Beinn Eighe
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Beinn Eighe
Beinn Eighe () is a mountain massif in the Torridon area of Wester Ross in the Northwest Highlands of Scotland. Lying south of Loch Maree, it forms a long ridge with many spurs and summits, two of which are classified as Munros: Ruadh-stac Mòr at and Spidean Coire nan Clach at . Unlike most other hills in the area it has a cap of Cambrian basal quartzite which gives the peaks of Beinn Eighe a distinctive light colour. Its complex topography has made it popular with both hillwalkers and climbers and the national nature reserve on its northern side makes it an accessible mountain for all visitors. Geography Located between Loch Maree and Glen Torridon on the west coast of Scotland, Beinn Eighe is a complex mountain. The main ridge runs on a line extending from close to the village of Kinlochewe in the north-east to the narrow glen of the Coire Dubh Mòr, which separates it from the neighbouring mountain of Liathach to the south-west. The slopes into Glen Torrido ...
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Kinlochewe
Kinlochewe ( gd, Ceann Loch Iù or ) is a village in Wester Ross in the Northwest Highlands of Scotland. It is in the parish of Gairloch, the community of Torridon and Kinlochewe and the Highland council area. It lies near the head of Loch Maree in its magnificent valley, and serves as a junction between the main Ullapool road north, and that which heads west to the coast at Loch Torridon. Loch Maree was at one time also known as Loch Ewe, hence the village's apparently confused name. Community Kinlochewe has a couple of shops, a hotel and bunkhouse, mountain chalets, several bed and breakfasts, a post office (with internet café), and one of very few petrol filling stations for many miles in any direction. Buses connect the village with Gairloch, the railhead at Achnasheen, Dingwall and Inverness. The village contains two churches, Kinlochewe Free Church, built in 1873, and the Church of Scotland. To the north of the village, by the car park, is a First World War (1914–18) ...
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Ridge
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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Climbing
Climbing is the activity of using one's hands, feet, or any other part of the body to ascend a steep topographical object that can range from the world's tallest mountains (e.g. the eight thousanders), to small boulders. Climbing is done for locomotion, sporting recreation, and for competition, and is also done in trades that rely on ascension; such as emergency rescue and military operations. Climbing is done indoors and outdoors and on natural (e.g. rock and ice) and artificial surfaces. Professional mountain guides or rock climbing guides (e.g. the UIAGM), were a significant element in developing the popularity of the sport in the natural environment, and remain so today. Since the 1980s, the development of competition climbing and the availability of artificial climbing walls have dramatically increased the popularity of rock climbing as a sport and led to the emergence of professional rock climbers, such as Wolfgang Güllich, Chris Sharma, Lynn Hill and Catherine ...
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Rock (geology)
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing ro ...
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Topographic Prominence
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key Saddle point, saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting pat ...
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National Trust For Scotland
The National Trust for Scotland for Places of Historic Interest or Natural Beauty, commonly known as the National Trust for Scotland ( gd, Urras Nàiseanta na h-Alba), is a Scottish conservation organisation. It is the largest membership organisation in Scotland and describes itself as "the conservation charity that protects and promotes Scotland's natural and cultural heritage for present and future generations to enjoy". The Trust owns and manages around 130 properties and of land, including castles, ancient small dwellings, historic sites, gardens, coastline, mountains and countryside. It is similar in function to the National Trust, which covers England, Wales, and Northern Ireland, and to other national trusts worldwide. History The Trust was established in 1931 following discussions held in the smoking room of Pollok House (now a Trust property). The Trust was incorporated on 1 May 1931, with John Stewart-Murray, 8th Duke of Atholl being elected as its first president, ...
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NatureScot
NatureScot ( gd, NàdarAlba), which was formerly known as Scottish Natural Heritage, is an executive non-departmental public body of the Scottish Government responsible for the country's natural heritage, especially its natural, genetic and scenic diversity. It advises the Scottish Government on nature conservation, and acts as a government agent in the delivery of conservation designations, i.e. national nature reserves, local nature reserves, national parks, Site of Special Scientific Interest, Sites of Special Scientific Interest (SSSIs), Special Area of Conservation, Special Areas of Conservation, Special Protection Areas and the national scenic area (Scotland), national scenic areas. It receives annual funding from the Government in the form of Grant in Aid to deliver Government priorities for the natural heritage. NatureScot is the Scottish Government's adviser on all aspects of nature, wildlife management and landscape across Scotland, and also helps the Scottish G ...
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A832 Road
The A832 is a road in the Scottish Highlands, linking Cromarty, on the east coast, to Gairloch on the west coast, and beyond Gairloch to Braemore Junction. It is long and runs entirely in the former county of Ross and Cromarty. The road forms part of the Wester Ross Coastal Trail. Cromarty to Gorstan Starting in Cromarty on the Black Isle, the A832 travels south alongside the Moray Firth to Fortrose, then turns west, heading inland. It crosses the A9 and A835 at Tore and continues to Muir of Ord, passing near to the Beauly Firth. Five miles after Muir of Ord, the A832 meets the A835 again at a T-junction, and turning left, multiplexes with the A835 for nine miles (14 km) to Gorstan. On this stretch it passes Contin, the Rogie Falls and Loch Garve. Gorstan to Gairloch At Gorstan the A832 and A835 diverge again. They meet again later on at Braemore Junction, where the A832 terminates at the A835. From Gorstan to Braemore Junction on the A835 is , however on the A832 it ...
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A896 Road
List of A roads in zone 8 in Great Britain starting north of the A8 and west of the A9 (roads beginning with 8). Single- and double-digit roads Triple-digit roads Four-digit roads See also * B roads in Zone 8 of the Great Britain numbering scheme * List of motorways in the United Kingdom This list of motorways in the United Kingdom is a complete list of motorways in the United Kingdom. Note that the numbering scheme used for Great Britain does not include roads in Northern Ireland, which are allocated numbers on an ad hoc basis ... * Transport in Glasgow#Other Roads * Transport in Scotland#Road {{UK road lists 8 ...
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Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ...
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