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Beinn Liath Mhòr
Beinn Liath Mhòr is a Scottish mountain situated in the mountainous area between Strath Carron and Glen Torridon in Wester Ross in the Highland region. Geologically Beinn Liath Mhòr is made up of Cambrian quartzite scree and Torridonian sandstones giving the mountain a distinctive colour contrast of light and dark. The mountain's other main characteristic is its two-kilometre-long undulating summit ridge which does not drop below 800 metres for its entire length. This culminates at the summit at its far western end at a height of 926 metres (3038 feet) making Beinn Liath Mhòr the 258th highest Munro. Ascent The most common approach to Beinn Liath Mhòr starts at Achnashellach on the A890 road and goes by the right of way to Glen Torridon. This follows the impressive Coire Lair, a rugged corrie surrounded by three imposing mountains, the other two being Sgorr Ruadh (which is also a Munro) and Fuar Tholl which is ranked as one of the finest Corbetts by mountain writers. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Munro
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 4,411 ft (1,345 m). 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 (reference date), epoch event of modern peak bagging. The list has been the subject of subsequent variation and , the Scottish Mountaineering Club has listed 282 Munros and 226 Munro Tops. "Munro bagging" is the activity of climbing all the listed Munros. , 7,654 people had rep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rights Of Way In Scotland
A right of way (also right-of-way) is a specific route that people, animals, vehicles, watercraft, or utility lines travel, or the legal status that gives them the right to do so. Rights-of-way in the physical sense include controlled-access highways, railroads, canals, hiking paths, bridle paths for horses, bicycle paths, the routes taken by high-voltage lines (also known as wayleave), utility tunnels, or simply the paved or unpaved local roads used by different types of traffic. The term ''highway'' is often used in legal contexts in the sense of "main way" to mean any public-use road or any public-use road or path. Some are restricted as to mode of use (for example, pedestrians only, pedestrians, horse and cycle riders, vehicles capable of a minimum speed). Rights-of-way in the legal sense (the right to pass through or to operate a transportation facility) can be created in a number of different ways. In some cases, a government, transportation company, or conservation n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of The Northwest Highlands
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 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 climate, mountains t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyns Of Scotland
This is a list of Marilyn hills and mountains in the United Kingdom, Ireland and surrounding islands and sea stacks. 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 2,010 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 more difficult to es ... [...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 4,411 ft (1,345 m). 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 (reference date), epoch event of modern peak bagging. The list has been the subject of subsequent variation and , the Scottish Mountaineering Club has listed 282 Munros and 226 Munro Tops. "Munro bagging" is the activity of climbing all the listed Munros. , 7,654 people had rep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Liathach From Beinn Liath Mhor
; pronounced ) is a mountain in the Torridon Hills, in the Northwest Highlands of Scotland. It stands between Loch Torridon and the neighbouring mountain Beinn Eighe. The mountain is a ridge running east–west, with several peaks, and its upper half is made up of many steep rocky terraces. The highest peak is the Munro of Spidean a' Choire Lèith ('peak of the grey corrie') at high. The other Munro peak is Mullach an Rathain at high. Geology The mountain is composed of Torridonian sandstone which forms massive near-horizontal strata. They form the numerous terraces that are obvious from afar. The rocks are mainly red and chocolate sandstones, arkoses, flagstones and shales with coarse conglomerates locally at the base. Some of the materials of these rocks were derived from the underlying Lewisian gneiss, upon the uneven surface of which they rest, but the bulk of the material was obtained from rocks that are nowhere now exposed. Upon this ancient denuded land surface the To ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Torridon
Loch Torridon () is a sea loch on the west coast of Scotland in the Northwest Highlands. The loch was created by glacial processes and is in total around 15 miles (25 km) long. It has two sections: Upper Loch Torridon to landward, east of Rubha na h-Airde Ghlaise, at which point it joins Loch Sheildaig; and the main western section of Loch Torridon proper. Loch a' Chracaich and Loch Beag are small inlets on the southern shores of the outer Loch, which joins the Inner Sound, Scotland, Inner Sound between the headlands of Rubha na Fearna to the south and Red Point to the north. The name ''Thoirbhearta'' has a similar root to ''Tarbert'' and indicates a place where boats were dragged overland. Islands The islets in the loch include: * in Loch Shieldaig: Eilean an Inbhire Bhàin, Eilean Dùghaill and Shieldaig Island. * in Upper Loch Torridon: Eilean à Chaoil, Eilean Cnapach, both of which are tidal. * in outer Loch Torridon: Eilean Mòr, Loch Torridon, Eilean Mòr, Eilean Tior ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Liathach
; pronounced ) is a mountain in the Torridon Hills, in the Northwest Highlands of Scotland. It stands between Loch Torridon and the neighbouring mountain Beinn Eighe. The mountain is a ridge running east–west, with several peaks, and its upper half is made up of many steep rocky terraces. The highest peak is the Munro of Spidean a' Choire Lèith ('peak of the grey corrie') at high. The other Munro peak is Mullach an Rathain at high. Geology The mountain is composed of Torridonian sandstone which forms massive near-horizontal strata. They form the numerous terraces that are obvious from afar. The rocks are mainly red and chocolate sandstones, arkoses, flagstones and shales with coarse conglomerates locally at the base. Some of the materials of these rocks were derived from the underlying Lewisian gneiss, upon the uneven surface of which they rest, but the bulk of the material was obtained from rocks that are nowhere now exposed. Upon this ancient denuded land surface the T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cairn
A cairn is a human-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the (plural ). Cairns have been and are used for a broad variety of purposes. In prehistory, they were raised as markers, as memorials and as burial monuments (some of which Chambered cairn, contained chambers). In the modern era, cairns are often raised as landmarks, especially to mark the summits of mountains, and as Trail blazing, trail markers. They vary in size from small piles of stones to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in size from small rock sculptures to substantial human-made hills of stone (some built on top of larger, natural hills). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hill Lists In The British Isles
The mountains and hills of the British Isles are categorised into various lists based on different combinations of elevation, prominence, and other criteria such as isolation. These lists are used for peak bagging, whereby hillwalkers attempt to reach all the summits on a given list, the oldest being the 282 Munros in Scotland, created in 1891. A height above 2,000 ft, or more latterly 610 m, is considered necessary to be classified as a mountain – as opposed to a hill – in the British Isles. With the exception of Munros, all the lists require a prominence above . A prominence of between (e.g. some Nuttalls and Vandeleur-Lynams), does not meet the International Climbing and Mountaineering Federation (UIAA) definition of an "independent peak", which is a threshold over . Most lists consider a prominence between as a "top" (e.g. many Hewitts and Simms). Marilyns, meanwhile, have a prominence above , with no additional height threshold. They range from small hills to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fuar Tholl
Fuar Tholl is a mountain in the Scottish Highlands, highlands of Scotland. The mountain is situated in the Coulin deer forest 21 km SW of Achnasheen in the Wester Ross region of the Highland (council area), Highland council area. Overview Fuar Tholl has a rocky summit, and has acquired the nickname Wellington's Nose because the summit ridge is similar in profile to an upturned face which bears a supposed likeness to Arthur Wellesley, 1st Duke of Wellington. The considerable nose on the face is provided the tip of the Mainreachan Buttress which can just be seen over the outline of the main summit. Fuar Tholl reaches a height of 907 metres (2976 feet) making it the 13th highest Corbett (hill), Corbett.www.scotclimb.org.uk. Gives list of Corbetts in height order. It fails to reach Munro status by just seve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sgorr Ruadh
Sgorr Ruadh () is a mountain between Strath Carron and Glen Torridon in Wester Ross in the Northwest Highlands of Scotland. It is located in Coire Lair near Achnashellach along with two other mountains, Beinn Liath Mhòr and Fuar Tholl, and is often climbed together with one or both of these other mountains. Geography Sgurr Ruadh is an attractive peak with Munro status which reaches a height of 962 metres (3156 feet), it is made up of red sandstone (hence its translated name of Red Peak) and shows many of the characteristics of the Torridon Hills to the west, in that it has steep terraced buttresses and considerable scree slopes. The north west face has precipitous cliffs which should be avoided by walkers, although these crags attract rock climbers with around 20 recognised traditional and winter climbs. The centre of the crag is split by a large couloir (gully). There are plenty of easier routes on the crag. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
