18.5 metric tons;
MTOW: 37.0 metric tons
Power Plant:
2x Shinnakasu Heavy Industry/P&W/Roice FF-2001 thermonuclear reaction turbine engines, output 650 MW each, rated at 11,500 kg in standard or in overboost (225.63 kN x 2)
4 x Shinnakasu Heavy Industry NBS-1 high-thrust vernier thrusters (1 x counter reverse vernier thruster nozzle mounted on the side of each leg nacelle/air intake, 1 x wing thruster roll control system on each wingtip);
18 x P&W LHP04 low-thrust vernier thrusters beneath multipurpose hook/handles
The S-FAST Pack added 4x P&W+EF-2001 booster thrusters with 120.000 kg each, plus a total of 28x P&W LHP04 low-thrust vernier thrusters
Performance:
Battroid Mode: maximum walking speed 160 km/h
Fighter Mode: at 10,000 m Mach 2.71; at 30,000+ m Mach 3.87
g limit: in space +7
Thrust-to-weight ratio: empty 3.47; standard T-O 2.49; maximum T-O 1.24
Design Features:
3-mode variable transformation; variable geometry wing; vertical take-off and landing; control-configurable vehicle; single-axis thrust vectoring; three "magic hand" manipulators for maintenance use; retractable canopy shield for Battroid mode and atmospheric reentry; option of GBP-1S system, atmospheric-escape booster, or FAST Pack system
Transformation:
Standard time from Fighter to Battroid (automated): under 5 sec.
Min. time from Fighter to Battroid (manual): 0.9 sec.
Armament:
2x internal Mauler RÖV-20 anti-aircraft laser cannon, firing 6,000 pulses per minute
1x Howard GU-11 55 mm three-barrel Gatling gun pod with 200 RPG, fired at 1,200 rds/min
4x underwing hard points for a wide variety of ordnance, including
12x AMM-1 hybrid guided multipurpose missiles (3/point), or
12x MK-82 LDGB conventional bombs (3/point), or
6x RMS-1 large anti-ship reaction missiles (2/outboard point, 1/inboard point), or
4x UUM-7 micro-missile pods (1/point) each carrying 15 x Bifors HMM-01 micro-missiles,
or a combination of above load-outs
The optional Shinnakasu Heavy Industry S-FAST Pack 2.1 augmentative space weapon system added:
6x micro-missiles in two NP-AR-01 micro-missile launcher pods (mounted rear-ward under center ventral section in Fighter mode or on lower arm sections in GERWALK/Battroid mode)
4x12 micro missiles in four HMMP-02 micro-missile launchers, one inside each booster pod
The kit and its assembly:
This VF-1 is another contribution to the “Old Kit” Group Build at whatifmodelers.com, running in late 2016. I am not certain about the moulds’ inception date, but since it is an ARII incarnation of this type of kit and even moulded in the early pastel green styrene, I’d think that it was produced in 1982 or 83.
Anyway, I love the Macross VF-1, IMHO a design masterpiece created by Shoji Kawamori and one of my favorite mecha designs ever, because it was created as a late 70ies style jet fighter that could transform into a robot in a secondary role. As a simple, purposeful military vehicle. And not like a flashy robot toy.
Effectively, this Super Valkyrie is a highly modified OOB kit with many donation parts, and this kit is a bit special, for several reasons. There are several 1:100 OOB kits with FAST Packs from ARII/Bandai available (and still around today), but these are normally only Battroids or Gerwalks with additional parts for the FAST kit conversion. The kit I used here is different: it is, after maybe 25 years of searching and building these kits, the #70 from the original production run. It is (so far!) the only Fighter mode kit with the additional FAST Pack parts! Must be rare, and I have never seen it in catalogues?
Until today, I converted my Super or Strike Valkyries from Gerwalk kits, a task that needs some improvisation esp. around the folded arms between the legs, and there’s no OOB option for an extended landing gear. The latter made this Fighter mode kit very attractive, even though the actual kit is pretty disappointing, and AFAIK this kit variant is only available as a VF-1S.
With the Super Valkyrie fighter kit you receive basically a Gerwalk with a standard fighter cockpit (which includes a front wheel well and an extended front wheel leg), plus extra parts. The leg/engine-mounted NP-FB-01 systems are less bulbous than the parts on the Gerwalk or Battroid kit, and the OOB dorsally mounted NP-BP-01 boosters are TINY, maybe 1:120 or even 1:144! WTF?
Further confusion: the kit includes a set of lower arm parts with integrated rocket launchers, but these are not necessary at all for the Fighter build?! As a kind of compensation there’s a new and exclusive element that simulates the folded arms under the ‘fuselage’ and which, as an added value, properly holds the hand gun under the fuselage. As a quirky flaw, though, the hand gun itself comes in the extended form for the Battroid/Gerwalk mode. For the fighter in flight mode, it has to be modified, but that’s easily done.
Anyway, with the potential option to build a Super Valkyrie with an extended landing gear, this was my route to go with this vintage kit. The Super Valkyrie already looks bulky with the FAST Pack added, but then I recently found the S-FAST Pack option with two more boosters under the wings – total overkill, but unique. And I had a spare pair of booster bulks in the stash (w/o their nozzles, though), as well as a complete pair of additional bigger standard FAST boosters that could replace the ridiculous OOB parts…
Building such a Super/Strike Valkyrie means building separate components, with a marriage of parts as one of the final steps. Consequently, cockpit, central fuselage with the wings and the air intakes, the folded stabilizer pack, the folded arms element with the handgun, the two legs and the four boosters plus other ordnance had to be built and painted separately.
Here and there, details were changed or added, e. g. a different head (a ‘J’ head for the flight leader’s aircraft with two instead of the rare, OOB ‘S’ variant with four laser cannon), covers for the main landing gear (the latter does not come with wells at all, but I did not scratch them since they are hardly recognizable when the kit is sitting on the ground), the typical blade aerials under the cockpit and the feet had to be modified internally to become truly ‘open’ jet exhausts.
The wing-mounted boosters received new nozzles and their front end was re-sculpted with 2C putty into a square shape, according to reference sketches. Not 100% exact, but the rest of the VF-1 isn’t either.
This VF-1 was also supposed to carry external ordnance and my first choice were four wing-mounted RMS-1 Anti-Ship Reaction Warheads, scratched from four 1.000 lb NATO bombs. But, once finished, I was not happy with them. So I looked for another option, and in a source book I found several laser-guided bombs and missiles, also for orbital use, and from this inspiration comes the final ordnance: four rocket-propelled kinetic impact projectiles. These are actually 1:72 JASDF LGB’s from a Hasegawa weapon set, sans aerodynamic steering surfaces and with rocket boosters added to the tail. Also not perfect, but their white color and sleek shape is a good counterpart to the FAST elements.
Experience from many former builds of this mecha kit family helped a lot, since the #70 kit is very basic and nothing really fits well. Even though there are not many major seams or large elements, PSR work was considerable. This is not a pleasant build, rather a fight with a lot of compromises and semi-accuracies.
Seriously, if you want a decent 1:100 VF-1, I’d rather recommend the much more modern WAVE kits (including more realistic proportions).
Painting and markings:
The paint scheme for this Super Valkyrie was settled upon before I considered the S-FAST Pack addition: U.N. Spacy’s SVF-124 is authentic, as well as its unique camouflage paint scheme.
The latter is a special scheme for the lunar environment where the unit was originally formed and based, with all-black undersides, a high, wavy waterline and a light grey upper surface, plus some medium grey trim and a few colorful US Navy style markings and codes.
My core reference is a ‘naked’ bread-and-butter VF-1A of SVF-124 in Fighter mode, depicted as a profile in a VF-1 source book from SoftBank Publishing. The colors for the FAST Pack elements are guesstimates and personal interpretations, though, since I could not find any reference for their look in this unit.
As a side note, another, later SVF-124 aircraft in a similar design is included as an option in a limited edition 1:72 VF-22S kit from Hasegawa, which is backed by CG pics in a VF-22 source book from Softbank, too.
Furthermore, SVF-124 finds mention in a Japanese modeler magazine, where the aforementioned VF-22S kit was presented in 2008. So there must be something behind the ‘Moon Shooters’ squadron.
According to the Hasegawa VF-22S’s painting instructions, the underside becomes black and the upper surfaces are to be painted with FS36270 (with some darker fields on the VF-22, though, similar to the USAF F-15 counter-shaded air superiority scheme, just a tad darker).
Due to the 1:100 scale tininess of my VF-1, I alternatively went for Revell 75 (RAL 7039), which is lighter and also has a brownish hue, so that the resulting aircraft would not look too cold and murky, and not resemble an USAF aircraft.
All FAST Pack elements were painted in a uniform dark grey (Humbrol 32), while some subtle decorative trim on the upper surfaces, e.g. the canopy frame, an anti-glare panel and a stripe behind the cockpit and decoration trim on the wings’ upper surfaces, was added with Revell 77 (RAL 7012). Overall, colors are rather dull, but IMHO very effective in the “landscape” this machine is supposed to operate, and the few colorful markings stand out even more!
The cockpit interior was painted in a bluish grey, with reddish brown seat cushions (late 70ies style!), and the landing gear became all white. For some added detail I painted the wings’ leading edges in a mustard tone (Humbrol 225, Mid Stone).
The kit received some weathering (black ink wash, drybrushing on panels) and extra treatment of the panel lines – even though the FAST Pack elements hide a lot of surface or obscure view.
More color and individuality came with the markings. The standard decals like stencils or the U.N. Spacy insignia come from the kit’s and some other VF-1s’ OOB sheets.
Based on the SVF-124 VF-1 profile and taking the basic design a bit further, I used dull red USAF 45° digits for the 2nd flight leader’s “200” modex and the Apollo Base’s code “MA” on the dorsal boosters. Some discreet red trim was also applied to the FAST Packs – but only a little.
Since all of SVF-124’s aircraft are rumored to carry personal markings, including nose art and similar decorations, I tried to give this VF-1JS a personal note: the pin-up badges on the dorsal boosters come from a Peddinghouse decal sheet for Allied WWII tanks, placed on a silver roundel base. Unfortunately (and not visible before I applied them) the pin-up decal was not printed on a white basis, so that the contrast on the silver is not very strong, but I left it that way. Additionally, the tagline “You’re a$$ next, Jerry” (which IS printed in opaque white…?) was added next to the artwork – but it’s so tiny that you have to get really close to decipher it at all…
Finally, after some soot stains around the exhausts and some vernier nozzels with graphite, the kit received a coat of matt acrylic varnish.
Building this vintage VF-1 kit took a while and a lot of effort, but I like the result: with the S-FAST Pack, the elegant VF-1 turned into a massive space fighter hulk! The normal Super Valkyries already look very compact and purposeful, but this here is truly menacing. Especially when standing on its own feet/landing gear, with its nose-down stance and the small, original wheels, this thing reminds of a Space Shuttle that had just landed.
Good that I recently built a simple VF-1 fighter as a warm-up session. ARII’s kit #70 is not a pleasant build, rather a fight with the elements and coupled with a lot of compromises – if you want a Super Valkyrie Fighter in 1:100, the much more modern WAVE kit is IMHO the better option (and actually not much more pricey than this vintage collector’s item). But for the vintage feeling, this exotic model kit was just the right ticket, and it turned, despite many weaknesses and rather corny details, into an impressive fighter. Esp. the lunar camouflage scheme looks odd, but very unique and purposeful.
Anyway, with so many inherent flaws of the ARII kit, my former method of converting a pure (and much more common) Gerwalk kit into a space-capable VF-1 fighter is not less challenging and complicated than trying to fix this OOB option into a decent model. :-/
She makes small parathas in her toy plate...and a moment of greatest happiness can be felt around her...the moment she could get one..done:)special moment of wonderful kids....are not to be missed..Mar 2010
This photo features cousins Paul Raatz and Herb Dietsche with a buck that Herb shot here in Wisconsin in the late 1930's.
This photo features a woman with black hair, wearing a brown shirt, standing on a beach. She is posing for the camera, with her hair blowing in the wind. The woman is also wearing a necklace and a watch on her wrist.
In the background, there are several other people scattered around the beach, enjoying the outdoor environment. A handbag can be seen placed on the ground near the woman, possibly belonging to her.
Warner Bros Studio Tour London: The Making of Harry Potter
Warner Bros Studio, Aerodrome Way, Leavesden, Watford, Herts, WD25 7LS
A great day out for every fan of the boy wizard.
The Making of Harry Potter studio tour, covering 150,000 square foot, on two soundstages opened on the 31st March 2012, with stars galore at the red carpet launch at the Leavesden Studios where all eight movies were produced.
The home for many film productions, including several James Bond features, before a relatively new production company arrived there to make a film about a young boy who on his 11th birthday discovers he is a wizard.
Over the next ten years, the cast and crew of over 4,000 in total used more and more of the studios as the popularity of the books and films grew. The three young stars lived, grew up, went to school and turned into adults there on those stages.
Your tour begins in the foyer, with a flying Ford Anglia hanging from the ceiling and the walls adorned with huge photos of the cast, along with a few props.
Passing by the set of the cupboard under the stairs, you enter a room with a number of vertical TV screens showing Potter movie posters from around the world, followed by a short video sequence showing the rise of Harry’s popularity, the production teams discovery of the stories and the enormous worldwide success of the books and films.
Moving into the cinema, a short film introduced by Daniel Radcliffe, Emma Watson and Rupert Grint, talking about their experiences growing up on a film set for ten years, with clips from all eight films. The film ends with them standing in front of the main doors to the Great Hall and they walk in through the doors and invite you to follow them.
The screen at this point slowly rises to reveal the actual main doors to the Great Hall, surrounded with stone statues and carvings. What a wizard way to start the tour.
Walking through into the Great Hall we are told that we were now walking on the actual stone floor used in the films and seeing the actual tables where the actors ate their feasts. Dummies down each side of the hall wear the actual costumes used in the films. At the far end of the hall is the teachers’ table area, with more amazing costumes worn by Professors Dumbledore, Snape, McGonagall, Moody, Trelawney and Flitwick, as well as Hagrid and Filch too.
Leaving the Great Hall you enter the first of two vast sound stages. This includes sets for the Gryffindor Common Room and Dormitory, Dumbledore’s Office, Potions Classroom, Hagrid’s Hut, Burrow’s Kitchen and parts of the Ministry of Magic, also Umbridge’s gaudy pink, feline office. Each filled to the brim with props and costumes.
Props can be seen everywhere, with a massive cage in the centre, chock-a-block with goblets, chandeliers, wands and armour. A huge glass case contains the wands of 24 of the major characters – less than 1 percent of the total number of wands made for the films. The ornate doors to a Gringott’s vault and to the Chamber of Secrets are seen after passing a wall dedicated to the paintings produced to decorate the walls of Hogwarts.
Below the giant swinging pendulum of the Hogwarts castle clock there are several huge touch screens containing an interactive Marauders Map.
There are sections of the soundstage dedicated to various movie-making crafts. The hair and makeup section, costumes section, animal department, graphic design and production.
The final section in this first soundstage is dedicated to the Special Effects department with three huge video screens showing all the tricks and techniques, including greenscreen footage and CGI. Props attached to their motion rigs, include the Gringott’s Vault Cart and Mad-Eye Moody’s Recumbent Broomstick.
In separate room you can have a go on a broomstick or drive the Ford Anglia yourself, using the greenscreen technology.
The Backlot about half way round the tour is an open air section between the two soundstages where refreshments are available, including Butterbeer the popular wizarding beverage.
Also featured on the backlot are the Knight Bus, another Ford Anglia, Hagrid’s motorbike/sidecar, the Riddle family tombstone, a section of the rickety wooden Hogwarts Bridge, Potter’s burnt out cottage from Godric’s Hollow and Number 4 Privet Drive.
Entering the second soundstage you pass some of the giant chess pieces from the first movie. A number of video screens here progressively show what it was like to work in the creature shop, cleverly leading you from one screen to the next, past models of Fawkes, a snapping Monster Book of Monsters and a giant animatronic head of Hagrid. The next room has the life size (i.e., ENORMOUS!) model of Aragog the spider and one of three animatronic Buckbeak models.
Walking around the corner (WOW) you are transported into another world entirely. The dark lighting and cobbled street can only mean one thing – you have entered Diagon Alley. The shops using the original sets have been rebuilt– Flourish & Blotts, Eeylops Owl Emporium, Potage’s Cauldron Shop and of course Ollivander’s Wand Shop, each and every one them is crammed full of detail. At the other end of the street is Weasleys’ Wizard Wheezes, with the bright orange shopfront standing out from the crowd of blackness and featuring a moving model of one of the red-haired twins doffing his hat.
At the end of Diagon Alley you move onto the Art and Design department with walls covered with architectural drawings and detailed plans, accurate down to the millimetre, for many of the props and sets already seen. A draftsman’s table serves as a projection screen for another video about the work of the art department.
Moving on, up the ascending path are walls full of concept paintings and artwork, also intricate cardboard models of Hogsmead and the Hogwarts.
You are only looking at a model of the model though, as entering the next room, there, spread over at least 15 square metres is the most amazing, complex and elaborate model built to a 1:24 scale. It has a bigger footprint than the average house.
The last part of the tour is a fitting tribute to the crew and cast of the most popular film franchise of all time. A much tidier recreation of the interior of Ollivander’s Wand shop, with over 4,000 wand boxes lining its shelves – one for every single person who worked on the films.
Exit through the Gift Shop.