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Canisp
Canisp (Scottish Gaelic: ''Canasp'') is a mountain in the far north west of Scotland. It is situated in the parish of Assynt, in the county of Sutherland, north of the town of Ullapool. Canisp reaches a height of and qualifies as a Corbett and Marilyn hill. The mountain's name translates from the Old Norse ''kambsnípa'' or point of the comb/ridge. Geography and geology Canisp is an isolated mountain that stands in the Glencanisp Forest, a large rock and water wilderness. It has a topographic prominence of . Canisp has little vegetation, even on its lower slopes large areas of Gneiss (one of the oldest rocks in the world) are visible on the surface. Canisp stands in a geologically important area. It is part of the Moine Thrust Belt and is typical of many of the Assynt hills in that it rises from a base of Lewisian Gneiss and is composed of Torridonian sandstone capped by Cambrian quartzite giving the hill a distinctive light grey crown. Canisp was formed when surround ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canisp From The East
Canisp (Scottish Gaelic: ''Canasp'') is a mountain in the far north west of Scotland. It is situated in the parish of Assynt, in the county of Sutherland, north of the town of Ullapool. Canisp reaches a height of and qualifies as a Corbett and Marilyn hill. The mountain's name translates from the Old Norse ''kambsnípa'' or point of the comb/ridge. Geography and geology Canisp is an isolated mountain that stands in the Glencanisp Forest, a large rock and water wilderness. It has a topographic prominence of . Canisp has little vegetation, even on its lower slopes large areas of Gneiss (one of the oldest rocks in the world) are visible on the surface. Canisp stands in a geologically important area. It is part of the Moine Thrust Belt and is typical of many of the Assynt hills in that it rises from a base of Lewisian Gneiss and is composed of Torridonian sandstone capped by Cambrian quartzite giving the hill a distinctive light grey crown. Canisp was formed when surrounding ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Awe, Inchnadamph
Loch Awe is a small loch, located 4 miles south of Loch Assynt and next to the village of Ledmore, within the Assynt area of Sutherland, Scotland. The loch is located in an area along with neighbouring Coigach, as the ''Assynt-Coigach National scenic area (Scotland), National Scenic Area'', one of 40 such areas in Scotland. Cairn Immediately south and west of the loch is a circular cairn at Cnoc Bad Na Cleithe. The first cairn measures 6 to 7 foot high and measures 63 feet on a north–south bearing at the base, by 70 feet. They were surveyed on 11 June 1909 and there is no sign of a cist or chamber. Geography Loch Awe in Sutherland is one of a number of lochs in that area that drain into the Loch Inver and Inver Basin. To the northwest of Loch Awe are smaller lochans that drain into Loch Awe. These are Loch Na Gruagaich and further northeast is Loch Na Saighe Duibhe as well as a small group of lochans, that are unnamed. Overlooking the loch to the north is the imposing bulk o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assynt
Assynt ( or ) is a sparsely populated area in the south-west of Sutherland, lying north of Ullapool on the west coast of Scotland. Assynt is known for its landscape and its remarkable mountains, which have led to the area, along with neighbouring Coigach, being designated as the Assynt-Coigach National Scenic Area, one of 40 such areas in Scotland. The western part of Assynt has many distinctively shaped mountains, including Quinag, Canisp, Suilven and Ben More Assynt, that rise steeply from the surrounding "cnoc and lochan" scenery. These can often appear higher than their actual height would indicate due to their steep sides and the contrast with the moorland from which they rise. Many of the most distinctive peaks such as Suilven were formed during the last Ice Age, when they were left exposed above the ice sheet as nunataks, and they now remain as inselbergs of highly eroded Torridonian sandstone sitting on a bedrock of much older Lewisian gneiss. The Moine Thrust ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conival
Conival (Scottish Gaelic: ''Cona Mheall'') is a Scottish mountain situated in Assynt in the Sutherland area of the Highland Council Area, north-northeast of Ullapool. Overview Conival is a distinct landmark when viewed from the A837 road to the west from where its conspicuous western face is well seen; this flank is made up of light coloured and distinctive Cambrian quartzite rock thickened by geological thrusting.University of Leeds Geology Site. Describes western face. The mountain reaches a height of 987 metres (3,238 feet) and is classified as a . It is connected to the adjoining and better known Munro of |
Suilven
Suilven is a Graham mountain in Scotland. Lying in a remote area in the west of Sutherland, it rises from a wilderness landscape of moorland, bogs and lochans known as Inverpolly National Nature Reserve. Suilven forms a steep-sided ridge some in length. The highest point, Caisteal Liath ("Grey Castle" in Scottish Gaelic), lies at the northwest end of this ridge. There are two other summits: Meall Meadhonach ("Middle Round Hill") at the central point of the ridge is high, whilst Meall Beag ("Little Round Hill") lies at the southeastern end. Name The name is Viking in origin, coming from the Old Norse ''súla fjell'', meaning "pillar mountain" (with the later substitution of Gaelic ''bheinn'' for ''fjell''). Geology Geologically, Suilven is formed of Torridonian sandstone, sitting on a landscape of Lewisian gneiss. The surrounding rocks were eroded during an episode of glaciation. Suilven was covered by the last British and Irish Ice Sheet. Prior research described Suilven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lewisian Complex
The Lewisian complex or Lewisian gneiss is a suite of Precambrian metamorphic rocks that outcrop in the northwestern part of Scotland, forming part of the Hebridean terrane and the North Atlantic craton, North Atlantic Craton. These rocks are of Archean, Archaean and Paleoproterozoic age, ranging from 3.0–1.7 billion years (Year#SI prefix multipliers, Ga). They form the Basement (geology), basement on which the Stoer Group, Wester Ross Supergroup and probably the Loch Ness Supergroup sediments were deposited. The Lewisian consists mainly of Granite, granitic gneisses with a minor amount of supracrustal rocks. Rocks of the Lewisian complex were caught up in the Caledonian orogeny, appearing in the hanging walls of many of the thrust faults formed during the late stages of this tectonic event. Distribution The main outcrops of the Lewisian complex are on the islands of the Outer Hebrides, including Isle of Lewis, Lewis, from which the complex takes its name. It is also exp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of The British Isles By Relative Height
This is a list of P600 mountains in Britain and Ireland by height. A P600 is defined as a mountain with a topographic prominence above , regardless of elevation or any other merits (e.g. topographic isolation); this is a similar approach to that of the Marilyn, Simms, HuMP and TuMP Lists of mountains and hills in the British Isles, British Isle mountain and hill classifications. By definition, P600s have a height above , the requirement to be called a Lists of mountains and hills in the British Isles#Elevation, "mountain" in the British Isles. The "P" terminology is an international classification, along with P1500 Ultra-prominent peak, Ultras. P600 and "Majors" are used interchangeably. , there were 120 P600s in the British Isles: 81 in Scotland, 25 in Ireland, 8 in Wales, 4 in England, 1 in Northern Ireland, and 1 in the Isle of Man. The 120 P600s contained 54 of the List of Munro mountains in Scotland, 282 Scottish Munros, and 10 of the List of Furth mountains in the Brit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunatak
A nunatak (from Inuit language, Inuit ) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also called glacial islands, and smaller nunataks rounded by glacial action may be referred to as rognons. The word is of Greenlandic language, Greenlandic origin and has been used in English since the 1870s. Description The term ''nunatak'' is typically used in areas where a permanent ice sheet is present and the ridge protrudes above the sheet.J. J. Zeeberg, ''Climate and Glacial History of the Novaya Zemlya Archipelago, Russian Arctic''. pp. 82–84 Nunataks present readily identifiable landmark reference points in glaciers or ice caps and are often named. While some are isolated, they can also form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, hampering the formation of glacial ice on thei ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sutherland
Sutherland () is a Counties of Scotland, historic county, registration county and lieutenancy areas of Scotland, lieutenancy area in the Scottish Highlands, Highlands of Scotland. The name dates from the Scandinavian Scotland, Viking era when the area was ruled by the Jarl of Orkney; although Sutherland includes some of the northernmost land on the island of Great Britain, it was called ' ("southern land") from the standpoint of Orkney and Caithness. From the 13th century, Sutherland was a provincial lordship, being an earldom controlled by the Earl of Sutherland. The earldom just covered the south-eastern part of the later county. A Shires of Scotland, shire called Sutherland was created in 1633, covering the earldom of Sutherland and the neighbouring provinces of Assynt to the west and Strathnaver to the north. Shires gradually eclipsed the old provinces in administrative importance, and also become known as counties. The county is generally rural and sparsely populated. Suth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northwest Highlands
The Northwest Highlands are located in the northern third of Scotland that is separated from the Grampian Mountains by the Great Glen (Glen More). The region comprises Wester Ross, Assynt, Sutherland and part of Caithness. The Caledonian Canal, which extends from Loch Linnhe in the south-west, via Loch Ness to the Moray Firth in the north-east splits this area from the rest of the country. The city of Inverness and the town of Fort William serve as gateways to the region from the south. Geology The geology of the Highlands is complex. Along the western coastal margin it is characterised by Lewisian gneiss, the oldest rock in Scotland. Liathach, Beinn Alligin, Suilven, Cùl Mòr, Cùl Beag, and Quinag are just some of the impressive rock islands of the significantly younger rich brown-coloured Torridonian sandstone which rests on the gneiss. Some of the peaks, such as Beinn Eighe and Canisp, are topped with later light grey or white Cambrian quartzite. Cambro-Ord ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Corbetts
This is a list of Corbett mountains in Scotland by height. Corbetts are defined as Scottish mountains between in height with a prominence of at least ; 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 (''i.e.'' below the elevation threshold of ), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyn (hill)
This is a list of Marilyn hills and mountains in the United Kingdom, Republic of Ireland, Ireland and surrounding islands and Stack (geology), sea stacks. Lists of mountains and hills in the British Isles#Marilyns, Marilyns are defined as peaks with a topographic prominence, prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Lists of mountains and hills in the British Isles#Munros, 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 homophone, homophonous with (Marilyn) ''Marilyn Monroe, Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
