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List Of Volcanoes In Scotland
There are no active volcanoes in the United Kingdom of Great Britain and Northern Ireland, although a few do exist in some British Overseas Territories, including Queen Mary's Peak in Tristan da Cunha, Soufrière Hills volcano on the Caribbean island of Montserrat, as well as Mount Belinda and Mount Michael in the British Overseas Territory of South Georgia and the South Sandwich Islands. The last time that volcanoes were active in what is now the United Kingdom was the early Palaeogene period, just over 50 million years ago (Ma), associated with the opening of the Atlantic Ocean. Modern day hills and mountains within the UK which are sometimes described as extinct volcanoes are usually the deeply eroded roots of volcanoes active in prehistoric times. Some locations popularly believed to be volcanoes, such as The Wrekin, actually have different origins, such as being sites where volcanic material was deposited. List Below is a list of extinct volcanoes in the United Kingdom. E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Overseas Territories
The British Overseas Territories (BOTs) or alternatively referred to as the United Kingdom Overseas Territories (UKOTs) are the fourteen dependent territory, territories with a constitutional and historical link with the United Kingdom that, while not forming part of the United Kingdom itself, are part of its sovereign territory. The permanently inhabited territories are delegated varying degrees of internal self-governance, with the United Kingdom retaining responsibility for Military, defence, foreign relations, and internal security, and ultimate responsibility for governance. Three of the territories are chiefly or only inhabited by military or scientific personnel, the rest hosting significant civilian populations. All fourteen have the British monarch as head of state. These UK government responsibilities are assigned to various departments of the Foreign, Commonwealth and Development Office and are subject to change. Population Most of the territories retain permanent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gurnard's Head
Gurnard's Head (, meaning ''desolate one''; ) is a prominent headland on the north coast of the Penwith peninsula in Cornwall, England. The name is supposed to reflect that the rocky peninsula resembles the head of the gurnard fish. Geography and geology Gurnard's Head is the site of basaltic pillow lavas, formed by underwater volcanic eruptions up to 400 million years ago. It is north of the hamlet of Treen in the parish of Zennor, to the west of Zennor Head. Almost entirely owned by the National Trust, the headland is within the Aire Point to Carrick Du SSSI, and the South West Coast Path crosses the southern part of the headland. The area is designated as part of the Penwith Heritage Coast and also designated as part of the Cornwall Area of Outstanding Natural Beauty. A pub and hotel on the B3306 coast road shares a name with the headland. History The headland is the site of an Iron Age promontory fort known as Trereen Dinas (not to be confused with Treryn Dinas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scawt Hill
Scawt Hill is a volcanic plug in County Antrim, Northern Ireland, in the borough of Larne, 5 km from the village of Ballygally. It gets its name from the Ulster Scots "" meaning scaly, scabby or rugged. Alternatively, '' 'scawt' '' meaning scruffy and contemptible, and when applied to rocks, covered in barnacles. Discovery of minerals Scawt Hill is notable for being the type locality for several hydrated calcium silicates, that is, the place where they were first identified. These minerals were formed when the existing chalk of the area was intensely altered by the intrusion of the feeder tube of an ancient volcano, now long since cooled and eroded to its roots.Wilson, H E et al (1986) Geological Survey of Northern Ireland, HMSO Minerals that were first discovered at Scawt Hill: * Larnite (''calcium orthosilicate'') a natural form of belite discovered in 1929 and named after Larne, the nearest town * Scawtite in 1929 * Portlandite in 1933 * Hydrocalumite in 1934 * Rank ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Ireland
Northern Ireland ( ; ) is a Countries of the United Kingdom, part of the United Kingdom in the north-east of the island of Ireland. It has been #Descriptions, variously described as a country, province or region. Northern Ireland shares Republic of Ireland–United Kingdom border, an open border to the south and west with the Republic of Ireland. At the 2021 United Kingdom census, 2021 census, its population was 1,903,175, making up around 3% of the Demographics of the United Kingdom#Population, UK's population and 27% of the population on the island of Ireland#Demographics, Ireland. The Northern Ireland Assembly, established by the Northern Ireland Act 1998, holds responsibility for a range of Devolution, devolved policy matters, while other areas are reserved for the Government of the United Kingdom, UK Government. The government of Northern Ireland cooperates with the government of Ireland in several areas under the terms of the Good Friday Agreement. The Republic of Ireland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Giant's Causeway
The Giant's Causeway () is an area of approximately 40,000 interlocking basalt columns, the result of an ancient volcano, volcanic fissure eruption, part of the North Atlantic Igneous Province active in the region during the Paleogene period. It is located in County Antrim on the north coast of Northern Ireland, about northeast of the town of Bushmills, County Antrim, Bushmills. It was declared a World Heritage Site by UNESCO in 1986 and a national nature reserve (United Kingdom), national nature reserve by the Department of the Environment (Northern Ireland), Department of the Environment for Northern Ireland in 1987. In a 2005 poll of ''Radio Times'' readers, the Giant's Causeway was named the fourth-greatest Wonders of the World, natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although some have four, five, seven, or eight sides. The tallest are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carrick-a-Rede Rope Bridge
The Carrick-a-Rede Rope Bridge (locally pronounced carrick-a-reed) is a rope bridge near Ballintoy in County Antrim, Northern Ireland. The bridge links the mainland to the tiny island of Carrickarede (). It spans and is above the rocks below. The bridge is mainly a tourist attraction and is owned and maintained by the National Trust. In 2018, the bridge had 485,736 visitors. The bridge is closed for winter (subject to weather) and people may cross it for a £13.50 to £15.50 (adult) fee. History It is thought salmon fishermen have been building bridges to the island for over 350 years. It has taken many forms over the years. In the 1970s it had only one handrail and large gaps between the slats. A new bridge, tested up to ten tonnes, was built with the help of local climbers and abseilers in 2000. Another was built in 2004 and offered visitors and fishermen alike a much safer passage to the island. The current wire rope and Douglas fir bridge was made by Heyn Construction i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hercynian Orogeny
The Variscan orogeny, or Hercynian orogeny, was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea. Nomenclature The name ''Variscan'' comes from the Medieval Latin name for the district '' Variscia'', the home of a Germanic tribe, the Varisci; Eduard Suess, professor of geology at the University of Vienna, coined the term in 1880. ( Variscite, a rare green mineral first discovered in the Vogtland district of Saxony in Germany, which is in the Variscan belt, has the same etymology.) ''Hercynian'', on the other hand, derives from the Hercynian Forest. Both words were descriptive terms of strike directions observed by geologists in the field, ''variscan'' for southwest to northeast, ''hercynian'' for northwest to southeast. The ''variscan'' direction reflected the direction of ancient fold belts cropping out throughout Germany and adjacent countries and the meaning shi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warboys
Warboys is a large village and civil parish in the Huntingdonshire non-metropolitan district, district of Cambridgeshire, England, north-east of Huntingdon. Geology Igneous diorite rocks are located around below ground at Warboys. Discovered in the 1960s, it is suspected that these rocks form the remnants of a volcano of the Hercynian Orogeny (+300 MYA). History Warboys is a large parish and a village on what was the eastern side of Huntingdonshire bordering on Cambridgeshire. The place-name 'Warboys' is first attested in a Saxon charter of 974, where it appears as ''Wardebusc'' and ''Weardebusc''. The name is perhaps from the Old Norse ''vardi'' and ''buski'', and means 'beacon with bushes'. "Wearda" was also an Old English personal name, and it has been suggested this word means, literally, "bush of a man called Wearda", or, that the first element is from the Old English "weard" (‘watch, protection’). Additionally, the first Norman family to settle there was nam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a Geologic time scale, geologic period and System (stratigraphy), system of the Paleozoic era (geology), era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the Permian Period, Ma. It is the fifth and penultimate period of the Paleozoic era and the fifth period of the Phanerozoic eon (geology), eon. In North America, the Carboniferous is often treated as two separate geological periods, the earlier Mississippian (geology), Mississippian and the later Pennsylvanian (geology), Pennsylvanian. The name ''Carboniferous'' means "coal-bearing", from the Latin ("coal") and ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern "system" names, it was coined by geologists William Conybeare (geologist), William Conybeare and William Phillips (geologist), William Phillips in 1822, based on a study of the British rock succession. Carboniferous is the per ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scafell Pike
Scafell Pike () is a mountain in the Lake District region of Cumbria, England. It has an elevation of above sea level, making it the highest and the most prominent mountain in England. The mountain is part of the Scafell massif, an extinct volcano, and is one of the Southern Fells. Etymology and name history The name ''Scafell'' is believed by some to derive from the Old Norse ''skalli fjall'', meaning either the fell with the shieling or the fell with the bald summit, and is first recorded in 1578 in the corrupted form ''Skallfield''. Alternatively, ''Scafell'' means "the mountain of the ''scaw'' (or promontory)". This usage can be compared etymologically with, for example, Skaw, Unst. The name originally referred to Scafell, which neighbours Scafell Pike.Dorothy Wordsworth's ascent of Scafell Pike, 1818, http://www.pastpresented.ukart.com/eskdale/wordsworth1.htm What are now known as Scafell Pike, Ill Crag, and Broad Crag were collectively called either ''the Pik ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scafells
The Scafells, or Scafell Massif, are a range of fells in the Cumbrian Mountains of England, made up of the remains of a caldera volcano. Fells in the range include Broad Crag, Ill Crag, Scafell, and Scafell Pike, England's tallest mountain. Great End, Lingmell and Slight Side are also usually included within the definition. These hills form part of the Southern Fells. Image:Annotated Scafell range.jpg, left, 400px, The Scafell range as seen looking west from Crinkle Crags. (Interactive labels.) rect 23 372 252 419 Slight Side (762m) rect 173 794 560 834 Scafell East Buttress rect 707 787 893 861 Esk Crag or Buttress (c. 750m) rect 245 303 409 358 Sca Fell (964m) rect 408 238 637 280 Mickledore (c.840m) rect 544 174 826 213 South Summit (c. 950m) rect 706 310 928 355 Scafell Pike (978m) rect 870 238 1108 286 Broad Crag (934m) rect 1043 308 1198 360 Ill Crag (935m) rect 1238 311 1446 351 Great End (910m) rect 0 0 1444 1085 Click hyperlink or button to expand desc n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lundy
Lundy is an English island in the Bristol Channel. It forms part of the district of Torridge in the county of Devon. About long and wide, Lundy has had a long and turbulent history, frequently changing hands between the British crown and various usurpers. In the 1920s, the island's owner, Martin Harman, tried to issue his own coinage and was fined. In 1941, two German Heinkel He 111 bombers crash landed on the island, and their crews were captured. In 1969, Lundy was purchased by British millionaire Jack Hayward, who donated it to the National Trust. It is now managed by the Landmark Trust, a conservation charity that derives its income from day trips and holiday lettings, most visitors arriving by boat from Bideford or Ilfracombe. A local tourist curiosity is the special "Puffin" postage stamp, a category known by philatelists as "local carriage labels", a collectors' item. As a steep, rocky island, often shrouded by fog, Lundy has been the scene of many shipwrec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
