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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 (Scotland), 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 slope ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kinlochewe
Kinlochewe ( 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) memorial. Two s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ridge
A ridge is a long, narrow, elevated geomorphologic landform, structural feature, or a combination of both separated from the surrounding terrain by steep sides. The sides of a ridge slope away from a narrow top, the crest or ridgecrest, with the terrain dropping down on either side. The crest, if narrow, is also called a ridgeline. Limitations on the dimensions of a ridge are lacking. Its height above the surrounding terrain can vary from less than a meter to hundreds of meters. A ridge can be either depositional, erosional, tectonic, or a combination of these in origin and can consist of either bedrock, loose sediment, lava, or ice depending on its origin. A ridge can occur as either an isolated, independent feature or part of a larger geomorphological and/or structural feature. Frequently, a ridge can be further subdivided into smaller geomorphic or structural elements. Classification As in the case of landforms in general, there is a lack of any commonly agreed clas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing
Climbing is the activity of using one's hands, feet, or other parts 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, for competition, and is also done in trades that rely on ascension, such as construction and military operations. Climbing is done indoors and outdoors, on natural surfaces (e.g. rock climbing and ice climbing), and on artificial surfaces (e.g. climbing walls and climbing gyms). The sport of climbing evolved by climbers making first ascents of new types of climbing routes, using new climbing techniques, at ever-increasing grades of difficulty, with ever-improving pieces of climbing equipment. Guides and guidebooks were an important element in developing the popularity of the sport in the natural environment. Early pioneers included Walter Bonatti, Riccardo Cassin, Hermann Buhl, and Gaston Rébuffat, wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 compound, chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the Earth's crust, crust, and most of its interior, except for the liquid Earth's outer core, 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 weathe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Prominence
In topography, prominence or relative height (also referred to as autonomous height, and shoulder drop in US English, and drop 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. The key col ("saddle") around the peak is a unique point on this contour line and the ''parent peak'' (if any) is some higher mountain, selected according to various criteria. Definitions The prominence of a peak is 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 manner: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''highest saddle (landform), saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prominence is the differ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Trust For Scotland
The National Trust for Scotland () is a Scottish Building preservation and conservation trusts in the UK, conservation organisation. It is the largest membership organisation in Scotland and describes itself as "the charity that cares for, shares and speaks up for Scotland's magnificent heritage". The trust owns and manages around 130 properties and of land, including List of castles in Scotland, castles, ancient small dwellings, historic sites, Gardens in Scotland, gardens, coastline, mountains and countryside. It is similar in function to the National Trust, which covers England, Wales, and Northern Ireland, and to National trust, other national trusts worldwide. History The trust was established in 1931 as the "National Trust for Scotland for Places of Historic Interest or Natural Beauty", following discussions held in the smoking room of Pollok House. The Trust was incorporated on 1 May 1931, with John Stewart-Murray, 8th Duke of Atholl being elected as its first presiden ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
NatureScot
NatureScot () is an Scottish public bodies#Executive NDPBs, executive non-departmental public body of the Scottish Government responsible for Scotland’s natural heritage, especially its nature, natural, genetics, 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 reserve (Scotland), national nature reserves, local nature reserves, National parks of Scotland, 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 Scottish Government in the form of Grant in Aid to deliver government priorities for Scotland’s natural heritage. NatureScot is the Scottish Government's adviser on all aspects of nature, wildlife management ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 road (Great Britain), A9 and A835 road, A835 at Tore, Scotland, Tore and continues to Muir of Ord, passing near to the Beauly Firth. Five miles after Muir of Ord, the A832 meets the A835 road, A835 again at a T-junction, and turning left, multiplexes with the A835 for 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ) is an amphitheatre-like valley formed by Glacier#Erosion, glacial erosion. Alternative names for this landform are corrie (from , 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 overdeepening, 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 (lake), tarn (small lake) behind a d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
