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Cairn Toul
Cairn Toul ( gd, Càrn an t-Sabhail, 'hill of the barn') is the fourth-highest mountain in Scotland and all of the British Isles, after Ben Nevis, Ben Macdui and Braeriach. The summit is 1,291 metres (4,236 feet) above sea level. It is in the western massif of the Cairngorms, linked by a bealach at about 1125 m to Braeriach. The mountain towers above the Lairig Ghru pass. Cairn Toul is often climbed together with other peaks. From the south, it may be climbed with The Devil's Point, which lies about 2.5 kilometres south-southeast. Alternatively, it may be climbed from the north, including Braeriach and Sgor an Lochain Uaine. Both routes are long days by Scottish standards: around 15 km (plus return) regardless of whether one starts from Coire Cas above Speyside, or Linn of Dee to the south. The mountain may also be climbed from the west, starting from Achlean in Glen Feshie. This provides for a slighter shorter route (around 27 km for the round trip), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Braeriach
Braeriach or Brae Riach ( gd, Am Bràigh Riabhach, 'the brindled upland') is the third-highest mountain in Scotland and all of the British Isles, after Ben Nevis and Ben Macdui, rising above sea level. It is in the Scottish Highlands and is the highest point in the western massif of the Cairngorms, separated from the central section by the Lairig Ghru pass. The summit is a crescent-shaped plateau, overlooking several Cirque, corries. The lingering snows of Braeriach are amongst the most persistent snow patches in Scotland and the whole British Isles. The north-facing Cirque, corrie of Garbh Coire Mor has been snow-free just nine times in the last one hundred years: 1933, 1959, 1996, 2003, 2006, 2017, 2018, 2021 and 2022 – but four times in the six years to 2022. The rate and occurrence of melting appears to be increasing. Probably the most commonly used route up Braeriach starts from Sugar Bowl car park, on the road leading to the Cairn Gorm ski area. From here a path lea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coire Cas , a town in Switzerland
{{Disambig ...
Coire may refer to: Geography * Cirque, a terrain feature created by glaciation in high mountains * Chur , neighboring_municipalities= Arosa, Churwalden, Tschiertschen-Praden, Domat/Ems, Felsberg, Malix, Trimmis, Untervaz, Pfäfers , twintowns = Bad Homburg (Germany), Cabourg (France), Mayrhofen (Austria), Mondorf-les-Bains (Luxembourg), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Aberdeenshire
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of The Cairngorms
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyns Of Scotland
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Ireland by height. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,011 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophonous with (Marilyn) '' Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequent British Isles classifications that rely solely on prominence, including the P600s, the HuMPs, and the TuMPs. Topographic prominence is a more difficult to estimate than t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Munros
A Munro () is defined as a mountain in Scotland with a height over , and which is on the Scottish Mountaineering Club (SMC) official list of Munros; there is no explicit topographical prominence requirement. The best known Munro is Ben Nevis (Beinn Nibheis), the highest mountain in the British Isles at . Munros are named after Sir Hugh Munro, 4th Baronet (1856–1919), who produced the first list of such hills, known as ''Munro's Tables'', in 1891. Also included were what Munro considered lesser peaks, now known as Munro Tops, which are also over 3,000 feet but are lower than the nearby primary mountain. The publication of the original list is usually considered to be the epoch event of modern peak bagging. The list has been the subject of subsequent variation and as of 10 December 2020, the Scottish Mountaineering Club has listed 282 Munros and 226 Munro Tops. "Munro bagging" is the activity of climbing all the listed Munros. As of 31 December 2021, 7,098 people had reported ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Scotland
Scotland is the most mountainous country in the United Kingdom. Scotland's mountain ranges can be divided in a roughly north to south direction into: the Scottish Highlands, the Central Belt and the Southern Uplands, the latter two primarily belonging to the Scottish Lowlands. The highlands eponymously contains the country's main mountain ranges, but hills and mountains are to be found south of these as well. The below lists are not exhaustive; there are countless subranges throughout the country. Ben Nevis (Beinn Nibheis), the highest mountain in Scotland and the United Kingdom at , is in the Highland region at the western end of the Grampian Mountains. A Scottish mountain over is referred to as a Munro, of which there are 282. As of 2019, hundreds of thousands of people visit mountains in Scotland every winter and 130,000 climb to the summit of Ben Nevis every year. Highlands Scotland's main mountainous region can be broadly further split into the Northwest Highlands, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Munro Mountains
This is a list of Munro mountains and Munro Tops in Scotland by height. Munros are defined as Scottish mountains over in height, and which are on the Scottish Mountaineering Club ("SMC") official list of Munros. In addition, the SMC define Munro Tops, as Scottish peaks above that are not considered Munros. Where the SMC lists a Munro Top, due to "insufficient separation", it will also list the "Parent Peak", a Munro, of the Munro Top. As of 6 September 2012, there were 282 Scottish Munros after the SMC confirmed that Beinn a' Chlaidheimh had been downgraded to a Corbett and as of 10 December 2020, there were 226 Scottish Munro Tops after Stob Coire na Cloiche, a Munro Top to Parent Peak Sgùrr nan Ceathramhnan, was surveyed at 912.5m and was deleted as a Munro Top and downgraded to a Corbett Top. The current SMC list totals 508 summits. While the SMC does not use a prominence metric for classifying Munros, all but one of the 282 Munros have a prominence above , the exception ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Defile (geography)
In geography, a defile is a narrow pass or gorge between mountains or hills. The term originates from a military description of a route through which troops can march only in a narrow column or with a narrow front. On emerging from a defile (or something similar) into open country, soldiers are said to "debouch". Background In a traditional military formation, soldiers march in ranks (the depth of the formation is the number of ranks) and files (the width of the formation is the number of files), so, if a column of soldiers approaches a narrow pass, the formation must narrow, and so the files on the outside must be ordered to the rear (or to some other position) so that the column has fewer files and more ranks. The French verb for this order is ''défiler'', from which the English verb comes, as does the physical description for a valley that forces this manoeuvre. Defiles of military significance can also be formed by other physical features that flank a pass or path and cause ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corrour Bothy
Corrour Bothy is a simple stone building on Mar Lodge Estate, Aberdeenshire, Scotland. It is located below Coire Odhar between The Devil's Point and Cairn Toul on the western side of the River Dee in the Lairig Ghru. The bothy is a single room with a fireplace and chimney in its northern gable. Its dimensions are 19.6 ft (6 m) by 11.8 ft (3.6m) . There is a toilet in the wooden extension to the building. It is used as a mountain refuge and as a starting point for ascents of Munros including The Devil's Point, Cairn Toul, and Braeriach. Name The name ''Corrour'' is used as a name for the locality as well as specifically as a name for the bothy itself, the name being derived from Coire Odhar according to , who continues: In the author gives the local pronunciation as ''Corower'', but without explanation. However in the section "Hints on Gaelic pronunciation" appears to suggest the final-vowels of ''Coire'' (and corrie) are dropped to give ''kor'', and that the '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bothy
A bothy is a basic shelter, usually left unlocked and available for anyone to use free of charge. It was also a term for basic accommodation, usually for gardeners or other workers on an estate. Bothies are found in remote mountainous areas of Scotland, Northern England, Ulster and Wales. They are particularly common in the Scottish Highlands, but related buildings can be found around the world (for example, in the Nordic countries there are wilderness huts). A bothy was also a semi-legal drinking den in the Isle of Lewis. These, such as ''Bothan Eòrapaidh'', were used until recent years as gathering points for local men and were often situated in an old hut or caravan. In Scots law, bothies are defined in law as: a building of no more than two storeys which— (a)does not have any form of— (i)mains electricity, (ii)piped fuel supply, and (iii)piped mains water supply, (b)is 100 metres or more from the nearest public road (within the meaning of section 151 of the Roads (S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
