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I was out and about doing deliveries for the local community support group this afternoon. At school run time there was a heavy, squally shower.
What does it take to make a good street photgraphy point and shoot camera? My short list includes:
-Fast auto-focus
-Sharp lens
-Pocketability
-Silent operation
-A waist level viewfinder.
Many P&S cameras fulfill the first four criteria, but only a few come equipped with a truly usable vertical viewfinder that leaves the subjects unaware their picture is taken. Two very common examples are the Yashica T3 and the Canon Sureshot Ace. I plan on testing both in the near future, but until then I thought I'd make a short comparison of specifications and user interface for anyone who might be interested in getting one of them.
Size-wise they are very similar and weigh pretty much the same. The Canon has a pretty streamlined shape that gives it a pleasant look even by today's standards. The Yashica seems quite outdated in that department. The Canon is a bit narrower / flatter, so this makes it marginally more pocketable.
Both cameras are quite ergonomic with a nice grip and easy access to all buttons and controls. The Yashica has a rubber grip cover so it might have the edge there, although the Canon feels very secure too. I really appreciate the fact that both cameras have a retractable lens barrier that serves as a ON-OFF switch too.
The conventional viewfinder of the Yashica has the edge, as it is bigger, brighter and has parallax marks, unlike that of the Canon. On the other hand, the vertical viewfinder is larger (although somehow darker) in the Canon.
What really let me down was the lack of a flash-off option in the Sureshot, which really forces one to use high speed film to avoid the flash firing all the time. The flash can be turned off in the Yashica, although it defaults to ON everytime the shutter fires.
Another plus of the Yashica is that you can get focus confirmation when you're shooting from the hip, as the "AF" sign shows in the LCD screen. This is not possible with the Canon, although you can definitely hear the lens move to focus and this is usually enough, unless the environment is noisy.
Both cameras use the expensive 2CR5 6V lithium battery, so prepare to spend a lot on the battery, either way.
ASA range is 50-1600 for the Canon, The Yashica goes from 64 to 1600. Regarding shutter speeds, the Yashica offers a full 1s-1/630s range, while the Canon is limited to a 1/40-1/125s range (but stops the lens down to f/32 if necessary)
Both cameras are pretty noisy, the Canon shutter being the louder of the two, although in both cameras the film does not advance until you lift your finger off the shutter button, so you can do that after taking the picture in order not to startle the subject.
In the critical field of optics, I am a fan of Canon Sureshots, so far I've had nothing but sharp, contrasty, flare-free pics from my other Canon P&S. However, the Canon lens looks like a certain underdog here, being a 3.5/35 triplet competing with a Zeiss 2.8/35 Tessar lens treated with the famous T* coating. However, only a field test will settle the score and hopefully I'm going to set it up soon enough.
So, the Yashica seems to be a clear winner regarding optics, exposure range and the crucial flash-off option. The larger waist-level viewfinder and the sleeker design of the Canon are not enough to claim victory over the Yashica, or even a draw for that matter. However, before declaring the Yashica the logical choice, consider this: The Canon usually sells for less than 1/20 the price of the Yashica...
The University of Greenwich is a public university located in London and Kent, United Kingdom. Previous names include Woolwich Polytechnic and Thames Polytechnic.
The university's main campus is at the Old Royal Naval College, which along with its Avery Hill campus, is located in the Royal Borough of Greenwich. Greenwich also has a satellite campus in Medway, Kent, as part of a shared campus. The university's range of subjects includes architecture, business, computing, mathematics, education, engineering, humanities, maritime studies, natural sciences, pharmacy and social sciences. Greenwich's alumni include two Nobel laureates: Abiy Ahmed and Charles K. Kao. It received a Silver rating in the UK government's Teaching Excellence Framework.
The university dates back to 1891, when Woolwich Polytechnic, the second-oldest polytechnic in the United Kingdom, opened in Woolwich. It was founded by Frank Didden, supported by and following the principles of Quintin Hogg, and opened to students in October 1891. Like Hogg's pioneering venture in London's Regent Street, it initially combined education with social and religious functions.
In 1894 it focused on an educational role, concentrating on higher technical education appropriate to its location close to Woolwich Dockyard and the Royal Arsenal; William Anderson, director-general of the Ordnance Factories, was a trustee and later a member of the board of governors. Its premises were also used for day schools – the first Woolwich Polytechnic School was established in 1897.
In 1970, Woolwich Polytechnic merged with part of Hammersmith College of Art and Building to form Thames Polytechnic. In the following years, Dartford College (1976), Avery Hill College of Education (1985), Garnett College (1987) and parts of Goldsmiths College and the City of London College (1988) were incorporated.[9]
In 1992, Thames Polytechnic was granted university status by the Major government (together with various other polytechnics) and renamed the University of Greenwich in 1993. On 1 January 1993, the Thames College of Health Care Studies, itself a merger of three local nursing and midwifery training schools, officially merged with the newly designated University of Greenwich, becoming a full faculty of the university.
Formerly a UK government research agency, the Natural Resources Institute (NRI) was incorporated into the university in 1996.
In 2001, the university gave up its historic main campus in the Bathway Quarter in Woolwich, relocating to its current main campus in Greenwich.
Greenwich Campus is located mainly in the Old Royal Naval College, into which it moved in the 1990s when the premises were sold by the Royal Navy.
The campus is home to the Business School and the Faculty of Liberal Arts and Sciences. The campus also includes university's Greenwich Maritime Institute, a specialist maritime management, policy and history teaching and research institute. The Old Royal Naval College also hosts "The Painted Hall", which was painted in the 18th century by Sir James Thornhill, which covers over 40,000 square feet of surface in 200 painting of kings, queens and mythological creatures.
The campus has a large library at Stockwell Street which houses an extensive collection of books and journals, language labs and a 300-PC computing facility. Other facilities include specialist computer laboratories including one at Dreadnought centre, a TV studio and editing suites. The Stephen Lawrence Gallery at the Stockwell Street building, showcases the work of contemporary artists and is linked to the School of Design.
The Avery Hill Campus comprises two sites, Mansion and Southwood. Both are situated in the 86-acre Avery Hill Park in the Royal Borough of Greenwich, south-east London.
The campus is home to the Faculty of Education & Health. Facilities include computer laboratories, a library and a TV studio, as well as a sports and teaching centre with a sports hall and 220-seat lecture theatre. Southwood site also has clinical skills laboratories. These replicate NHS wards, enabling trainee health professionals to gain hands-on experience. The village complex provides student accommodation, a general shop and a launderette. The Dome, in the centre of the complex, houses a food outlet and gym. Rugby, football, indoor pitches, netball and tennis courts, and a dance studio are on Avery Hill campus.
The facility, which was built by Wimpey Construction under a PFI contract, was completed in 1996.
The Winter Garden, the centrepiece of the Mansion site, has fallen into neglect and is on Historic England's 'At Risk' Register. A campaign to restore the Winter Garden is putting pressure on the university and Greenwich Council to ensure its future.
The Medway Campus is located on a former Royal Navy shorebase (called HMS Pembroke) opened in 1903 at Chatham Maritime, Kent.
The Faculty of Engineering and Science is based here, as is the Natural Resources Institute, a centre for research, consultancy and education in natural and human resources. It is also the home of Medway School of Pharmacy, a joint school operated by the Universities of Greenwich and Kent. The Faculty of Education & Health offers a number of its programmes at Medway. Facilities include laboratories, workshops, a computer-aided design studio and a training dispensary.
The Drill Hall Library is a learning resource centre with a library, computers, study areas and teaching rooms. Social facilities include a sports hall, bar, gym and outdoor tennis courts. The university is a member of Universities at Medway, a partnership of educational establishments at Chatham Maritime that is developing the area as a major higher education centre in the Medway region.
Greenwich Campus is near 74-hectare Greenwich Park, home to the Royal Observatory, Greenwich. The Stockwell Street Building opened in 2014 and is now home to the campus library, film and TV studios, and state-of-the-art editing suites. In 2015, it was shortlisted for the Stirling Prize for excellence in architecture.
The Dreadnought Building is a central hub for the Greenwich Campus, with further teaching and social spaces.
The Student Village at Avery Hill Campus provides accommodation for around 1,000 students. On-site facilities include a café, canteen, shop, launderette, bicycle parking, and a gym.
Medway Campus has 350 rooms across five halls of residence dedicated to student accommodation.
Greenwich Students' Union is the university's students' union. In October 2019, the GSU Student Assembly voted to ask the university to declare a climate emergency and for the university and union sustainability strategies to consult with students in creating them. This call to action aimed to speed up the university's efforts at becoming carbon neutral.
At the Medway campus in Kent there is a partnership between the University of Greenwich Students' Union, Canterbury Christ Church and University of Kent Union on the Medway campus. Greenwich Students' Union has been leading the partnership since July 2021 and manages The Hub space, previously The Student Hub when it was looked after by GK Unions – the Greenwich & Kent Students' Unions Together (once the Universities at Medway Students Association, UMSA).
Greenwich Students' Union delivers at Avery Hill, Greenwich and Medway campus.
Greenwich research seeks to influence and enhance health, education, science, engineering, computing and social policy, and attracts international agencies, government departments and global corporations (for example, Pfizer, GlaxoSmithKline, BAE Systems, Airbus, GE Aviation and Merck Consumer Health) from over 50 countries. Significant areas of research and consultancy include landscape architecture, employment relations, fire safety, natural resources, tourism and hospitality, social network analysis, education, training, educational leadership and public services.
Examples of research
The university's Natural Resources Institute has developed an artificial cow that attracts and kills the tsetse fly. This was recognised by a Universities UK survey in 2009 as one of the ten most important discoveries to be made in a UK university over the past 60 years.
The Fire Safety Engineering Group, part of the School of Computing & Mathematical Sciences, is a world leader in computational fire engineering, including expertise in aircraft, building, ship and rail evacuation and fire modelling. It has developed airEXODUS, a leading evacuation model in the aviation industry.
A University of Greenwich research team helped restore the Cutty Sark after it was badly damaged by fire.
Researchers working on 19 sustainable development and agriculture projects in India helped the university to win the 2010 Times Higher Education Award for Outstanding International Strategy.
Two University of Greenwich scientists have developed a technology which converts contaminated land and industrial waste into harmless pebbles, capturing large amounts of carbon dioxide at the same time.
The Greenwich Maritime Institute makes internationally recognised contributions to research in maritime history and economics, such as its exploration of the governance of the River Thames since the 1960s and the effects this has had on the economic development of adjacent communities.
The university has had many famous movie productions that were filmed on campus, one example of a movie is the classic 2013 Marvel movie Thor: Dark World
Rankings
Rankings
National rankings
Complete (2024)110
Guardian (2024)116
Times / Sunday Times (2024)105
Global rankings
ARWU (2023)601–700
QS (2024)671–680
THE (2024)501–600
The university was ranked 94 out of 121 UK institutions according to The Guardian University Guide 2022 league table. For 2023, the University of Greenwich was ranked 60 according to Times Higher education (THE). Moreover, University of Greenwich ranked first in London for Events, Tourism and Hospitality by the Guardian’s 2023 university rankings. Subjects taught at Greenwich have seen rises in the Guardian university league tables for 2022: Chemistry was at 10, up 10 places since 2021. Forensic Science (9), Criminology (10), Mechanical Engineering (12), and Education (48) also moved up significantly.
In Center for World University Rankings World University Rankings 2020–21 – University of Greenwich was ranked 76 in the UK. In 2022, University of Greenwich was ranked in the 750-800 range globally by QS World University Rankings.
In the Times Higher Education (THE) Impact Rankings 2020, Greenwich performed well in several categories:
Responsible Consumption and Production (24th)
Life on Land (66th)
Reduced Inequalities (68th)
Climate Action (75th)
Partnership for the Goals (77th)
Awards
In 2012, the university was rated as the greenest in the UK by People & Planet Green League Table. In 2019, it was ranked 14 in UK, and third in London. The University has gained many national awards, including four Queen's Anniversary Prizes, nine Times Higher Education Awards and two Guardian University Awards.
In 2019, the university's Natural Resources Institute was awarded a Queen's Anniversary Prize for its research in pest management and control to combat human and animal diseases in the UK and internationally; in 2015 it won a prize for work on the cassava crop in Africa.
In 2023, the university has been classified as Gold in Teaching Excellence Framework (TEF) of Higher Education.
Cafeteria workers' dispute
In 2019, the university's main cafeteria was operated by BaxterStorey, which paid its workers £9.25 per hour without contractual sick pay. After a chef had collapsed on his way home from a shift during a typical 80-hour week, all workers joined UVW union. After four strike days in October 2019, and protests disrupting the annual graduation ceremony and a board meeting, Greenwich University announced in early January 2020 that all outsourced cafe workers, cleaners and security guards would receive the London living wage of £10.55, in addition to the same sick pay and annual leave as university staff.
Partnership with Charlton Athletic
In 2018, the University of Greenwich started a partnership with Charlton Athletic F.C.
Notable alumni
Abiy Ahmed is Prime Minister of Ethiopia and a Nobel Peace prize winner
Sir Charles Kao was one of the distinguished alumni at UOG
Demitu Hambisa Bonsa
Prominent alumni of the university and its predecessor organisations include Nobel Laureate Charles Kao, who was awarded the Nobel Prize in Physics in 2009 for his work on transmission of light in fibre optics, and Abiy Ahmed, who won the 2019 Nobel Peace Prize. In June 2021, representatives from multiple countries called for the award of the Nobel Peace Prize to Abiy to be re-considered because of the war crimes committed in Tigray. Two British government ministers, Richard Marsh and Gareth Thomas, are also graduates. A more extensive list is given below.
Abiy Ahmed, Prime Minister of Ethiopia and Nobel Peace prize winner
Jamie 'JME' Adenuga, MC
Bola Agbaje, playwright
Helen Bailey, writer
Natasha Bedingfield, pop singer (did not graduate)
John Behr, theologian
Malorie Blackman, children's author
Demitu Hambisa Bonsa, Ethiopian government minister
John Boyega, actor, best known for Star Wars: The Force Awakens
Sheila Bromberg, musician
Liam Brown, author
Campbell Christie, chairman of Falkirk F.C.
Terry Christian, radio and television presenter
Mark Daly, Irish senator
Siobhan Dowd, writer (A Swift Pure Cry)
Sarah Eberle, garden designer
Jenni Fagan, author
Leo Fortune-West, professional footballer
Sarah Gillespie, singer-songwriter
Pippa Guard, actress
Andrey Guryev (born 1982), Russian entrepreneur
Gareth Hale, comedian
Patrick Harrington, politician in the National Front (1979–1989) and currently Third Way (UK) think tank; general secretary of Solidarity – The Union for British Workers
Rachael Heyhoe-Flint, cricketer
Roy Hodgson, England and Premier League football manager
Dermot Hudson, left-wing political activist
Brian Jacks, 1972 Summer Olympics bronze medallist in Judo
Mark Jackson, musician (VNV Nation)
Charles K. Kao, Nobel Prize winning scientist
Graham Kendrick, Christian worship leader
Sammy Lee, IVF specialist
Pablo Daniel Magee, writer, journalist and playwright
Richard Marsh, Baron Marsh, politician
Rui Moreira, Portuguese politician and businessman; mayor of Porto
Chinenye Ochuba, former Most Beautiful Girl in Nigeria
Sarah Ockwell-Smith, childcare author
Joy Onumajuru, model and philanthropist
Norman Pace, comedian
Ann Packer, 1964 Summer Olympics gold medallist
Lara Pulver, Olivier Award-nominated dancer and actress
Richard Pybus, cricket coach
George Rose, businessman
Dave Rowntree, musician (Blur)
Etienne Schneider, Deputy Prime Minister of Luxembourg
Peter Skinner, MEP
Aramazd Stepanian, playwright
William G. Stewart, TV presenter (Fifteen to One)
Nina Stibbe, author
Adelle Stripe, author
Gareth Thomas, politician
Ewen Whitaker, lunar astronomer (alumnus of Woolwich Polytechnic)
Joel Willans, author and copywriter of works in Finland.
Includes my chapter on the history of Disney animation scores. (Part of the "much, much more.....")
Carl Stalling was Disney's first composer. He left Walt for Warner Bros in the early 1930s.
Mark Mothersbaugh is a founding member of DEVO.
We all know Leonard.
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Major engineering work to renew Stoats Nest Junction (Coulsdon) has led to main London-Gatwick-Brighton line being blocked from Christmas to New Year.
Alternative routes advertised include trains running to Gatwick via Sutton, Dorking and Horsham ; to Brighton via Dorking, Horsham and Littlehampton ; fast trains to East Grinstead for bus connections to Gatwick and Three Bridges ; and buses linking Coulsdon Town (on the Tattenham Corner branch) with Redhill, Gatwick and Three Bridges.
The Coulsdon Town service has provided a use for the crossovers and signals installed to facilitate terminating trains that were installed when Coulsdon North was closed. However, the facility has not been regularly used for many years.
Buses from Coulsdon Town were operated by Go-Ahead London General with a mixture of vehicles, many running non-stop via the M23 motorway to Gatwick or Three Bridges. The stopping services to Redhill I saw were being operated by Metrobus who are of course also a Go-Ahead company.
Plenty of rail and Go-ahead staff were on site to assist passengers with luggage of which there seemed to be a great deal.
It was probably as well that there were no school services required as this meant spare buses and crews were available ; including work for the Tridents with LED destination displays which cannot, of course, operate TfL services.
A bit daft to put that advertising sign in the middle of the pavement. I moved it to the side, before someone fell over it.
Includes Teams from Wagner/Bon Homme, Britton-Hecla, Vermillion, Stanley County and West Central. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.
©2021 SDPB
Charleville Railway Station was established by the Queensland Government in 1888 as part of a rail link to service Western Queensland. Structures of cultural heritage significance at the station include the passenger station, opened in 1957 and the goods shed, the core of which was completed in 1888. These structures reflect the historic importance of Charleville as a western railway station.
In Australia, government fostered the development of railways as a means of developing the country and providing social benefits. It was argued that rail would reduce freight costs and save travel time for passengers. An added incentive for rail development in Queensland was the very poor state of the roads. In wet weather especially, this hampered the transport of freight. Railway development became the province of government because of the doubtful economics of building and operating a rail service for the widely distributed, sparse population of rural Queensland. In most cases the capital costs were high in relation to the potential revenue likely to be raised from passengers and freight. These economies imposed a limit on the expansion of railways into remote areas.
The government initially gave priority to developing a railway west of Brisbane. As well as providing graziers and farmers with a more efficient transport link to the coast, railways were seen as a key to encouraging closer settlement west of the Great Dividing Range. The first section of rail, opened on 31 July 1865, was between Ipswich and Bigg's Camp, 34 kilometres west of Ipswich. By February 1868 the rail was extended to Dalby in the Darling Downs. With a railhead provided for the squatters in this region, extensions further west ceased while the railway was developed elsewhere. It was 1876 before construction of the railway westward from Dalby recommenced. The rail was opened to Roma in 1880, Mitchell in 1885 and Charleville on 1 March 1888. With the opening of the rail to the west, the train became an important transport link for passengers and freight.
There were a number of factors that contributed to Charleville's importance as a rail terminus. Situated on the banks of the Warrego River, a natural stock route from New South Wales to Western Queensland, Charleville was already an important regional centre. Moreover, it was to remain the main western rail terminus for at least a decade. The economies of extending the line further west were doubtful. In any case the depression of the 1890s precluded further railway construction for some years. An extension to the line was opened in 1898. However, it was designed to intercept cross-border trade with New South Wales so it was south southwest from Charleville to Cunnamulla rather than west. A further development west did not begin until 1911 when a line to Quilpie was commenced as part of the ill-fated Great Western Railway scheme. Until the opening of this line in 1917, Charleville remained the most western railhead. Also, Charleville was made a locomotive depot due to its distance from the closest existing facility at Roma.
Charleville's importance meant that the station was provided with more than the usual station facilities. By August 1888, most of the station structures were completed. These included platform, tank, booking and telegraph offices, goods shed, stationmaster's house, and guards, enginemen and firemen's cottages. Engine and carriage sheds were moved from Mitchell to Charleville. Cattle and sheep yards were in place by January 1889 and by 1916, a 50-ton weighbridge had been added to the complex. The weighbridge currently on the site is 40 tons and appears to post-date 1976.
The original wooden station building was destroyed by fire on 6 July 1954 and the engine shed was blown down in a severe windstorm in October 2003. Most of the other 1888 buildings appear to have been either removed or demolished.
The Goods Shed has survived a serious fire and has undergone significant modification. On 4 April 1900, a fire destroyed the entire contents of the Goods Shed, then rented from the Government by N Nielsen. It seems that no substantial modifications were made to the structure as a result of this fire. The shed has been upgraded at least twice since that time. In the 1920s, an extension of some 12 metres by 3.7 metres to the platform at the eastern end was approved. Then in 1962, major white ant damage in the office and deterioration of the timber platform was reported. Repair work was delayed because a complete rearrangement of the yard was under consideration but as this did not proceed, tenders were called for renovations in 1974. Substantial changes were made to the structure including a new goods office, reconstruction of much of the timber platform, a new concrete platform and a new toilet.
Following the destruction of the original passenger station, a new station building was opened in 1957. It was designed by Queensland Railways Department's architectural office under the supervision of Charles Da Costa and erected by K D Morris and Sons, Brisbane. Da Costa had been a specialist in re-inforced concrete design for at least thirty years. He trained as a pupil of T. S. Martin of Sydney from 1905, joining Queensland Railways in 1907 as a Junior Draftsman. After retrenchment in 1921, he began private practise as an architect and structural designer in Brisbane. Later he worked for Burns Philp and Company and then, in 1935 rejoined Queensland Railways as an Architect. He became Principal Architect in 1938 and retired in 1955. Charleville Railway Station may have been one of his last designs before retiring.
The building was more substantial than its predecessor. It was built in an era of economic prosperity augmented by a wool industry that was booming in the mid-1950s and in an environment of Government investment in post-war rehabilitation of rail infrastructure. However, at the opening ceremony, the Honourable T Moore indicated that the new building also reflected the continued importance of Charleville as a western railhead:
'Mindful of the important contribution made by the Charleville district to the earnings of the Railway Department (the revenue from outward and inward traffic for the last financial year totalled £ 246, 856 and £ 186, 369 respectively) and the wealth of the State generally, the Government decided that the wooden station building which was destroyed by fire in 1954 should be replaced by a modern structure, worthy of this prosperous and progressive town and district, one which would meet, for many years to come, the increasing needs of the Department's customers and a building which would provide the maximum of comfort for travellers to and from the West...'
Charleville was the third busiest goods station on the Western Line after Quilpie and Cunnamulla and the busiest passenger station at the time, earning £26 810 in revenue from passengers in 1954/55 ahead of Roma (£17 346) and Dalby (£10 816).
The station, as designed in 1954, was a large building almost 92 metres long and 12.5 metres wide with a 162.7 metres long concrete platform shaded with cantilever awnings extending well beyond the northeastern end of the building. A 46 metre long loading dock was built at the north end of the building with access to King Street. The entrance opened to a spacious terrazzo tiled vestibule located in the centre of the building. Some 26 other rooms made up the building including Tranship Room, Cloak and Luggage Room, Parcels Office, Station Master and Assistant Station Master's Offices, Clerks' Office, Telegraph Room, Ticket Office, Ladies Waiting Room, Refreshment Rooms, Store Rooms, Guards and Porters' Rooms, Mail Room and Lavatories.
The design of the building, according to Moore, was influenced by the local climate. The reinforced concrete walls were designed to insulate the interior against extremes of temperature. The building was provided with projecting eaves to provide shade and large windows to capture breezes.
The furniture in the building, a quantity of which is still extant, was manufactured partly by contractors and partly by the railway's Northgate workshops.
Charleville is the only station of its design on the Queensland Rail network. Hughenden also has a large concrete station. However, it was built some ten years earlier than Charleville, is less than half the size and is made of pre-cast concrete beams not reinforced concrete.
With the greater use of other modes of transport such as road and air coupled with a decline in rural population, passenger numbers on the Western Line have declined sharply since the 1950s. Passenger traffic through Charleville is now much less than it was when the station was built in 1957.
Source: Queensland Heritage Register.
Includes 1918A2 BAR, Cartridge Belt with full complement of magazines (1942), Jungle First Aid pouch (1944) with contents, Carlisle bandage (1945), Canteen, Cup, & cover (1943), M3 Trench Knife, Leather tool box, Combo Tool, Oil Can, Reamer, Brushes, Compass, BAR Field Manual (1944).
The ammo belt was the very first piece of my entire collection and was purchased for less than $10 when I was a kid. It is in excellent condition, and similar belts go for over $125 today!
Weighing in at around 20 pounds, this must have been a beast to carry all day long. Many "experts" have three major complaints about the Browning Automatic Rifle. 1)The Weight 2)The 20-round magazine capacity 3)The relatively complicated internal parts. However, most combat veterans seem to admire its firepower and felt a sense of comfort when they heard their squad's Automatic rifle chugging away at the enemy. A typical Army squad would have one BAR while a Marine Corps squad would have two. The Army BAR fired in a fast or slow automatic mode wile the Marine Corps BAR fired auto or semi-auto, like the original design. A lot of soldiers would remove the Bi-pod, and carry handle to lighten their load.
I am trying to imagine what my dad carried in combat. He was a BAR gunner and told me he had a jungle first aid kit and LOVED his M3 trench knife. He also described what must have been a "jungle" pack and a poncho.
Celebrating its 30th anniversary and back after a 2 year break due to pandemic, the Brighton Pride parade was as colourful and lively as ever.
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
Bugatti Type 40 (1926-30) Engine 1496cc S4 SOHC Production 830 (includes Type 40A)
Entrant Julia de Baldanza
Registration Number DS 7138
BUGATTI SET
www.flickr.com/photos/45676495@N05/sets/72157623635625235...
The Bugatti type 40 Fiacre, otherwise known as the Type 40, was Introduced in 1926, as a Grand Sport tourer, featured an open-top bodywork with a narrow engine compartment with aerodynamic design, with a twin plug 1496c engine of 45bhp and with the Type 40A in 1930 with a larger 1627cc 50bhp engine. Small in stature it offered a four seat interior with bench a bench for two passenger in the back.
The Type 40 was a replacement for the former voiturette Brescia Bugatti and continued production until 1940, with a total of 780 units built.
Diolch am 95,970,498 o olygfeydd anhygoel, mae pob un yn cael ei werthfawrogi'n fawr.
Thanks for 95,970,498 amazing views, every one is greatly appreciated.
Shot 07.08.2022, at the VSCC Prescott Speed Hill Climb, Prescott, Gloucestershire REF 162-188
Lotus Elan 26R (1964-circa 68) Engine 1558 cc S4 DOC(includes S1, S2 and S3 Elans)
Race Number 86 Jeremy Cocke
LOTUS SET
www.flickr.com/photos/45676495@N05/sets/72157623671671113...
The original Elan was introduced in 1962 as a roadster, although an optional hardtop was offered in 1963 and a coupé version in 1965. The two-seat Lotus Elan replaced the Lotus Elite. It was the first Lotus road car to use a steel backbone chassis with a fibreglass body. At 1,600 lb the Elan was both lightweight and had highly responsive handling. Initial versions of the Elan were also available as a kit to be assembled by the customer. The Elan was technologically advanced with a DOHC 1557 cc engine, 4-wheel disc brakes, rack and pinion steering, and 4-wheel independent suspension.
The Elan was the first Lotus not be specifically designed for racing, however customers were still prepared to race Elans in Club events. Lotus reply was to creare the Elan 26R as a racing version of the Elan. Mechanically, the 26R differed from the standard car by featuring lightweight competition-spec wishbones, sliding spline driveshafts in place of rubber joints, bigger anti-roll bars and a degree of reinforcement around the suspension pick-up points. Pedals were repositioned to aid heel-and-toeing, dual circuit brakes with twin master cylinders and light alloy calipers coming as standard. As did a 140bhp Cosworth-tuned ‘four’ although up to 160bhp was offered in time, other changes included flared wheel arches, which allowed for larger wheels and tires.
Series 1 introduced in 1962 with pop up head lights, built on a backbone frame, all independant springing and discs all round. The early ones had a 1498 cc engine, changed to the 1558 after the first batch.
The Series 2 (1964-66) was the same basic spec. and appearance, with enlarged brake calipers, polished veneer fascia, and centre locking wheels. All were fixed heads until June 1966.
The Series 3 has a higher final drive ratio and optional close ratio gearbox. The Special Equipment model has an uprated 115 bhp
An Elan was famously used by Emma Peel, the leather clad heroine on the Avengers TV Series.
This car raced at Donington in the Masters Gentlemen Drivers Pre-66 GT Race
Many thanks for a fantabulous 35,559,400 views
3hot at The AMOC Meeting, Oulton Park, Cheshire 16:05:2015 Ref 106-121
It's amazing how far north of west the sun sets as we approach the the longest days of the year. Tonight's sunset from Truleigh Hill. The Sun dropped out of thick cloud in to a clear patch for about 20 minutes before disappearing over the horizon. No editing - straight out of the camera (SOOC)
Swartaasvoel
(Torgos tracheliotus)
The lappet-faced vulture or Nubian vulture (Torgos tracheliotos) is an Old World vulture belonging to the bird order Accipitriformes, which also includes eagles, kites, buzzards and hawks. It is the only member of the genus Torgos. It is not closely related to the superficially similar New World vultures, and does not share the good sense of smell of some members of that group.
The lappet-faced vulture was formerly considered monotypical, but now is separated into two subspecies. The nominate race lives throughout Africa. The subspecies T. t. negevensis, differing considerably in appearance from African vultures (as described below), occurs in the Sinai, the Negev desert, and probably north-west Saudi Arabia.
This species is patchily distributed through much of Africa, though it is absent from much of the central and western parts of the continent and declining elsewhere in its range. The lappet-faced vulture nests in Senegal, Mali, Burkina Faso, Niger, Chad, Sudan, southeastern Egypt, Ethiopia, Somalia, Kenya, Tanzania, Uganda, Rwanda, easternmost part of the Democratic Republic of the Congo, Zambia, Malawi, Mozambique, Swaziland, northeastern South Africa, Zimbabwe, Botswana, Namibia, the Gambia, Guinea, Ivory Coast, Benin, the Central African Republic, southern Angola and possibly in Mauritania and Nigeria. Across the Red Sea, the species nests in Arabia, Yemen, Oman and the United Arab Emirates.
This vulture prefers to live in dry savannah, thornbush, arid plains, deserts with scattered trees in wadis, open mountain slopes. They are usually found in undisturbed open country with a scattering of trees and apparently prefer areas with minimal grass cover. While foraging, they can wander into denser habitats and even into human habitated areas, especially if drawn to road kills. They may be found in elevation from sea-level to 4,500 m (14,800 ft).
The lappet-faced vulture is a huge species, ranking as the longest and largest winged vulture in its range behind the closely related cinereous vulture, although some co-occurring Gyps vultures tend to be heavier on average, especially the Cape vulture and Eurasian griffon. This species measures around 95–115 cm (37–45 in) in body length, with a wingspan of 2.5–2.9 m (8.2–9.5 ft). Among the standard measurements, the wing chord is 71.5–82.5 cm (28.1–32.5 in), the tail is 33–36 cm (13–14 in) and the tarsus is 12.2–15 cm (4.8–5.9 in). The bill, at up to 10 cm (3.9 in) long and 5 cm (2.0 in) deep, ranks as one of the largest of any accipitrid, although a reported culmen length of 7.2 cm (2.8 in) is slightly less than the culmen length of the cinereous vulture. Wild vultures, of the subspecies T. t. tracheliotus, range from 4.4 to 9.4 kg (9.7 to 20.7 lb) and, in East Africa, average only 6.2 kg (14 lb). On the other hand, captive vultures of the larger T. t. negevensis subspecies, weighed 6.5–9.2 kg (14–20 lb) in males and 10.5–13.6 kg (23–30 lb) in females.
Overall, the lappet-faced vulture is blackish above with a strongly contrasting white thigh feathers. The black feathers on the back of African vultures are lined with brown, while Arabian birds are dark brown rather than black above. The underside can range from pure white to buff-brown. Like many vultures, it has a bald head. The head coloration can range from reddish in southern Africa to dull pink in more northern Africa to pink on the back of the head and gray on the front in the Arabian Peninsula. The combination of the colorful head and fleshy folds on the side of it are distinctive. The bald head of the lappet-faced vulture is advantageous, because a feathered head would become spattered with blood and other fluids, and thus be difficult to keep clean. While flying, lappet-faced vultures have large, broad wings held with the front edges held parallel and slightly pointed, serrated-looking wingtips. Compared to the somewhat similarly marked hooded vulture, it is considerably larger with a more massive bill and can only be confused at a great distance. The Gyps vultures are generally much paler, with less white lining the wings and more bulging secondaries. The cinereous vulture (which may overlap in range in the Arabian area) has a similar body shape but is all dark, with no contrasting plumage.
The lappet-faced vulture is a scavenging bird, feeding mostly from animal carcasses, which it finds by sight or by watching other vultures. More so than many other African vultures, they often find carrion on their own and start tearing through the skin. They are the most powerful and aggressive of the African vultures, and other vultures will usually cede a carcass to the lappet-faced vulture if it decides to assert itself. This is often beneficial to the less powerful vultures because the Lappet-face can tear through the tough hides and knotty muscles of large mammals that the others cannot penetrate, although hyenas are even more efficient in this regard (if more voracious eaters). However, lappet-faced vultures frequently hang around the edges of the throngs at large carcasses, waiting until the other vultures are done, to feed on remnant skin, tendons and other coarse tissues that the others will not eat. Big game animals, up to the size of elephants, are preferred as carrion, since they provide the most subsistence at a sitting. A full crop can contain up to 1.5 kg (3.3 lb) of meat.
Perhaps more than any other true vulture, lappet-faced vultures have been recorded as regularly feeding on freshly killed smaller mammals, birds and reptiles. Some of these are probably road-kills or are pirated from eagles or other raptors but they are also believed to occasionally attack live animals, especially young and weak animals and the nests and young of other birds. Flamingo colonies (including eggs, young and adults), young impalas and guineafowl have reportedly been predated. They are believed to still-hunt from an elevated perch and then drop on their prey, stunning them with the impact and tearing them apart with their strong bills. Most remains found at nests are from small animals possibly caught alive.
Lappet-faced vultures are generally solitary birds. They do not nest in cohesive colonies as do many smaller vultures, with one tree or area usually only having 1 to 2 nests in it, though rarely up to 10 nests have been recorded in one area. The home range of a lappet-faced vulture is usually at least 8 to 15 km (5.0 to 9.3 mi). Groups of up to 25 to 50 Lappet-faces may congregate at large carcasses or watering holes, though typically only from 1 to as many as 7 turn up per carcass.
This species nests in November through July in the north of its range, throughout the year in eastern Africa and May to January in southern Africa. The huge nest, a pile of neatly formed sticks, measures 120–220 cm (47–87 in) across and 30–70 cm (12–28 in) deep. The nest is often lined with green leaves, as well as animal hair and skins. Nests are almost always placed in the main fork or top of an Acacia tree, though Balanites and Terminalia trees are sometimes also used, at 5 to 15 m (16 to 49 ft) off the ground. The clutch contains 1 or 2 eggs, which are incubated by both parents over the course of 54 to 56 days. The young fledge at 124 to 135 days old, although can be dependent on their parents for up to an age of 1 year or more, sometimes forcing parents to only nest in alternate years. There is a single remarkable record of a lappet-faced vulture pair successfully raising a white-headed vulture. The lappet-faced vultures does not usually breed until it is around 6 years of age.
The lappet-faced vulture's world population is believed to have decreased perceptibly (As for October 2015 their IUCN status was updated to Endangered). They are declining in Sahel and several parts of their southern, northern and western distribution in Africa. They are apparently currently stable in Arabia but have a small population there and have been extirpated from Israel as a breeding bird. The declines are almost entirely due to human activities, including disturbances from habitat destruction and cultivation, disturbances at the nesting site (to which the species is reportedly quite sensitive) and ingestion of pesticides, which are usually set out for jackals and other small mammalian carnivores. Domestic cattle, who have replaced natural prey over much of the range, are now often sold off, rather than abandoned, due to the proliferation of markets and abattoirs and rarely left to die and be consumed by vultures. Lappet-faced vultures are also sometimes victims of direct persecution, including shooting and the use of strychnine and other poisons. In Namibia, 86 lappet-faced vultures died after eating poisoned cattle carcasses, because the farmers erroneously believed they were killing and eating the cattle. In some cases the poisoning is done by poachers, who fear the presence of vultures will alert authorities to their activities, the illegal killings of protected species. They are considered Vulnerable at the species level, with an estimated world population of under 9,000 individuals.
Wikipedia
Cheddar is a large village and civil parish in the English county of Somerset. It is situated on the southern edge of the Mendip Hills, 9 miles (14 km) north-west of Wells, 11 miles (18 km) south-east of Weston-super-Mare and 18 miles (29 km) south-west of Bristol. The civil parish includes the hamlets of Nyland and Bradley Cross. The parish had a population of 5,755 in 2011 and an acreage of 8,592 acres (3,477 ha) as of 1961.
Cheddar Gorge, on the northern edge of the village, is the largest gorge in the United Kingdom and includes several show caves, including Gough's Cave. The gorge has been a centre of human settlement since Neolithic times, including a Saxon palace. It has a temperate climate and provides a unique geological and biological environment that has been recognised by the designation of several Sites of Special Scientific Interest. It is also the site of several limestone quarries. The village gave its name to Cheddar cheese and has been a centre for strawberry growing. The crop was formerly transported on the Cheddar Valley rail line, which closed in the late 1960s and is now a cycle path. The village is now a major tourist destination with several cultural and community facilities, including the Cheddar Show Caves Museum.
The village supports a variety of community groups including religious, sporting and cultural organisations. Several of these are based on the site of the Kings of Wessex Academy, which is the largest educational establishment.
The name Cheddar comes from the Old English word ceodor, meaning deep dark cavity or pouch.
There is evidence of occupation from the Neolithic period in Cheddar. Britain's oldest complete human skeleton, Cheddar Man, estimated to be 9,000 years old, was found in Cheddar Gorge in 1903. Older remains from the Upper Late Palaeolithic era (12,000–13,000 years ago) have been found. There is some evidence of a Bronze Age field system at the Batts Combe quarry site. There is also evidence of Bronze Age barrows at the mound in the Longwood valley, which if man-made it is likely to be a field system. The remains of a Roman villa have been excavated in the grounds of the current vicarage.
The village of Cheddar had been important during the Roman and Saxon eras. There was a royal palace at Cheddar during the Saxon period, which was used on three occasions in the 10th century to host the Witenagemot. The ruins of the palace were excavated in the 1960s. They are located on the grounds of the Kings of Wessex Academy, together with a 14th-century chapel dedicated to St. Columbanus. Roman remains have also been uncovered at the site. Cheddar was listed in the Domesday Book of 1086 as Ceder, meaning "Shear Water", from the Old English scear and Old Welsh dŵr. An alternative spelling in earlier documents, common through the 1850s is Chedder.
As early as 1130 AD, the Cheddar Gorge was recognised as one of the "Four wonders of England". Historically, Cheddar's source of wealth was farming and cheese making for which it was famous as early as 1170 AD. The parish was part of the Winterstoke Hundred.
The manor of Cheddar was deforested in 1337 and Bishop Ralph was granted a licence by the King to create a hunting forest.
As early as 1527 there are records of watermills on the river. In the 17th and 18th centuries, there were several watermills which ground corn and made paper, with 13 mills on the Yeo at the peak, declining to seven by 1791 and just three by 1915. In the Victorian era it also became a centre for the production of clothing. The last mill, used as a shirt factory, closed in the early 1950s.
William Wilberforce saw the poor conditions of the locals when he visited Cheddar in 1789. He inspired Hannah More in her work to improve the conditions of the Mendip miners and agricultural workers. In 1801, 4,400 acres (18 km2) of common land were enclosed under the Inclosure Acts.
Tourism of the Cheddar gorge and caves began with the opening of the Cheddar Valley Railway in 1869.
Cheddar, its surrounding villages and specifically the gorge has been subject to flooding. In the Chew Stoke flood of 1968 the flow of water washed large boulders down the gorge, washed away cars, and damaged the cafe and the entrance to Gough's Cave.
Cheddar is recognised as a village. The adjacent settlement of Axbridge, although only about a third the population of Cheddar, is a town. This apparently illogical situation is explained by the relative importance of the two places in historic times. While Axbridge grew in importance as a centre for cloth manufacturing in the Tudor period and gained a charter from King John, Cheddar remained a more dispersed mining and dairy-farming village. Its population grew with the arrival of the railways in the Victorian era and the advent of tourism.
The parish council, which has 15 members who are elected for four years, is responsible for local issues, including setting an annual precept (local rate) to cover the council's operating costs and producing annual accounts for public scrutiny. The parish council evaluates local planning applications and works with the police, district council officers, and neighbourhood watch groups on matters of crime, security, and traffic. The parish council's role also includes initiating projects for the maintenance and repair of parish facilities, as well as consulting with the district council on the maintenance, repair, and improvement of highways, drainage, footpaths, public transport, and street cleaning. Conservation matters (including trees and listed buildings) and environmental issues are also the responsibility of the council.
The village is in the 'Cheddar and Shipham' electoral ward. After including Shipham the total population of the ward taken at the 2011 census is 6,842.
For local government purposes, since 1 April 2023, the village comes under the unitary authority of Somerset Council. Prior to this, it was part of the non-metropolitan district of Sedgemoor, which was formed on 1 April 1974 under the Local Government Act 1972, having previously been part of Axbridge Rural District. Fire, police and ambulance services are provided jointly with other authorities through the Devon and Somerset Fire and Rescue Service, Avon and Somerset Constabulary and the South Western Ambulance Service.
It is also part of the Wells county constituency represented in the House of Commons of the Parliament of the United Kingdom. It elects one Member of Parliament (MP) by the first past the post system of election. Prior to Brexit in 2020, it was part of the South West England constituency of the European Parliament.
Cheddar is twinned with Felsberg, Germany and Vernouillet, France, and it has an active programme of exchange visits. Initially, Cheddar twinned with Felsberg in 1984. In 2000, Cheddar twinned with Vernouillet, which had also been twinned with Felsberg. Cheddar also has a friendship link with Ocho Rios in Saint Ann Parish, Jamaica.
It is also twinned with the commune of Descartes in the Indre-et-Loire department.
The area is underlain by Black Rock slate, Burrington Oolite and Clifton Down Limestone of the Carboniferous Limestone Series, which contain ooliths and fossil debris on top of Old Red Sandstone, and by Dolomitic Conglomerate of the Keuper. Evidence for Variscan orogeny is seen in the sheared rock and cleaved shales. In many places weathering of these strata has resulted in the formation of immature calcareous soils.
Cheddar Gorge, which is located on the edge of the village, is the largest gorge in the United Kingdom. The gorge is the site of the Cheddar Caves, where Cheddar Man was found in 1903. Older remains from the Upper Late Palaeolithic era (12,000–13,000 years ago) have been found. The caves, produced by the activity of an underground river, contain stalactites and stalagmites. Gough's Cave, which was discovered in 1903, leads around 400 m (437 yd) into the rock-face, and contains a variety of large rock chambers and formations. Cox's Cave, discovered in 1837, is smaller but contains many intricate formations. A further cave houses a children's entertainment walk known as the "Crystal Quest".
Cheddar Gorge, including Cox's Cave, Gough's Cave and other attractions, has become a tourist destination, attracting about 500,000 visitors per year. In a 2005 poll of Radio Times readers, following its appearance on the 2005 television programme Seven Natural Wonders, Cheddar Gorge was named as the second greatest natural wonder in Britain, surpassed only by the Dan yr Ogof caves.
There are several large and unique Sites of Special Scientific Interest (SSSI) around the village.
Cheddar Reservoir is a near-circular artificial reservoir operated by Bristol Water. Dating from the 1930s, it has a capacity of 135 million gallons (614,000 cubic metres). The reservoir is supplied with water taken from the Cheddar Yeo, which rises in Gough's Cave in Cheddar Gorge and is a tributary of the River Axe. The inlet grate for the 54-inch (1.4 m) water pipe that is used to transport the water can be seen next to the sensory garden in Cheddar Gorge. It has been designated as a Site of Special Scientific Interest (SSSI) due to its wintering waterfowl populations.
Cheddar Wood and the smaller Macall's Wood form a biological Site of Special Scientific Interest from what remains of the wood of the Bishops of Bath and Wells in the 13th century and of King Edmund the Magnificent's wood in the 10th. During the 19th century, its lower fringes were grubbed out to make strawberry fields. Most of these have been allowed to revert to woodland. The wood was coppiced until 1917. This site compromises a wide range of habitats which include ancient and secondary semi-natural broadleaved woodland, unimproved neutral grassland, and a complex mosaic of calcareous grassland and acidic dry dwarf-shrub heath. Cheddar Wood is one of only a few English stations for starved wood-sedge (Carex depauperata). Purple gromwell (Lithospermum purpurocaeruleum), a nationally rare plant, also grows in the wood. Butterflies include silver-washed fritillary (Argynnis paphia), dark green fritillary (Argynnis aglaja), pearl-bordered fritillary (Boloria euphrosyne), holly blue (Celastrina argiolus) and brown argus (Aricia agestis). The slug Arion fasciatus, which has a restricted distribution in the south of England, and the soldier beetle Cantharis fusca also occur.
By far the largest of the SSSIs is called Cheddar Complex and covers 441.3 hectares (1,090.5 acres) of the gorge, caves and the surrounding area. It is important because of both biological and geological features. It includes four SSSIs, formerly known as Cheddar Gorge SSSI, August Hole/Longwood Swallet SSSI, GB Cavern Charterhouse SSSI and Charterhouse on-Mendip SSSI. It is partly owned by the National Trust who acquired it in 1910 and partly managed by the Somerset Wildlife Trust.
Close to the village and gorge are Batts Combe quarry and Callow Rock quarry, two of the active Quarries of the Mendip Hills where limestone is still extracted. Operating since the early 20th century, Batts Combe is owned and operated by Hanson Aggregates. The output in 2005 was around 4,000 tonnes of limestone per day, one third of which was supplied to an on-site lime kiln, which closed in 2009; the remainder was sold as coated or dusted aggregates. The limestone at this site is close to 99 percent carbonate of calcium and magnesium (dolomite).
The Chelmscombe Quarry finished its work as a limestone quarry in the 1950s and was then used by the Central Electricity Generating Board as a tower testing station. During the 1970s and 1980s it was also used to test the ability of containers of radioactive material to withstand impacts and other accidents.
Along with the rest of South West England, Cheddar has a temperate climate which is generally wetter and milder than the rest of the country. The annual mean temperature is approximately 10 °C (50.0 °F). Seasonal temperature variation is less extreme than most of the United Kingdom because of the adjacent sea, which moderates temperature. The summer months of July and August are the warmest with mean daily maxima of approximately 21 °C (69.8 °F). In winter mean minimum temperatures of 1 °C (33.8 °F) or 2 °C (35.6 °F) are common. In the summer the Azores high-pressure system affects the south-west of England. Convective cloud sometimes forms inland, reducing the number of hours of sunshine; annual sunshine rates are slightly less than the regional average of 1,600 hours. Most of the rainfall in the south-west is caused by Atlantic depressions or by convection. Most of the rainfall in autumn and winter is caused by the Atlantic depressions, which are most active during those seasons. In summer, a large proportion of the rainfall is caused by sun heating the ground leading to convection and to showers and thunderstorms. Average rainfall is around 700 mm (28 in). About 8–15 days of snowfall per year is typical. November to March have the highest mean wind speeds, and June to August have the lightest winds. The predominant wind direction is from the south-west.
The parish has a population in 2011 of 5,093, with a mean age of 43 years. Residents lived in 2,209 households. The vast majority of households (2,183) gave their ethnic status at the 2001 census as white.
The village gave its name to Cheddar cheese, which is the most popular type of cheese in the United Kingdom. The cheese is now made and consumed worldwide, and only one producer remains in the village.
Since the 1880s, Cheddar's other main produce has been the strawberry, which is grown on the south-facing lower slopes of the Mendip hills. As a consequence of its use for transporting strawberries to market, the since-closed Cheddar Valley line became known as The Strawberry Line after it opened in 1869. The line ran from Yatton to Wells. When the rest of the line was closed and all passenger services ceased, the section of the line between Cheddar and Yatton remained open for goods traffic. It provided a fast link with the main markets for the strawberries in Birmingham and London, but finally closed in 1964, becoming part of the Cheddar Valley Railway Nature Reserve.
Cheddar Ales is a small brewery based in the village, producing beer for local public houses.
Tourism is a significant source of employment. Around 15 percent of employment in Sedgemoor is provided by tourism, but within Cheddar it is estimated to employ as many as 1,000 people. The village also has a youth hostel, and a number of camping and caravan sites.
Cheddar has a number of active service clubs including Cheddar Vale Lions Club, Mendip Rotary and Mendip Inner Wheel Club. The clubs raise money for projects in the local community and hold annual events such as a fireworks display, duck races in the Gorge, a dragon boat race on the reservoir and concerts on the grounds of the nearby St Michael's Cheshire Home.
Several notable people have been born or lived in Cheddar. Musician Jack Bessant, the bass guitarist with the band Reef grew up on his parents' strawberry farm, and Matt Goss and Luke Goss, former members of Bros, lived in Cheddar for nine months as children. Trina Gulliver, ten-time World Professional Darts Champion, previously lived in Cheddar until 2017. The comedian Richard Herring grew up in Cheddar. His 2008 Edinburgh Festival Fringe show, The Headmaster's Son is based on his time at The Kings of Wessex School, where his father Keith was the headmaster. The final performance of this show was held at the school in November 2009. He also visited the school in March 2010 to perform his show Hitler Moustache. In May 2013, a community radio station called Pulse was launched.
The market cross in Bath Street dates from the 15th century, with the shelter having been rebuilt in 1834. It has a central octagonal pier, a socket raised on four steps, a hexagonal shelter with six arched four-centred openings, shallow two-stage buttresses at each angle, and an embattled parapet. The shaft is crowned by an abacus with figures in niches, probably from the late 19th century, although the cross is now missing. It was rebuilt by Thomas, Marquess of Bath. It is a scheduled monument (Somerset County No 21) and Grade II* listed building.
In January 2000, the cross was seriously damaged in a traffic accident. By 2002, the cross had been rebuilt and the area around it was redesigned to protect and enhance its appearance. The cross was badly damaged again in March 2012, when a taxi crashed into it late at night demolishing two sides. Repair work, which included the addition of wooden-clad steel posts to protect against future crashes, was completed in November 2012 at a cost of £60,000.
Hannah More, a philanthropist and educator, founded a school in the village in the late 18th century for the children of miners. Her first school was located in a 17th-century house. Now named "Hannah More's Cottage", the Grade II-listed building is used by the local community as a meeting place.
The village is situated on the A371 road which runs from Wincanton, to Weston-super-Mare. It is approximately 5 miles (8.0 km) from the route of the M5 motorway with around a 10 miles (16 km) drive to junction 22.
It was on the Cheddar Valley line, a railway line that was opened in 1869 and closed in 1963. It became known as The Strawberry Line because of the large volume of locally-grown strawberries that it carried. It ran from Yatton railway station through Cheddar to Wells (Tucker Street) railway station and joined the East Somerset Railway to make a through route via Shepton Mallet (High Street) railway station to Witham. Sections of the now-disused railway have been opened as the Strawberry Line Trail, which currently runs from Yatton to Cheddar. The Cheddar Valley line survived until the "Beeching Axe". Towards the end of its life there were so few passengers that diesel railcars were sometimes used. The Cheddar branch closed to passengers on 9 September 1963 and to goods in 1964. The line closed in the 1960s, when it became part of the Cheddar Valley Railway Nature Reserve, and part of the National Cycle Network route 26. The cycle route also intersects with the West Mendip Way and various other footpaths.
The principal bus route is hourly service 126 between Weston-super-Mare and Wells operated by First West of England. Other bus routes include the service 668 from Shipham to Street which runs every couple of hours operated by Libra Travel, as well as the college bus service 66 which runs from Axbridge to the Bridgwater Campus of Bridgwater and Taunton College in the mornings and evenings of college term times and is operated by Bakers Dolphin.
The first school in Cheddar was set up by Hannah More during the 18th Century, however now Cheddar has three schools belonging to the Cheddar Valley Group of Schools, twelve schools that provide Cheddar Valley's three-tier education system. Cheddar First School has ten classes for children between 4 and 9 years. Fairlands Middle School, a middle school categorised as a middle-deemed-secondary school, has 510 pupils between 9 and 13. Fairlands takes children moving up from Cheddar First School as well as other first schools in the Cheddar Valley. The Kings of Wessex Academy, a coeducational comprehensive school, has been rated as "good" by Ofsted. It has 1,176 students aged 13 to 18, including 333 in the sixth form. Kings is a faith school linked to the Church of England. It was awarded the specialist status of Technology College in 2001, enabling it to develop its Information Technology (IT) facilities and improve courses in science, mathematics and design technology. In 2007 it became a foundation school, giving it more control over its own finances. The academy owns and runs a sports centre and swimming pool, Kings Fitness & Leisure, with facilities that are used by students as well as residents. It has since November 2016 been a part of the Wessex Learning Trust which incorporates eight academies from the surrounding area.
The Church of St Andrew dates from the 14th century. It was restored in 1873 by William Butterfield. It is a Grade I listed building and contains some 15th-century stained glass and an altar table of 1631. The chest tomb in the chancel is believed to contain the remains of Sir Thomas Cheddar and is dated 1442. The tower, which rises to 100 feet (30 m), contains a bell dating from 1759 made by Thomas Bilbie of the Bilbie family. The graveyard contains the grave of the hymn writer William Chatterton Dix.
There are also churches for Roman Catholic, Methodist and other denominations, including Cheddar Valley Community Church, who not only meet at the Kings of Wessex School on Sunday, but also have their own site on Tweentown for meeting during the week. The Baptist chapel was built in 1831.
Kings Fitness & Leisure, situated on the grounds of the Kings of Wessex School, provides a venue for various sports and includes a 20-metre swimming pool, racket sport courts, a sports hall, dance studios and a gym. A youth sports festival was held on Sharpham Road Playing Fields in 2009. In 2010 a skatepark was built in the village, funded by the Cheddar Local Action Team.
Cheddar A.F.C., founded in 1892 and nicknamed "The Cheesemen",[111] play in the Western Football League Division One. In 2009 plans were revealed to move the club from its present home at Bowdens Park on Draycott Road to a new larger site.
Cheddar Cricket Club was formed in the late 19th century and moved to Sharpham Road Playing Fields in 1964. They now play in the West of England Premier League Somerset Division. Cheddar Rugby Club, who own part of the Sharpham playing fields, was formed in 1836. The club organises an annual Cheddar Rugby Tournament. Cheddar Lawn Tennis Club, was formed in 1924, and play in the North Somerset League and also has social tennis and coaching. Cheddar Running Club organised an annual half marathon until 2009.
The village is both on the route of the West Mendip Way and Samaritans Way South West.
Somerset is a ceremonial county in South West England. It is bordered by the Bristol Channel, Gloucestershire, and Bristol to the north, Wiltshire to the east and the north-east, Dorset to the south-east, and Devon to the south-west. The largest settlement is the city of Bath, and the county town is Taunton.
Somerset is a predominantly rural county, especially to the south and west, with an area of 4,171 km2 (1,610 sq mi) and a population of 965,424. After Bath (101,557), the largest settlements are Weston-super-Mare (82,418), Taunton (60,479), and Yeovil (49,698). Wells (12,000) is a city, the second-smallest by population in England. For local government purposes the county comprises three unitary authority areas: Bath and North East Somerset, North Somerset, and Somerset.
The centre of Somerset is dominated by the Levels, a coastal plain and wetland, and the north-east and west of the county are hilly. The north-east contains part of the Cotswolds AONB, all of the Mendip Hills AONB, and a small part of Cranborne Chase and West Wiltshire Downs AONB; the west contains the Quantock Hills AONB, a majority of Exmoor National Park, and part of the Blackdown Hills AONB. The main rivers in the county are the Avon, which flows through Bath and then Bristol, and the Axe, Brue, and Parrett, which drain the Levels.
There is evidence of Paleolithic human occupation in Somerset, and the area was subsequently settled by the Celts, Romans and Anglo-Saxons. The county played a significant part in Alfred the Great's rise to power, and later the English Civil War and the Monmouth Rebellion. In the later medieval period its wealth allowed its monasteries and parish churches to be rebuilt in grand style; Glastonbury Abbey was particularly important, and claimed to house the tomb of King Arthur and Guinevere. The city of Bath is famous for its Georgian architecture, and is a UNESCO World Heritage Site. The county is also the location of Glastonbury Festival, one of the UK's major music festivals.
Somerset is a historic county in the south west of England. There is evidence of human occupation since prehistoric times with hand axes and flint points from the Palaeolithic and Mesolithic eras, and a range of burial mounds, hill forts and other artefacts dating from the Neolithic, Bronze and Iron Ages. The oldest dated human road work in Great Britain is the Sweet Track, constructed across the Somerset Levels with wooden planks in the 39th century BCE.
Following the Roman Empire's invasion of southern Britain, the mining of lead and silver in the Mendip Hills provided a basis for local industry and commerce. Bath became the site of a major Roman fort and city, the remains of which can still be seen. During the Early Medieval period Somerset was the scene of battles between the Anglo-Saxons and first the Britons and later the Danes. In this period it was ruled first by various kings of Wessex, and later by kings of England. Following the defeat of the Anglo-Saxon monarchy by the Normans in 1066, castles were built in Somerset.
Expansion of the population and settlements in the county continued during the Tudor and more recent periods. Agriculture and coal mining expanded until the 18th century, although other industries declined during the industrial revolution. In modern times the population has grown, particularly in the seaside towns, notably Weston-super-Mare. Agriculture continues to be a major business, if no longer a major employer because of mechanisation. Light industries are based in towns such as Bridgwater and Yeovil. The towns of Taunton and Shepton Mallet manufacture cider, although the acreage of apple orchards is less than it once was.
The Palaeolithic and Mesolithic periods saw hunter-gatherers move into the region of Somerset. There is evidence from flint artefacts in a quarry at Westbury that an ancestor of modern man, possibly Homo heidelbergensis, was present in the area from around 500,000 years ago. There is still some doubt about whether the artefacts are of human origin but they have been dated within Oxygen Isotope Stage 13 (524,000 – 478,000 BP). Other experts suggest that "many of the bone-rich Middle Pleistocene deposits belong to a single but climatically variable interglacial that succeeded the Cromerian, perhaps about 500,000 years ago. Detailed analysis of the origin and modification of the flint artefacts leads to the conclusion that the assemblage was probably a product of geomorphological processes rather than human work, but a single cut-marked bone suggests a human presence." Animal bones and artefacts unearthed in the 1980s at Westbury-sub-Mendip, in Somerset, have shown evidence of early human activity approximately 700,000 years ago.
Homo sapiens sapiens, or modern man, came to Somerset during the Early Upper Palaeolithic. There is evidence of occupation of four Mendip caves 35,000 to 30,000 years ago. During the Last Glacial Maximum, about 25,000 to 15,000 years ago, it is probable that Somerset was deserted as the area experienced tundra conditions. Evidence was found in Gough's Cave of deposits of human bone dating from around 12,500 years ago. The bones were defleshed and probably ritually buried though perhaps related to cannibalism being practised in the area at the time or making skull cups or storage containers. Somerset was one of the first areas of future England settled following the end of Younger Dryas phase of the last ice age c. 8000 BC. Cheddar Man is the name given to the remains of a human male found in Gough's Cave in Cheddar Gorge. He is Britain's oldest complete human skeleton. The remains date from about 7150 BC, and it appears that he died a violent death. Somerset is thought to have been occupied by Mesolithic hunter-gatherers from about 6000 BCE; Mesolithic artefacts have been found in more than 70 locations. Mendip caves were used as burial places, with between 50 and 100 skeletons being found in Aveline's Hole. In the Neolithic era, from about 3500 BCE, there is evidence of farming.
At the end of the last ice age the Bristol Channel was dry land, but later the sea level rose, particularly between 1220 and 900 BC and between 800 and 470 BCE, resulting in major coastal changes. The Somerset Levels became flooded, but the dry points such as Glastonbury and Brent Knoll have a long history of settlement, and are known to have been occupied by Mesolithic hunters. The county has prehistoric burial mounds (such as Stoney Littleton Long Barrow), stone rows (such as the circles at Stanton Drew and Priddy) and settlement sites. Evidence of Mesolithic occupation has come both from the upland areas, such as in Mendip caves, and from the low land areas such as the Somerset Levels. Dry points in the latter such as Glastonbury Tor and Brent Knoll, have a long history of settlement with wooden trackways between them. There were also "lake villages" in the marsh such as those at Glastonbury Lake Village and Meare. One of the oldest dated human road work in Britain is the Sweet Track, constructed across the Somerset Levels with wooden planks in the 39th century BC, partially on the route of the even earlier Post Track.
There is evidence of Exmoor's human occupation from Mesolithic times onwards. In the Neolithic period people started to manage animals and grow crops on farms cleared from the woodland, rather than act purely as hunter gatherers. It is also likely that extraction and smelting of mineral ores to make tools, weapons, containers and ornaments in bronze and then iron started in the late Neolithic and into the Bronze and Iron Ages.
The caves of the Mendip Hills were settled during the Neolithic period and contain extensive archaeological sites such as those at Cheddar Gorge. There are numerous Iron Age Hill Forts, which were later reused in the Dark Ages, such as Cadbury Castle, Worlebury Camp and Ham Hill. The age of the henge monument at Stanton Drew stone circles is unknown, but is believed to be from the Neolithic period. There is evidence of mining on the Mendip Hills back into the late Bronze Age when there were technological changes in metal working indicated by the use of lead. There are numerous "hill forts", such as Small Down Knoll, Solsbury Hill, Dolebury Warren and Burledge Hill, which seem to have had domestic purposes, not just a defensive role. They generally seem to have been occupied intermittently from the Bronze Age onward, some, such as Cadbury Camp at South Cadbury, being refurbished during different eras. Battlegore Burial Chamber is a Bronze Age burial chamber at Williton which is composed of three round barrows and possibly a long, chambered barrow.
The Iron Age tribes of later Somerset were the Dobunni in north Somerset, Durotriges in south Somerset and Dumnonii in west Somerset. The first and second produced coins, the finds of which allows their tribal areas to be suggested, but the latter did not. All three had a Celtic culture and language. However, Ptolemy stated that Bath was in the territory of the Belgae, but this may be a mistake. The Celtic gods were worshipped at the temple of Sulis at Bath and possibly the temple on Brean Down. Iron Age sites on the Quantock Hills, include major hill forts at Dowsborough and Ruborough, as well as smaller earthwork enclosures, such as Trendle Ring, Elworthy Barrows and Plainsfield Camp.
Somerset was part of the Roman Empire from 47 AD to about 409 AD. However, the end was not abrupt and elements of Romanitas lingered on for perhaps a century.
Somerset was invaded from the south-east by the Second Legion Augusta, under the future emperor Vespasian. The hillforts of the Durotriges at Ham Hill and Cadbury Castle were captured. Ham Hill probably had a temporary Roman occupation. The massacre at Cadbury Castle seems to have been associated with the later Boudiccan Revolt of 60–61 AD. The county remained part of the Roman Empire until around 409 AD.
The Roman invasion, and possibly the preceding period of involvement in the internal affairs of the south of England, was inspired in part by the potential of the Mendip Hills. A great deal of the attraction of the lead mines may have been the potential for the extraction of silver.
Forts were set up at Bath and Ilchester. The lead and silver mines at Charterhouse in the Mendip Hills were run by the military. The Romans established a defensive boundary along the new military road known the Fosse Way (from the Latin fossa meaning ditch). The Fosse Way ran through Bath, Shepton Mallet, Ilchester and south-west towards Axminster. The road from Dorchester ran through Yeovil to meet the Fosse Way at Ilchester. Small towns and trading ports were set up, such as Camerton and Combwich. The larger towns decayed in the latter part of the period, though the smaller ones appear to have decayed less. In the latter part of the period, Ilchester seems to have been a "civitas" capital and Bath may also have been one. Particularly to the east of the River Parrett, villas were constructed. However, only a few Roman sites have been found to the west of the river. The villas have produced important mosaics and artifacts. Cemeteries have been found outside the Roman towns of Somerset and by Roman temples such as that at Lamyatt. Romano-British farming settlements, such as those at Catsgore and Sigwells, have been found in Somerset. There was salt production on the Somerset Levels near Highbridge and quarrying took place near Bath, where the Roman Baths gave their name to Bath.
Excavations carried out before the flooding of Chew Valley Lake also uncovered Roman remains, indicating agricultural and industrial activity from the second half of the 1st century until the 3rd century AD. The finds included a moderately large villa at Chew Park, where wooden writing tablets (the first in the UK) with ink writing were found. There is also evidence from the Pagans Hill Roman Temple at Chew Stoke. In October 2001 the West Bagborough Hoard of 4th century Roman silver was discovered in West Bagborough. The 681 coins included two denarii from the early 2nd century and 8 Miliarense and 671 Siliqua all dating to the period AD 337 – 367. The majority were struck in the reigns of emperors Constantius II and Julian and derive from a range of mints including Arles and Lyons in France, Trier in Germany and Rome.
In April 2010, the Frome Hoard, one of the largest-ever hoards of Roman coins discovered in Britain, was found by a metal detectorist. The hoard of 52,500 coins dated from the 3rd century AD and was found buried in a field near Frome, in a jar 14 inches (36 cm) below the surface. The coins were excavated by archaeologists from the Portable Antiquities Scheme.
This is the period from about 409 AD to the start of Saxon political control, which was mainly in the late 7th century, though they are said to have captured the Bath area in 577 AD. Initially the Britons of Somerset seem to have continued much as under the Romans but without the imperial taxation and markets. There was then a period of civil war in Britain though it is not known how this affected Somerset. The Western Wandsdyke may have been constructed in this period but archaeological data shows that it was probably built during the 5th or 6th century. This area became the border between the Romano-British Celts and the West Saxons following the Battle of Deorham in 577 AD. The ditch is on the north side, so presumably it was used by the Celts as a defence against Saxons encroaching from the upper Thames Valley. According to the Anglo-Saxon Chronicle, the Saxon Cenwalh achieved a breakthrough against the British Celtic tribes, with victories at Bradford-on-Avon (in the Avon Gap in the Wansdyke) in 652 AD, and further south at the Battle of Peonnum (at Penselwood) in 658 AD, followed by an advance west through the Polden Hills to the River Parrett.
The Saxon advance from the east seems to have been halted by battles between the British and Saxons, for example; at the siege of Badon Mons Badonicus (which may have been in the Bath region e.g. at Solsbury Hill), or Bathampton Down. During the 5th, 6th and 7th centuries, Somerset was probably partly in the Kingdom of Dumnonia, partly in the land of the Durotriges and partly in that of the Dobunni. The boundaries between these is largely unknown, but may have been similar to those in the Iron Age. Various "tyrants" seem to have controlled territories from reoccupied hill forts. There is evidence of an elite at hill forts such as Cadbury Castle and Cadbury Camp; for example, there is imported pottery. Cemeteries are an important source of evidence for the period and large ones have been found in Somerset, such as that at Cannington, which was used from the Roman to the Saxon period. The towns of Somerset seem to have been little used during that period but there continued to be farming on the villa sites and at the Romano-British villages.
There may have been effects from plague and volcanic eruption during this period as well as marine transgression into the Levels.
The language spoken during this period is thought to be Southwestern Brythonic, but only one or two inscribed stones survive in Somerset from this period. However, a couple of curse tablets found in the baths at Bath may be in this language. Some place names in Somerset seem to be Celtic in origin and may be from this period or earlier, e.g. Tarnock. Some river names, such as Parrett, may be Celtic or pre-Celtic. The religion of the people of Somerset in this period is thought to be Christian but it was isolated from Rome until after the Council of Hertford in 673 AD when Aldhelm was asked to write a letter to Geraint of Dumnonia and his bishops. Some church sites in Somerset are thought to date from this period, e.g., Llantokay Street.
Most of what is known of the history of this period comes from Gildas's On the Ruin of Britain, which is thought to have been written in Durotrigan territory, possibly at Glastonbury.
The earliest fortification of Taunton started for King Ine of Wessex and Æthelburg, in or about the year 710 AD. However, according to the Anglo-Saxon Chronicle this was destroyed 12 years later.
This is the period from the late 7th century (for most of Somerset) to 1066, though for part of the 10th and 11th centuries England was under Danish control. Somerset, like Dorset to the south, held the West Saxon advance from Wiltshire/Hampshire back for over a century, remaining a frontier between the Saxons and the Romano-British Celts.
The Saxons conquered Bath following the Battle of Deorham in 577, and the border was probably established along the line of the Wansdyke to the north of the Mendip Hills. Then Cenwalh of Wessex broke through at Bradford-on-Avon in 652, and the Battle of Peonnum possibly at Penselwood in 658, advancing west through the Polden Hills to the River Parrett. In 661 the Saxons may have advanced into what is now Devon as a result of a battle fought at Postesburh, possibly Posbury near Crediton.
Then in the period 681–85 Centwine of Wessex conquered King Cadwaladr and "advanced as far as the sea", but it is not clear where this was. It is assumed that the Saxons occupied the rest of Somerset about this time. The Saxon rule was consolidated under King Ine, who established a fort at Taunton, demolished by his wife in 722. It is sometimes said that he built palaces at Somerton and South Petherton but this does not seem to be the case. He fought against Geraint in 710. In 705 the diocese of Sherborne was formed, taking in Wessex west of Selwood. Saxon kings granted land in Somerset by charter from the 7th century onward. The way and extent to which the Britons survived under the Saxons is a debatable matter. However, King Ine's laws make provision for Britons. Somerset originally formed part of Wessex and latter became a separate "shire". Somersetshire seems to have been formed within Wessex during the 8th century though it is not recorded as a name until later. Mints were set up at times in various places in Somerset in the Saxon period, e.g., Watchet.
Somerset played an important part in defeating the spread of the Danes in the 9th century. The Anglo-Saxon Chronicle records that in 845 Alderman Eanwulf, with the men of Somersetshire (Sumorsǣte), and Bishop Ealstan, and Alderman Osric, with the men of Dorsetshire, conquered the Danish army at the mouth of the Parret. This was the first known use of the name Somersæte. The Anglo-Saxon Chronicle reports that in January 878 the King Alfred the Great fled into the marshes of Somerset from the Viking's invasion and made a fort at Athelney. From the fort Alfred was able to organize a resistance using the local militias from Somerset, Wiltshire and Hampshire.
Viking raids took place for instance in 987 and 997 at Watchet and the Battle of Cynwit. King Alfred was driven to seek refuge from the Danes at Athelney before defeating them at the Battle of Ethandun in 878, usually considered to be near Edington, Wiltshire, but possibly the village of Edington in Somerset. Alfred established a series of forts and lookout posts linked by a military road, or Herepath, so his army could cover Viking movements at sea. The Herepath has a characteristic form which is familiar on the Quantocks: a regulation 20 m wide track between avenues of trees growing from hedge laying embankments. The Herepath ran from the ford on the River Parrett at Combwich, past Cannington hill fort to Over Stowey, where it climbed the Quantocks along the line of the current Stowey road, to Crowcombe Park Gate. Then it went south along the ridge, to Triscombe Stone. One branch may have led past Lydeard Hill and Buncombe Hill, back to Alfred's base at Athelney. The main branch descended the hills at Triscombe, then along the avenue to Red Post Cross, and west to the Brendon Hills and Exmoor. A peace treaty with the Danes was signed at Wedmore and the Danish king Guthrum the Old was baptised at Aller. Burhs (fortified places) had been set up by 919, such as Lyng. The Alfred Jewel, an object about 2.5 inch long, made of filigree gold, cloisonné-enamelled and with a rock crystal covering, was found in 1693 at Petherton Park, North Petherton. Believed to have been owned by Alfred the Great it is thought to have been the handle for a pointer that would have fit into the hole at its base and been used while reading a book.
Monasteries and minster churches were set up all over Somerset, with daughter churches from the minsters in manors. There was a royal palace at Cheddar, which was used at times in the 10th century to host the Witenagemot, and there is likely to have been a "central place" at Somerton, Bath, Glastonbury and Frome since the kings visited them. The towns of Somerset seem to have been in occupation in this period though evidence for this is limited because of subsequent buildings on top of remains from this period. Agriculture flourished in this period, with a re-organisation into centralised villages in the latter part in the east of the county.
In the period before the Norman Conquest, Somerset came under the control of Godwin, Earl of Wessex, and his family. There seems to have been some Danish settlement at Thurloxton and Spaxton, judging from the place-names. After the Norman Conquest, the county was divided into 700 fiefs, and large areas were owned by the crown, with fortifications such as Dunster Castle used for control and defence.
This period of Somerset's history is well documented, for example in the Anglo-Saxon Chronicle and Asser's Life of Alfred.
This is the period from 1066 to around 1500. Following the defeat of the Saxons by the Normans in 1066, various castles were set up in Somerset by the new lords such as that at Dunster, and the manors was awarded to followers of William the Conqueror such as William de Moyon and Walter of Douai. Somerset does not seem to have played much part in the civil war in King Stephen's time, but Somerset lords were main players in the murder of Thomas Becket.
A good picture of the county in 1086 is given by Domesday Book, though there is some difficulty in identifying the various places since the hundreds are not specified. The total population given for the county, which had different boundaries to those today, was 13,399, however this only included the heads of households, so with their families this may have been around 67,000. Farming seems to have prospered for the next three centuries but was severely hit by the Black Death which in 1348 arrived in Dorset and quickly spread through Somerset, causing widespread mortality, perhaps as much as 50% in places. It re-occurred, resulting in a change in feudal practices since the manpower was no longer so available.
Reclamation of land from marsh in the Somerset Levels increased, largely under monastic influence. Crafts and industries also flourished, the Somerset woollen industry being one of the largest in England at this time. "New towns" were founded in this period in Somerset, i.e. Newport, but were not successful. Coal mining on the Mendips was an important source of wealth while quarrying also took place, an example is near Bath.
The towns grew, again often by monastic instigation, during this period and fairs were started. The church was very powerful at this period, particularly Glastonbury Abbey. After their church burnt down, the monks there "discovered" the tomb of "King Arthur" and were able rebuild their church. There were over 20 monasteries in Somerset at this period including the priory at Hinton Charterhouse which was founded in 1232 by Ela, Countess of Salisbury who also founded Lacock Abbey. Many parish churches were re-built in this period. Between 1107 and 1129 William Giffard the Chancellor of King Henry I, converted the bishop's hall in Taunton into Taunton Castle. Bridgwater Castle was built in 1202 by William Brewer. It passed to the king in 1233 and in 1245 repairs were ordered to its motte and towers. During the 11th century Second Barons' War against Henry III, Bridgwater was held by the barons against the King. In the English Civil War the town and the castle were held by the Royalists under Colonel Sir Francis Wyndham. Eventually, with many buildings destroyed in the town, the castle and its valuable contents were surrendered to the Parliamentarians. The castle itself was deliberately destroyed in 1645.
During the Middle Ages sheep farming for the wool trade came to dominate the economy of Exmoor. The wool was spun into thread on isolated farms and collected by merchants to be woven, fulled, dyed and finished in thriving towns such as Dunster. The land started to be enclosed and from the 17th century onwards larger estates developed, leading to establishment of areas of large regular shaped fields. During this period a Royal Forest and hunting ground was established, administered by the Warden. The Royal Forest was sold off in 1818.
In the medieval period the River Parrett was used to transport Hamstone from the quarry at Ham Hill, Bridgwater was part of the Port of Bristol until the Port of Bridgwater was created in 1348, covering 80 miles (130 km) of the Somerset coast line, from the Devon border to the mouth of the River Axe. Historically, the main port on the river was at Bridgwater; the river being bridged at this point, with the first bridge being constructed in 1200 AD. Quays were built in 1424; with another quay, the Langport slip, being built in 1488 upstream of the Town Bridge. A Customs House was sited at Bridgwater, on West Quay; and a dry dock, launching slips and a boat yard on East Quay. The river was navigable, with care, to Bridgwater Town Bridge by 400 to 500 tonnes (440 to 550 tons) vessels. By trans-shipping into barges at the Town Bridge the Parrett was navigable as far as Langport and (via the River Yeo) to Ilchester.
This is the period from around 1500 to 1800. In the 1530s, the monasteries were dissolved and their lands bought from the king by various important families in Somerset. By 1539, Glastonbury Abbey was the only monastery left, its abbot Richard Whiting was then arrested and executed on the orders of Thomas Cromwell. From the Tudor to the Georgian times, farming specialised and techniques improved, leading to increases in population, although no new towns seem to have been founded. Large country houses such as at Hinton St George and Montacute House were built at this time.
The Bristol Channel floods of 1607 are believed to have affected large parts of the Somerset Levels with flooding up to 8 feet (2 m) above sea level. In 1625, a House of Correction was established in Shepton Mallet and, today, HMP Shepton Mallet is England's oldest prison still in use.
During the English Civil War, Somerset was largely Parliamentarian, although Dunster was a Royalist stronghold. The county was the site of important battles between the Royalists and the Parliamentarians, notably the Battle of Lansdowne in 1643 and the Battle of Langport in 1645. The castle changed hands several times during 1642–45 along with the town. During the Siege of Taunton it was defended by Robert Blake, from July 1644 to July 1645. This war resulted in castles being destroyed to prevent their re-use.
In 1685, the Duke of Monmouth led the Monmouth Rebellion in which Somerset people fought against James II. The rebels landed at Lyme Regis and travelled north hoping to capture Bristol and Bath, puritan soldiers damaged the west front of Wells Cathedral, tore lead from the roof to make bullets, broke the windows, smashed the organ and the furnishings, and for a time stabled their horses in the nave. They were defeated in the Battle of Sedgemoor at Westonzoyland, the last battle fought on English soil. The Bloody Assizes which followed saw the losers being sentenced to death or transportation.
The Society of Friends established itself in Street in the mid-17th century, and among the close-knit group of Quaker families were the Clarks: Cyrus started a business in sheepskin rugs, later joined by his brother James, who introduced the production of woollen slippers and, later, boots and shoes. C&J Clark still has its headquarters in Street, but shoes are no longer manufactured there. Instead, in 1993, redundant factory buildings were converted to form Clarks Village, the first purpose-built factory outlet in the United Kingdom.
The 18th century was largely one of peace and declining industrial prosperity in Somerset. The Industrial Revolution in the Midlands and Northern England spelt the end for most of Somerset's cottage industries. However, farming continued to flourish, with the Bath and West of England Agricultural Society being founded in 1777 to improve methods. John Billingsley conducted a survey of the county's agriculture in 1795 but found that methods could still be improved.
Arthur Wellesley took his title, Duke of Wellington from the town of Wellington. He is commemorated on a nearby hill with a large, spotlit obelisk, known as the Wellington Monument.
In north Somerset, mining in the Somerset coalfield was an important industry, and in an effort to reduce the cost of transporting the coal the Somerset Coal Canal was built; part of it was later converted into a railway. Other canals included the Bridgwater and Taunton Canal, Westport Canal, Grand Western Canal, Glastonbury Canal and Chard Canal.[9] The Dorset and Somerset Canal was proposed, but very little of it was ever constructed.
The 19th century saw improvements to Somerset's roads with the introduction of turnpikes and the building of canals and railways. The usefulness of the canals was short-lived, though they have now been restored for recreation. The railways were nationalised after the Second World War, but continued until 1965, when smaller lines were scrapped; two were transferred back to private ownership as "heritage" lines.
In 1889, Somerset County Council was created, replacing the administrative functions of the Quarter Sessions.
The population of Somerset has continued to grow since 1800, when it was 274,000, particularly in the seaside towns such as Weston-super-Mare. Some population decline occurred earlier in the period in the villages, but this has now been reversed, and by 1951 the population of Somerset was 551,000.
Chard claims to be the birthplace of powered flight, as it was here in 1848 that the Victorian aeronautical pioneer John Stringfellow first demonstrated that engine-powered flight was possible through his work on the Aerial Steam Carriage. North Petherton was the first town in England (and one of the few ever) to be lit by acetylene gas lighting, supplied by the North Petherton Rosco Acetylene Company. Street lights were provided in 1906. Acetylene was replaced in 1931 by coal gas produced in Bridgwater, as well as by the provision of an electricity supply.
Around the 1860s, at the height of the iron and steel era, a pier and a deep-water dock were built, at Portishead, by the Bristol & Portishead Pier and Railway to accommodate the large ships that had difficulty in reaching Bristol Harbour. The Portishead power stations were coal-fed power stations built next to the dock. Construction work started on Portishead "A" power station in 1926. It began generating electricity in 1929 for the Bristol Corporation's Electricity Department. In 1951, Albright and Wilson built a chemical works on the opposite side of the dock from the power stations. The chemical works produced white phosphorus from phosphate rock imported, through the docks, into the UK. The onset of new generating capacity at Pembroke (oil-fired) and Didcot (coal-fired) in the mid-1970s brought about the closure of the older, less efficient "A" Station. The newer of the two power stations ("B" Station) was converted to burn oil when the Somerset coalfields closed. Industrial activities ceased in the dock with the closure of the power stations. The Port of Bristol Authority finally closed the dock in 1992, and it has now been developed into a marina and residential area.
During the First World War hundreds of Somerset soldiers were killed, and war memorials were put up in most of the towns and villages; only a few villages escaped casualties. There were also casualties – though much fewer – during the Second World War, who were added to the memorials. The county was a base for troops preparing for the 1944 D-Day landings, and some Somerset hospitals still date partly from that time. The Royal Ordnance Factory ROF Bridgwater was constructed early in World War II for the Ministry of Supply. It was designed as an Explosive ROF, to produce RDX, which was then a new experimental high-explosive. It obtained water supplies from two sources via the Somerset Levels: the artificial Huntspill River which was dug during the construction of the factory and also from the King's Sedgemoor Drain, which was widened at the same time. The Taunton Stop Line was set up to resist a potential German invasion, and the remains of its pill boxes can still be seen, as well as others along the coast. A decoy town was constructed on Black Down, intended to represent the blazing lights of a town which had neglected to follow the black-out regulations. Sites in the county housed Prisoner of War camps including: Norton Fitzwarren, Barwick, Brockley, Goathurst and Wells. Various airfields were built or converted from civilian use including: RNAS Charlton Horethorne (HMS Heron II), RAF Weston-super-Mare, RNAS Yeovilton (HMS Heron), Yeovil/Westland Airport, RAF Weston Zoyland, RAF Merryfield, RAF Culmhead and RAF Charmy Down.
Exmoor was one of the first British National Parks, designated in 1954, under the 1949 National Parks and Access to the Countryside Act. and is named after its main river. It was expanded in 1991 and in 1993 Exmoor was designated as an Environmentally Sensitive Area. The Quantock Hills were designated as an Area of Outstanding Natural Beauty (AONB) in 1956, the first such designation in England under the National Parks and Access to the Countryside Act 1949. The Mendip Hills followed with AONB designation in 1972.
Hinkley Point A nuclear power station was a Magnox power station constructed between 1957 and 1962 and operating until ceasing generation in 2000. Hinkley Point B is an Advanced Gas-cooled Reactor (AGR) which was designed to generate 1250 MW of electricity (MWe). Construction of Hinkley Point B started in 1967. In September 2008 it was announced, by Électricité de France (EDF), that a third, twin-unit European Pressurised Reactor (EPR) power station known as Hinkley Point C is planned, to replace Hinkley Point B which was due for closure in 2016, but has now has its life extended until 2022.
Somerset today has only two small cities, Bath and Wells, and only small towns in comparison with other areas of England. Tourism is a major source of employment along the coast, and in Bath and Cheddar for example. Other attractions include Exmoor, West Somerset Railway, Haynes Motor Museum and the Fleet Air Arm Museum as well as the churches and the various National Trust and English Heritage properties in Somerset.
Agriculture continues to be a major business, if no longer a major employer because of mechanisation. Light industries take place in towns such as Bridgwater and Yeovil. The towns of Taunton and Shepton Mallet manufacture cider, although the number of apple orchards has reduced.
In the late 19th century the boundaries of Somerset were slightly altered, but the main change came in 1974 when the county of Avon was set up. The northern part of Somerset was removed from the administrative control of Somerset County Council. On abolition of the county of Avon in 1996, these areas became separate administrative authorities, "North Somerset" and "Bath and North East Somerset". The Department for Communities and Local Government was considering a proposal by Somerset County Council to change Somerset's administrative structure by abolishing the five districts to create a Somerset unitary authority. The changes were planned to be implemented no later than 1 April 2009. However, support for the county council's bid was not guaranteed and opposition among the district council and local population was strong; 82% of people responding to a referendum organised by the five district councils rejected the proposals. It was confirmed in July 2007 that the government had rejected the proposals for unitary authorities in Somerset, and that the present two-tier arrangements of Somerset County Council and the district councils will remain.
Dylan Marlais Thomas (27 October 1914 – 9 November 1953) was a Welsh poet and writer whose works include the poems "Do not go gentle into that good night" and "And death shall have no dominion", the "play for voices", Under Milk Wood, and stories and radio broadcasts such as A Child's Christmas in Wales and Portrait of the Artist as a Young Dog. He became popular in his lifetime and remained so after his premature death in New York. In his later life he acquired a reputation, which he encouraged, as a "roistering, drunken and doomed poet".
Thomas was born in Swansea, Wales, in 1914. An undistinguished student, he left school at 16, becoming a journalist for a short time. Although many of his works appeared in print while he was still a teenager, it was the publication of "Light breaks where no sun shines", in 1934, that caught the attention of the literary world. While living in London, Thomas met Caitlin Macnamara, whom he married in 1937. Their relationship was defined by alcoholism and was mutually destructive. In the early part of his marriage, Thomas and his family lived hand-to-mouth, settling in the Welsh fishing village of Laugharne.
Although Thomas was appreciated as a popular poet in his lifetime, he found earning a living as a writer difficult, which resulted in him augmenting his income with reading tours and broadcasts. His radio recordings for the BBC during the latter half of the 1940s brought him a level of celebrity. In the 1950s, Thomas travelled to America, where his readings brought him a level of fame, though his erratic behaviour and drinking worsened. His time in America cemented Thomas' legend, where he recorded to vinyl works such as A Child's Christmas in Wales. During his fourth trip to New York in 1953, Thomas became gravely ill and fell into a coma from which he did not recover. Thomas died on 9 November 1953 and his body was returned to Wales where he was buried at the village churchyard in Laugharne.
In May 1948 Thomas and his family moved to his final home, the Boat House at Laugharne purchased for him at a cost of £2,500 in April 1949 by Margaret Taylor, first wife of historian A. J. P. Taylor. Thomas acquired a garage a hundred yards from the house on a cliff ledge which he turned into his writing shed, and where he penned several of his most acclaimed poems. Just before moving into there, Thomas rented "Pelican House" opposite his regular drinking den, Brown's Hotel, for his parents who lived there from 1949 until 1953. It was there that his father died and the funeral was held. Caitlin gave birth to their third child, a boy named Colm Garan Hart on 25 July 1949.
Source: Wikipedia Free Encyclopedia.
Photo in comments box of the Writing Shed.
★Includes: • Hud with 24 Colors for Top&Short • Maitreya//Belleza All Bodys// Slink & Hourglass In-world: maps.secondlife.com/secondlife/Bad%20Girls/155/94/25 Marketplace: marketplace.secondlife.com/p/KC-Xesca-Outfit/12821053
Models : Nany Jurado & Luixa Sciavo
Photographe: Nany Jurado
Shoreham Heroes - a new feature on the Beach end of the Adur Ferry Bridge. Peter Huxtable devoted 43 years to the RNLI, 20 as Coxswain of the Shoreham boat. Peter was involved in the rescue of 449 people and received 2 awards for gallantry
Prudhoe is a town in the south of Northumberland, England. It is 11 miles (18 km) west of Newcastle upon Tyne and just south of the River Tyne. Situated on a steep, north-facing hill in the Tyne valley, Prudhoe had a population of 11,675 at the 2011 census.
Nearby villages include Ovingham, Ovington, Wylam, Stocksfield, Crawcrook, Hedley on the Hill and Mickley.
The name derives from the Anglo-Saxon personal name Prud (from prūd, meaning 'proud') and hoe or haugh, 'a spur of land'.
There has been a castle at Prudhoe since ancient times, when England was at war with Scotland. The area now known as Castlefields was a fruit orchard, and the Scots were rumoured to have burnt this orchard while attempting to capture Prudhoe Castle. The castle, originally owned by the d'Umfraville family, then the Percys and now English Heritage, is considered to be the only medieval fortification in Northumberland never to have been captured by the Scots
In 1914, a Territorial Army drill hall was developed on Swalwell Close, which housed a company of the 4th Battalion of the Northumberland Fusiliers. The drill hall site (now disused) was scheduled to be redeveloped from 2018, with the scheme further delayed and complicated by the jailing of the owner for eight years in 2021.
During the Cold War, there was a Royal Observer Corps Underground Monitoring Post opposite Highfield Park; the surface features have since been demolished. It was one of approximately 1,563 similar underground monitoring posts built all across the UK during the Cold War to monitor the effects of a nuclear strike. They were operated by the Royal Observer Corps (ROC), mostly civilian volunteers, who worked in groups of three inside the posts. Prudhoe ROC post was opened in June 1962 and closed in September 1991 after the collapse of the Soviet Union, which saw the end of the Cold War.
Local government services for Prudhoe are provided by Northumberland County Council. The town is in the parliamentary constituency of Hexham. Prudhoe is the primary settlement within the Civil Parish of Prudhoe, which is situated in Tynedale. The Town Council meets at The Spetchells Centre, Front Street.
Traditionally Prudhoe has had more in common politically with places like Blaydon than the rest of Hexham constituency. For example, in 2013 both wards in Prudhoe returned Labour councillors, with the Conservatives only able to finish third. This contrasts with Hexham, where the Conservatives dominated, and especially other rural areas. However, in 2017, both Prudhoe wards were won by the Conservatives as they became the largest group on Northumberland County Council. In 2021 Prudhoe North returned to Labour when the ward was won by Angie Scott.
The town of Prudhoe is built on a steep, north-facing hill, with an elevation of up to 200 metres in the extreme south of the town. There is a prominent bend in the River Tyne, which the castle overlooks. To the south of Prudhoe is Prudhoe Moor, the very top of the town, and then a small valley where Prudhoe Hospital and Humbles Wood are located. As well as being steep and elevated, the land to the south of Prudhoe is heavily forested and rural. Further south are Hedley on the Hill, and then Ebchester over the County Durham border. Towards the north-east of Prudhoe Civil Parish is the steep Hagg Bank, which winds down to Hagg Bank Farm near Points Bridge on the riverside.
Via West Wylam and Eastwood Park, as well as Dukeshagg and Low Guards Wood, the eastern reaches of the town border the Metropolitan Borough of Gateshead, Tyne and Wear; near the A695 bypass is Stanley Burn, which flows out into the River Tyne at Wylam.
Prudhoe was once a coal mining town. There is still evidence of the old coal mine at West Wylam, signified by a miner's cart when driving into Castlefields up Cockshot Dean. The cart was found in brambles nearby by a former mine employee. This was the site of West Wylam Colliery. The main drift entrance of the colliery is buried under the modern road.
The town has an industrial estate, called Low Prudhoe that lies alongside the A695 road, which now bypasses the town to the north. There are a few factories and several smaller businesses straddling the side of this road.
Prudhoe has one large factory operated by essity. Originally built by Kimberly-Clark, the mill was bought by SCA after the Monopolies Commission forced Kimberly-Clark to sell.[citation needed] The factory consists of the mill, housing the paper machines, converting lines, warehousing and Unifibres and makes paper products such as tissues. The site where SCA stands was first used by ICI for producing agricultural fertiliser (sulfate and ammonium sulfate).[citation needed] In 1963 this plant closed leaving behind the "Spetchells" chalk hills – heaps of waste product which were subsequently turfed over. After ICI closed, the site was owned by Cleveland Engineering, which produced automobile parts,[citation needed] and following its closure in 1969 Kimberly-Clark opened.
Once home to a 1200-patient large mental health hospital based on the Prudhoe Hall site, Prudhoe was then home to a 40-bed specialist mental health facility for children and young people, Ferndene, which is operated by Cumbria Northumberland Tyne and Wear NHS Foundation Trust.
Prudhoe Castle is a Norman castle, which was for a long time involved in the border wars between England and Scotland. It was built by the de Umfraville family: the Norman Sir Robert de Umfraville was granted the freedom of Redesdale by William the Conqueror. For much of its history the castle was owned by the Percy family. It is now run by English Heritage. The castle is unique in being the only medieval defensive fortification in the whole of Northumbria (the modern counties of Northumberland, Tyne and Wear and County Durham to the south) to avoid capture by the Scots.
The majority of the surviving building work dates from the 12th century, although the site of Prudhoe Castle has strong Norman origins. In the 14th/15th centuries, the tower was extended to provide an extra level with turrets. Only the southwest turret survives to this day.
Prudhoe Hall (built 1868–70) and the Catholic Church of Our Lady and St Cuthbert in Prudhoe (built 1890–91, but incorporating the Cottier windows from an earlier smaller chapel built 1868–70) have some of Daniel Cottier's earliest stained glass. Matthew Liddell presumably commissioned Cottier to design the stained glass windows in both the main hall and the original chapel because his architect, Archibald Dunn, was impressed by the fact that Cottier had recently won a prize for the superb harmony of colours in his armorial window at the 1867 Paris International Exhibition. Indeed, Daniel Cottier has referred to his Paris prize in the graphite border of the large window in the main hall of Prudhoe Hall.
The stained glass in the small original chapel, which was opened on 19 October 1870, was eventually incorporated in the enlarged church of 1891 and then subsequently moved again a mile into the town of Prudhoe in 1904–05, when the Liddell family moved away from the area and could no longer support the Catholic mission, which Matthew Liddell had begun in 1870. The black-and-white photographs of the first chapel at Prudhoe Hall in Fr Paul Zielinski's book, The Church that Moved, show exactly the same windows containing the Cottier glass that have been retained in the larger church that replaced it. This means that the Cottier windows have been moved twice from their original site, and this would explain the necessity for so much extra remedial lead-work within some of the panes of glass, presumably repairing damage caused by two removals and two re-installations.
The small windows at Prudhoe Hall depicting idyllic naturalistic scenes of a rising sun over a river are especially beautiful, and seem to have a strong similarity to the work of Louis Comfort Tiffany. Made in about 1870, they pre-date by ten years or more the collaboration between Cottier and Tiffany in the 1880s in America. The swaying reeds in particular would seem to suggest that Cottier may well have been a significant influence on Tiffany before Tiffany returned the compliment, and Cottier brought some of his ideas back into his own artistic creations in Scotland.
There is a memorial stone to John Wesley set in a low wall on South Road (outside the former Prudhoe Council offices), the former main street of the town, commemorating his visits to the town.
Towards the eastern edge of Prudhoe is West Wylam, an area of largely social housing. It is home to an elderly care home, Prudhoe Town AFC, a small row of takeaways as well as a local NISA store and Eastwood Park; where several local football teams play their league games. The area also has allotments and Adderlane First School, which was opened in 1978. The last church on the estate, West Wylam Ebenezer Methodist Church, closed in 2014.
Prudhoe is linked to Newcastle upon Tyne and the A1 by the A695 which used to pass through the centre of the town along Front Street. The A695 road now bypasses the town to the north through the industrial estate at Low Prudhoe. The better transport links of the new bypass have allowed the industrial estate to expand alongside the new road to the east, named Princess Way after the royal who opened SCA Hygiene.
Northumberland County Council sought a significant landmark feature adjacent to the new bypass, and commissioned the Prudhoe Badger under their 'percent for art' policy. The sculpture is 30m long, and was constructed with the help of drystone wallers in stone and marble. It was designed to integrate with the rural environment, create awareness about ecology and provide a link with the nearby Countryside Centre. The badger sculpture is sited adjacent to the roundabout on the A695 road at Low Prudhoe.
The town is served by Prudhoe railway station on the Newcastle and Carlisle Railway, also known as the Tyne Valley Line. The line was opened in 1838, and links the city of Newcastle upon Tyne with Carlisle. The line follows the course of the River Tyne through Northumberland. Passenger services on the Tyne Valley Line are operated by Northern only after the May 2022 timetable change. The line is also heavily used for freight. The next railway stations are those at Wylam and Stocksfield.
The town has direct bus links to Newcastle, Hexham and the MetroCentre.
Local news and television programmes are provided by BBC North East and Cumbria and ITV Tyne Tees. Television signals are received from the Pontop Pike TV transmitter and one of the two relay transmitters (Newton and Fenham).
Local radio stations are BBC Radio Newcastle, Heart North East, Capital North East, Smooth Radio North East, Greatest Hits Radio North East, Metro Radio, Koast Radio and Radio Prudhoe, a community based station.
The town is served by the local newspapers, Hexham Courant and Chronicle Extra.
First schools:
Prudhoe Castle First School.
Prudhoe West First Academy (which celebrated its 100-year anniversary in 2009).
St Matthew's Catholic Primary.
Middle schools:
Highfield Middle School.
Ovingham Middle School.
Eastwood Middle School (closed in 2006 and is now home of Prudhoe Youth Football Club)
High schools:
Prudhoe Community High School.
Prudhoe is home to a number of churches, which form as a meeting place for the local community. The churches include:
The Parish Church of Saint Mary Magdalene (Church of England)
Prudhoe Methodist Church
Our Lady and Saint Cuthbert's Catholic Church
The Gate Church Prudhoe (formerly Prudhoe Community Church)
Edgewell Christian Centre
Prudhoe has its own senior football club, Prudhoe Town AFC, which formerly resided at Kimberley Park, West Wylam.
Tyne Riverside Country Park in Low Prudhoe lies on the southern bank of the River Tyne. The park includes the artificial chalk hills known as the "Spetchells" which have attracted some natural chalk-loving flora and fauna not normally found in the region. It has been proposed that they be made 'sites of scientific interest'. A public bridleway runs from the country park to Hagg Bank, over the Points Bridge to Wylam. Now forming a traffic-free part of National Cycle Network Route 72, it runs on the bed of a disused railway line to Newburn, Tyne and Wear, Newcastle upon Tyne, and on to the coast at Tynemouth.
Prudhoe Town Football Club are currently in the Wearside Football League, in the eleventh tier of the English football league system. The future of the club has recently been in doubt following the loss of its ground, Kimberley Park, in West Wylam.
Prudhoe Waterworld provides swimming and other fitness activities and is the home of Prudhoe Millennium Tapestry.
The town has a skatepark, Highfield Park, which is located at the top of Prudhoe.
Prudhoe is home to the North East Ferret Rescue, which helps unwanted and abandoned ferrets. It is the only active ferret rescue in the North East of England.
Notable people
Henry Travers (1874–1965), Oscar-nominated character actor who is perhaps best known as the angel Clarence from It's a Wonderful Life. He was born in Prudhoe, but grew up in Berwick-upon-Tweed.
Gaz Beadle, star of reality TV show, Geordie Shore from 2011 to 2017.
Jak Alnwick, Footballer (Goalkeeper), who currently plays for Scottish premiership team St. Mirren, and his brother Ben Alnwick, Footballer (Goalkeeper), who played for Bolton Wanderers, were born in Prudhoe.
John Callender – (1903–1980), English footballer, born at West Wylam
George Honeyman, Footballer (Midfielder), who currently plays for Millwall, was born in Prudhoe
Steven Savile, English science fiction and fantasy novelist and game writer, lived in Prudhoe between 1985–1991
Popular culture
Prudhoe is the hometown of Ruth Archer and her mother Heather Pritchard, in the long-running BBC radio serial The Archers.
International links
France – Prudhoe is twinned with Mitry-Mory, near Paris, France. Evidence of this partnership is seen when entering the town and there are several murals depicting the twinning.
United States – Prudhoe Bay, an area of northern Alaska containing the largest oil field in the US is named indirectly after Prudhoe. The explorer, John Franklin, who discovered the area, named it after his good friend, Baron Prudhoe of Prudhoe.
Northumberland is a ceremonial county in North East England, bordering Scotland. It is bordered by the Scottish Borders to the north, the North Sea to the east, Tyne and Wear and County Durham to the south, and Cumbria to the west. The town of Blyth is the largest settlement.
The county has an area of 5,013 km2 (1,936 sq mi) and a population of 320,274, making it the least-densely populated county in England. The south-east contains the largest towns: Blyth (37,339), Cramlington (27,683), Ashington (27,670), and Morpeth (14,304), which is the administrative centre. The remainder of the county is rural, and the largest towns are Berwick-upon-Tweed (12,043) in the far north and Hexham (13,097) in the west. For local government purposes the county is a unitary authority area. The county historically included the parts of Tyne and Wear north of the River Tyne.
The west of Northumberland contains part of the Cheviot Hills and North Pennines, while to the east the land becomes flatter before reaching the coast. The Cheviot (815 m (2,674 ft)), after which the range of hills is named, is the county's highest point. The county contains the source of the River North Tyne and much of the South Tyne; near Hexham they combine to form the Tyne, which exits into Tyne and Wear shortly downstream. The other major rivers in Northumberland are, from south to north, the Blyth, Coquet, Aln, Wansbeck and Tweed, the last of which forms part of the Scottish border. The county contains Northumberland National Park and two national landscapes: the Northumberland Coast and part of the North Pennines.
Much of the county's history has been defined by its position on a border. In the Roman era most of the county lay north of Hadrian's Wall, and the region was contested between England and Scotland into the Early Modern era, leading to the construction of many castles, peel towers and bastle houses, and the early modern fortifications at Berwick-upon-Tweed. Northumberland is also associated with Celtic Christianity, particularly the tidal island of Lindisfarne. During the Industrial Revolution the area had significant coal mining, shipbuilding, and armaments industries.
Northumberland, England's northernmost county, is a land where Roman occupiers once guarded a walled frontier, Anglian invaders fought with Celtic natives, and Norman lords built castles to suppress rebellion and defend a contested border with Scotland. The present-day county is a vestige of an independent kingdom that once stretched from Edinburgh to the Humber, hence its name, meaning literally 'north of the Humber'. Reflecting its tumultuous past, Northumberland has more castles than any other county in England, and the greatest number of recognised battle sites. Once an economically important region that supplied much of the coal that powered the industrial revolution, Northumberland is now a primarily rural county with a small and gradually shrinking population.
As attested by many instances of rock art, the Northumberland region has a rich prehistory. Archeologists have studied a Mesolithic structure at Howick, which dates to 7500 BC and was identified as Britain's oldest house until it lost this title in 2010 when the discovery of the even older Star Carr house in North Yorkshire was announced, which dates to 8770 BC. They have also found tools, ornaments, building structures and cairns dating to the bronze and iron ages, when the area was occupied by Brythonic Celtic peoples who had migrated from continental Europe, most likely the Votadini whose territory stretched from Edinburgh and the Firth of Forth to Northumberland. It is not clear where the boundary between the Votadini and the other large tribe, the Brigantes, was, although it probably frequently shifted as a result of wars and as smaller tribes and communities changed allegiances. Unlike neighbouring tribes, Votadini farms were surrounded by large walls, banks and ditches and the people made offerings of fine metal objects, but never wore massive armlets. There are also at least three very large hillforts in their territory (Yeavering Bell, Eildon Hill and Traprain Law, the latter two now in Scotland), each was located on the top of a prominent hill or mountain. The hillforts may have been used for over a thousand years by this time as places of refuge and as places for meetings for political and religious ceremonies. Duddo Five Stones in North Northumberland and the Goatstones near Hadrian's Wall are stone circles dating from the Bronze Age.
When Gnaeus Julius Agricola was appointed Roman governor of Britain in 78 AD, most of northern Britain was still controlled by native British tribes. During his governorship Agricola extended Roman control north of Eboracum (York) and into what is now Scotland. Roman settlements, garrisons and roads were established throughout the Northumberland region.
The northern frontier of the Roman occupation fluctuated between Pons Aelius (now Newcastle) and the Forth. Hadrian's Wall was completed by about 130 AD, to define and defend the northern boundary of Roman Britain. By 142, the Romans had completed the Antonine Wall, a more northerly defensive border lying between the Forth and Clyde. However, by 164 they abandoned the Antonine Wall to consolidate defences at Hadrian's Wall.
Two important Roman roads in the region were the Stanegate and Dere Street, the latter extending through the Cheviot Hills to locations well north of the Tweed. Located at the intersection of these two roads, Coria (Corbridge), a Roman supply-base, was the most northerly large town in the Roman Empire. The Roman forts of Vercovicium (Housesteads) on Hadrian's Wall, and Vindolanda (Chesterholm) built to guard the Stanegate, had extensive civil settlements surrounding them.
The Celtic peoples living in the region between the Tyne and the Forth were known to the Romans as the Votadini. When not under direct Roman rule, they functioned as a friendly client kingdom, a somewhat porous buffer against the more warlike Picts to the north.
The gradual Roman withdrawal from Britain in the 5th century led to a poorly documented age of conflict and chaos as different peoples contested territories in northern Britain.
Nearly 2000-year-old Roman boxing gloves were uncovered at Vindolanda in 2017 by the Vidolanda Trust experts led by Dr Andrew Birley. According to the Guardian, being similar in style and function to the full-hand modern boxing gloves, these two gloves found at Vindolanda look like leather bands date back to 120 AD. It is suggested that based on their difference from gladiator gloves warriors using this type of gloves had no purpose to kill each other. These gloves were probably used in a sport for promoting fighting skills. The gloves are currently displayed at Vindolanda's museum.
Conquests by Anglian invaders led to the establishment of the kingdoms of Deira and Bernicia. The first Anglian settlement was effected in 547 by Ida, who, accompanied by his six sons, pushed through the narrow strip of territory between the Cheviots and the sea, and set up a fortress at Bamburgh, which became the royal seat of the Bernician kings. About the end of the 6th century Bernicia was first united with the rival kingdom of Deira under the rule of Æthelfrith of Northumbria, and the district between the Humber and the Forth became known as the kingdom of Northumbria.
After Æthelfrith was killed in battle around 616, Edwin of Deira became king of Northumbria. Æthelfrith's son Oswald fled northwest to the Gaelic kingdom of Dál Riata where he was converted to Christianity by the monks of Iona. Meanwhile, Paulinus, the first bishop of York, converted King Edwin to Roman Christianity and began an extensive program of conversion and baptism. By his time the kingdom must have reached the west coast, as Edwin is said to have conquered the islands of Anglesey and Man. Under Edwin the Northumbrian kingdom became the chief power in Britain. However, when Cadwallon ap Cadfan defeated Edwin at Hatfield Chase in 633, Northumbria was divided into the former kingdoms of Bernicia and Deira and Christianity suffered a temporary decline.
In 634, Oswald defeated Cadwallon ap Cadfan at the Battle of Heavenfield, resulting in the re-unification of Northumbria. Oswald re-established Christianity in the kingdom and assigned a bishopric at Hexham, where Wilfrid erected a famous early English church. Reunification was followed by a period of Northumbrian expansion into Pictish territory and growing dominance over the Celtic kingdoms of Dál Riata and Strathclyde to the west. Northumbrian encroachments were abruptly curtailed in 685, when Ecgfrith suffered complete defeat by a Pictish force at the Battle of Nechtansmere.
When Saint Aidan came at the request of Oswald to preach to the Northumbrians he chose the island of Lindisfarne as the site of his church and monastery, and made it the head of the diocese which he founded in 635. For some years the see continued in peace, numbering among its bishops Saint Cuthbert, but in 793 Vikings landed on the island and burnt the settlement, killing many of the monks. The survivors, however, rebuilt the church and continued to live there until 883, when, through fear of a second invasion of the Danes, they fled inland, taking with them the body of Cuthbert and other holy relics.
Against this background, the monasteries of Northumbria developed some remarkably influential cultural products. Cædmon, a monk at Whitby Abbey, authored one of the earliest surviving examples of Old English poetry some time before 680. The Lindisfarne Gospels, an early example of insular art, is attributed to Eadfrith, the bishop of Lindisfarne from 698 to 721. Stenton (1971, p. 191) describes the book as follows.
In mere script it is no more than an admirable example of a noble style, and the figure drawing of its illustrations, though probably based on classical models, has more than a touch of naïveté. Its unique importance is due to the beauty and astonishing intricacy of its decoration. The nature of its ornament connects it very closely with a group of Irish manuscripts of which the Book of Kells is the most famous.
Bede's writing, at the Northumbrian monasteries at Wearmouth and Jarrow, gained him a reputation as the most learned scholar of his age. His work is notable for both its breadth (encompassing history, theology, science and literature) and quality, exemplified by the rigorous use of citation. Bede's most famous work is Ecclesiastical History of the English People, which is regarded as a highly influential early model of historical scholarship.
The kingdom of Northumbria ceased to exist in 927, when it was incorporated into England as an earldom by Athelstan, the first king of a united England[citation needed].. In 937, Athelstan's victory over a combined Norse-Celtic force in the battle of Brunanburh secured England's control of its northern territory.
The Scottish king Indulf captured Edinburgh in 954, which thenceforth remained in possession of the Scots. His successors made repeated attempts to extend their territory southwards. Malcolm II was finally successful, when, in 1018, he annihilated the Northumbrian army at Carham on the Tweed, and Eadulf the earl of Northumbria ceded all his territory to the north of that river as the price of peace. Henceforth Lothian, consisting of the former region of Northumbria between the Forth and the Tweed, remained in possession of the Scottish kings.
The term Northumberland was first recorded in its contracted modern sense in 1065 in an entry in the Anglo-Saxon Chronicle relating to a rebellion against Tostig Godwinson.
The vigorous resistance of Northumbria to William the Conqueror was punished by ruthless harrying, mostly south of the River Tees. As recounted by the Anglo-Saxon Chronicle:
A.D. 1068. This year King William gave Earl Robert the earldom over Northumberland; but the landsmen attacked him in the town of Durham, and slew him, and nine hundred men with him. Soon afterwards Edgar Etheling came with all the Northumbrians to York; and the townsmen made a treaty with him: but King William came from the South unawares on them with a large army, and put them to flight, and slew on the spot those who could not escape; which were many hundred men; and plundered the town. St. Peter's minster he made a profanation, and all other places also he despoiled and trampled upon; and the ethelling went back again to Scotland.
The Normans rebuilt the Anglian monasteries of Lindisfarne, Hexham and Tynemouth, and founded Norman abbeys at Newminster (1139), Alnwick (1147), Brinkburn (1180), Hulne, and Blanchland. Castles were built at Newcastle (1080), Alnwick (1096), Bamburgh (1131), Harbottle (1157), Prudhoe (1172), Warkworth (1205), Chillingham, Ford (1287), Dunstanburgh (1313), Morpeth, Langley (1350), Wark on Tweed and Norham (1121), the latter an enclave of the palatine bishops of Durham.
Northumberland county is not mentioned in the Domesday Survey, but the account of the issues of the county, as rendered by Odard the sheriff, is entered in the Great Roll of the Exchequer for 1131.
In 1237, Scotland renounced claims to Northumberland county in the Treaty of York.
During the reign of Edward I (1272–1307), the county of Northumberland was the district between the Tees and the Tweed, and had within it several scattered liberties subject to other powers: Durham, Sadberge, Bedlingtonshire, and Norhamshire belonging to the bishop of Durham; Hexhamshire to the archbishop of York; Tynedale to the king of Scotland; Emildon to the earl of Lancaster; and Redesdale to Gilbert de Umfraville, Earl of Angus. These franchises were exempt from the ordinary jurisdiction of the shire. Over time, some were incorporated within the county: Tynedale in 1495; Hexhamshire in 1572; and Norhamshire, Islandshire and Bedlingtonshire by the Counties (Detached Parts) Act 1844.
The county court for Northumberland was held at different times at Newcastle, Alnwick and Morpeth, until by statute of 1549 it was ordered that the court should thenceforth be held in the town and castle of Alnwick. Under the same statute the sheriffs of Northumberland, who had been in the habit of appropriating the issues of the county to their private use, were required thereafter to deliver in their accounts to the Exchequer in the same manner as the sheriffs of other counties.
From the Norman Conquest until the union of England and Scotland under James I and VI, Northumberland was the scene of perpetual inroads and devastations by the Scots. Norham, Alnwick and Wark were captured by David I of Scotland in the wars of Stephen's reign. In 1174, during his invasion of Northumbria, William I of Scotland, also known as William the Lion, was captured by a party of about four hundred mounted knights, led by Ranulf de Glanvill. This incident became known as the Battle of Alnwick. In 1295, Robert de Ros and the earls of Athol and Menteith ravaged Redesdale, Coquetdale and Tynedale. In 1314 the county was ravaged by king Robert Bruce. And so dire was the Scottish threat in 1382, that by special enactment the earl of Northumberland was ordered to remain on his estates to protect the border. In 1388, Henry Percy was taken prisoner and 1500 of his men slain at the battle of Otterburn, immortalised in the ballad of Chevy Chase.
Alnwick, Bamburgh and Dunstanburgh were garrisoned for the Lancastrian cause in 1462, but after the Yorkist victories of Hexham and Hedgley Moor in 1464, Alnwick and Dunstanburgh surrendered, and Bamburgh was taken by storm.
In September 1513, King James IV of Scotland was killed at the Battle of Flodden on Branxton Moor.
Roman Catholic support in Northumberland for Mary, Queen of Scots, led to the Rising of the North in 1569.
After uniting the English and Scottish thrones, James VI and I sharply curbed the lawlessness of the border reivers and brought relative peace to the region. There were Church of Scotland congregations in Northumberland in the 17th and 18th centuries.
During the Civil War of the 17th century, Newcastle was garrisoned for the king by the earl of Newcastle, but in 1644 it was captured by the Scots under the earl of Leven, and in 1646 Charles I was led there a captive under the charge of David Leslie.
Many of the chief Northumberland families were ruined in the Jacobite rebellion of 1715.
The mineral resources of the area appear to have been exploited to some extent from remote times. It is certain that coal was used by the Romans in Northumberland, and some coal ornaments found at Angerton have been attributed to the 7th century. In a 13th-century grant to Newminster Abbey a road for the conveyance of sea coal from the shore about Blyth is mentioned, and the Blyth coal field was worked throughout the 14th and 15th centuries. The coal trade on the Tyne did not exist to any extent before the 13th century, but from that period it developed rapidly, and Newcastle acquired the monopoly of the river shipping and coal trade. Lead was exported from Newcastle in the 12th century, probably from Hexhamshire, the lead mines of which were very prosperous throughout the 16th and 17th centuries. In a charter from Richard I to Hugh de Puiset creating him earl of Northumberland, mines of silver and iron are mentioned. A salt pan is mentioned at Warkworth in the 12th century; in the 13th century the salt industry flourished at the mouth of the river Blyth, and in the 15th century formed the principal occupation of the inhabitants of North and South Shields. In the reign of Elizabeth I, glass factories were set up at Newcastle by foreign refugees, and the industry spread rapidly along the Tyne. Tanning, both of leather and of nets, was largely practised in the 13th century, and the salmon fisheries in the Tyne were famous in the reign of Henry I.
John Smeaton designed the Coldstream Bridge and a bridge at Hexham.
Stephenson's Rocket
Invention of the steam turbine by Charles Algernon Parsons
Includes teams from Brookings, SF Lincoln, SF Roosevelt, RC Central. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.
©2021 SDPB
02/12/17 #1797. Action from a comfortable win for Shoreham over an under strength Rye side, who were unable to field a full team of 15 players. I went for a mix of the conventional and arty panning shots.
Includes teams from Mitchell, Harrisburg, Watertown, Aberdeen Central. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.
©2021 SDPB
Includes teams from Mitchell, Harrisburg, Watertown, Aberdeen Central. Permission granted for journalism outlets and educational purposes. Not for commercial use. Must be credited. Photo courtesy of South Dakota Public Broadcasting.
©2021 SDPB
Evening light on the way to a social evening at the pub with some colleagues from work - the first, and given the new restrictions announced today, possibly last, for some time.
Wabi-sabi #69 for the Treasure Hunt
· ▸ Particles & Sound Enabled
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Orbit and Mirror Version.
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Lowell National Historical Park in Lowell, Massachusetts, includes several sites in and around the city related to the era of textile manufacturing during the Industrial Revolution.
The Boott Cotton Mills building included a museum with a working loom.
It was an amazing park to visit. It was also depressing to see the large and dangerous looms that children were expected to run.
We visited the park in July 2003.