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Beinn Damh
Beinn Damh (or ''Ben Damph'') is a Scotland, Scottish mountain situated in the wild mountainous area between Upper Loch Torridon and Glen Carron, 25 kilometres north northeast of Kyle of Lochalsh. Beinn Damh is classed as a List of Corbetts (mountains), Corbett reaching a height of 903 metres (2,962 feet) failing to qualify as a Munro by eleven metres, despite this it is a fine mountain with a four-kilometre-long undulating summit ridge with three tops, it has steep slopes and crags with its eastern face being especially dramatic with huge buttresses and cliffs. The mountain has the conspicuous “Stirrup Mark” just to the south west of the summit, this is a semi circular area of white quartzite surrounded by grey rock which stands out when the mountain is viewed from the south west. The mountain's translated name of “Hill of the Stag” is apt because it stands in the middle of the Ben Damh deer estate. Ascent The ascent of Beinn Damh starts from the Loch Torridon H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maol Cheann-dearg
Maol Cheann-Dearg is a mountain in the Northwest Highlands of Scotland, between Upper Loch Torridon and Loch Carron, in the Coulags deer forest in Wester Ross. It is one of three Munros in this area (the others being Sgorr Ruadh and Beinn Liath Mhòr) and reaches a height of 933 metres (3,060 feet), it is slightly isolated from the other two being separated by a low col of 420 metres and therefore tends to be ascended separately. The mountain is typical of the region in that geologically it is made up of a mixture of sandstone and quartzite, it has a steep flanks and is rock-strewn. The dome shaped summit is littered with red sandstone boulders and lacking in vegetation making its translated name of "red-headed brow" especially appropriate. The mountain is not to be confused with Maol Chinn-dearg, another Munro on the south Glen Shiel ridge. Ascent Maol Cheann-dearg is one of the few Scottish hills which is encircled by good Game stalker, stalkers paths, being located on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Torridon
Torridon (Scottish Gaelic: ''Toirbheartan'') is a small village in the Northwest Highlands of Scotland. However the name is also applied to the area surrounding the village, particularly the Torridon Hills, mountains to the north of Glen Torridon. It lies on the shore of Loch Torridon. Location Torridon is on the west coast of Scotland, north of Fort William and west of Inverness. Situated in an area well known to climbers, photographers, wildlife enthusiasts, hikers, and countless visitors from around the world, the surrounding mountains rise steeply to from the deep sea lochs. There is a large hotel, The Torridon, which holds 3 AA Rosettes as well as 5 red stars and is a leading hotel in the UK, a popular public bar (Bo & Muc), and a youth hostel within walking distance. The Torridon area is widely acknowledged as having some of the most dramatic mountain scenery in the whole of the British Isles. Notable residents * From 1925 until 1931 John McQueen Johnston served as G ... [...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] |
Corbetts
This is a list of Corbett mountains in Scotland by height. Corbetts are defined as Scottish mountains between in height with a prominence over ; solely imperial measurement thresholds. The first list was compiled in the 1920s by John Rooke Corbett, a Bristol-based climber and Scottish Mountaineering Club ("SMC") member, and was published posthumously, after his sister passed it to the SMC, in the 1953 edition of ''Munro's Tables''. Corbetts are the next category down from the Munros and Munro Tops in terms of height (e.g. below the threshold), but their explicit prominence threshold of , ensure they are material peaks. By definition, all Corbetts, given their prominence, are Marilyns. The SMC keeps a list of Corbetts. , there were 222 Corbetts in Scotland. 21 of these 222 Corbetts have a prominence that exceeds the P600 threshold of , which would class them as "Majors". The highest Corbett, Beinn a' Chlaidheimh, at is just below the threshold for a Munro, a status it ... [...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] |
Applecross
Applecross ( gd, A' Chomraich) is a peninsula north-west of Kyle of Lochalsh in the council area of Highland, Scotland. The name Applecross is at least 1,300 years old and is ''not'' used locally to refer to the 19th century village (which is correctly called 'Shore Street', or simply 'The Street') with the Applecross Inn, lying on the Applecross Bay, facing the Inner Sound, on the opposite side of which lies the Inner Hebridean island of Raasay. The monastery of Applecross was established by St Maelrubha, in the 7th century. A sculptured stone is the only remaining relic of Maelrubha, who built a chapel there. The Applecross peninsula ( gd, A' Chomraich, 'The Sanctuary') is a peninsula in Wester Ross, Highland, on the north west coast of Scotland. Geography This row of houses which is often referred to as 'Applecross', and is marked as Applecross on some maps, is actually called 'Shore Street' and is referred to locally just as 'The Street'. The name Applecross applies to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Liathach
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 surfa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beinn Alligin
Beinn Alligin ( gd, Beinn Àilleagan) is one of the classic mountains of the Torridon region of Scotland, lying to the north of Loch Torridon, in the Highlands. The name Beinn Alligin is from the Scottish Gaelic, meaning ''Jewelled Hill''. The mountain has two peaks of Munro status: Tom na Gruagaich () to the south, and Sgùrr Mhòr at to the north. One of the most prominent features of Beinn Alligin is a great cleft known as Eag Dhubh na h-Eigheachd (''black gash of the wailing'') or Leum na Caillich, which cuts into the ridge south of the summit. It is the scar of the most spectacular rockslide or rock avalanche in Britain, which runs out into the corrie of Toll a' Mhadaidh Mor. It occurred around 3750 years ago and is around 3.5 million cubic metres in volume. According to local folklore shepherds on the mountain would hear cries from the gash; those who investigated the source of these cries would inevitably fall to their deaths. Beinn Alligin lies on the National Tru ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scrambling
Scrambling is a mountaineering term for ascending steep terrain using one's hands to assist in holds and balance.''New Oxford American Dictionary''. It is also used to describe terrain that falls between hiking and rock climbing (as a “scramble”). Sure-footedness and a head for heights are essential. Canyoning and stream climbing are other types of scrambling. Overview Scrambling is ascending or traversing a grade without technical apparatus. Unroped ascent in exposed situations is potentially one of the most dangerous of mountaineering activities. As soon as an ascent involves a rope, going up or down, it is no longer a scramble. Alpine scrambling Alpine scrambling is scrambling in high mountains and may not follow a defined or waymarked path. The Seattle Mountaineers climbing organization defines alpine scrambling as follows: Alpine Scrambles are off-trail trips, often on snow or rock, with a 'non-technical' summit as a destination. A non-technical summit is one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch
''Loch'' () is the Scottish Gaelic, Scots language, Scots and Irish language, Irish word for a lake or sea inlet. It is Cognate, cognate with the Manx language, Manx lough, Cornish language, Cornish logh, and one of the Welsh language, Welsh words for lake, llwch. In English English and Hiberno-English, the Anglicisation, anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuary, estuaries, straits or bays. Background This name for a body of water is Insular Celtic languages, Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish language, Irish, Manx language, Manx, and has been borrowed into Scots language, Lowland Scots, Scottish English, Iri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which Erosion, erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
