Aonach Beag
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Aonach Beag
Aonach Beag is a mountain in the Scottish Highlands. It is located about 3 km east of Ben Nevis on the north side of Glen Nevis, near the town of Fort William. Apart from Ben Nevis, Aonach Beag is the highest peak in the British Isles outwith the Cairngorm mountains of eastern Scotland. Aonach Beag is linked to its close neighbour to the north, Aonach Mòr, by a high saddle or bealach. The name Aonach Beag (''small ridge'') might imply that this mountain is smaller than Aonach Mòr (''big ridge''). However, Aonach Beag is higher; the names refer to the relative bulk of the two mountains rather than their elevation. The easiest way up is to take the gondola lift serving the Nevis Range ski area on Aonach Mòr to an elevation of 650 m and follow the ridge joining the two peaks. More traditionally, the hill is often climbed from the south from Glen Nevis. This way the walker avoids the paraphernalia associated with the ski development. Aonach Beag is often clim ...
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Aonach Mòr
Aonach Mòr is a mountain in the Scottish Highlands. It is located about northeast of Ben Nevis on the south side of Glen Spean, near Fort William. The mountain has a summit elevation of and is classified as a Munro. The name Aonach Mòr (''big ridge'') might suggest that the mountain is taller than its close neighbour to the south, Aonach Beag (''small ridge'') to which it is linked by a high bealach. However, the names refer to the relative bulk of the mountains when seen from the glen, rather than their elevation; the summit of Aonach Mòr is lower than the summit of Aonach Beag. The quickest and shortest ascent route for hikers is to take the gondola to the Snowgoose Terminal at an elevation of and then hike to the summit. More traditionally, the mountain is often climbed from the south from Glen Nevis and in conjunction with Aonach Beag. Climate The summit of Aonach Mòr has tundra climate (''ET'' climate in the Köppen classification). The annual mean temperature i ...
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Cairngorms
The Cairngorms ( gd, Am Monadh Ruadh) are a mountain range in the eastern Highlands of Scotland closely associated with the mountain Cairn Gorm. The Cairngorms became part of Scotland's second national park (the Cairngorms National Park) on 1 September 2003. Although the Cairngorms give their name to, and are at the heart of, the Cairngorms National Park, they only form one part of the national park, alongside other hill ranges such as the Angus Glens and the Monadhliath, and lower areas like Strathspey. The Cairngorms consists of high plateaux at about above sea level, above which domed summits (the eroded stumps of once much higher mountains ) rise to around . Many of the summits have tors, free-standing rock outcrops that stand on top of the boulder-strewn landscape. In places, the edges of the plateau form steep cliffs of granite and they are excellent for skiing, rock climbing and ice climbing. The Cairngorms form an arctic-alpine mountain environment, with tundra-like ...
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Mountains And Hills Of The Central 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 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 ...
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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 ...
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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 ...
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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, ...
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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 ...
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Snow Patches In Scotland
Long-lying snow patches in Scotland have been noted from at least the 18th century, with snow patches on Ben Nevis being observed well into summer and autumn. Indeed, the summit observatory, which operated from 1883 to 1904, reported that snow survived on the north-east cliffs through more years than it vanished. More recently, additional and methodical field study on the subject has been carried out by others, most notably by ecologist Dr Adam Watson. Most of this work concentrated on the mountains of north-east Scotland (in particular, the Cairngorms), but more recent observations by him and others has shed light on various locations throughout Scotland where long-lying snow persists. The available information systematically gathered by observers over the last 50 years or so, and greatly increased since the 1990s, has built up a level of knowledge that points to Scotland's snow patches being now amongst the best documented in the world. General locations There are many loc ...
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Skiing
Skiing is the use of skis to glide on snow. Variations of purpose include basic transport, a recreational activity, or a competitive winter sport. Many types of competitive skiing events are recognized by the International Olympic Committee (IOC), and the International Ski Federation (FIS). History Skiing has a history of almost five millennia. Although modern skiing has evolved from beginnings in Scandinavia, it may have been practiced more than 100 centuries ago in what is now China, according to an interpretation of ancient paintings. However, this continues to be debated. The word "ski" comes from the Old Norse word "skíð" which means to "split piece of wood or firewood". Asymmetrical skis were used in northern Finland and Sweden until at least the late 19th century. On one foot, the skier wore a long straight non-arching ski for sliding, and a shorter ski was worn on the other foot for kicking. The underside of the short ski was either plain or covered with animal ...
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Nevis Range
Nevis is a small island in the Caribbean Sea that forms part of the inner arc of the Leeward Islands chain of the West Indies. Nevis and the neighbouring island of Saint Kitts constitute one country: the Federation of Saint Kitts and Nevis. Nevis is located near the northern end of the Lesser Antilles archipelago, about east-southeast of Puerto Rico and west of Antigua. Its area is and the capital is Charlestown. Saint Kitts and Nevis are separated by a shallow channel known as "The Narrows". Nevis is roughly conical in shape, with a volcano known as Nevis Peak at its centre. The island is fringed on its western and northern coastlines by sandy beaches composed of a mixture of white coral sand with brown and black sand eroded and washed down from the volcanic rocks that make up the island. The gently-sloping coastal plain ( wide) has natural freshwater springs as well as non-potable volcanic hot springs, especially along the western coast. The island was named ''O ...
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Gondola Lift
A gondola lift is a means of cable transport and type of aerial lift which is supported and propelled by cables from above. It consists of a loop of steel wire rope that is strung between two stations, sometimes over intermediate supporting towers. The cable is driven by a bullwheel in a terminal, which is typically connected to an engine or electric motor. It is often considered a ''continuous system'' since it features a haul rope which continuously moves and circulates around two terminal stations. In contrast, an aerial tramway operates solely with fixed grips and simply shuttles back and forth between two end terminals. The capacity, cost, and functionality of a gondola lift will differ dramatically depending on the combination of cables used for support and haulage and the type of grip (detachable or fixed). Because of the proliferation of such systems in the Alps, the it, Cabinovia and french: Télécabine are also used in English-language texts. The systems m ...
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Bealach
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap, saddle, col or notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pass. Passes are often found just above the source of a river, const ...
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