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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 language as ''“White Mountain”''. 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 rocks ... [...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 language as ''“White Mountain”''. 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 rocks ... [...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'', 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 of Canisp (Scottish Gaelic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Assynt
Assynt ( gd, Asainn 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 ... [...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 [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suilven
Suilven ( gd, Sùilebheinn) is a 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. 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 and many other mountains in Northwest Scotland as nunataks, but cosmogenic isotope dating of mountaintop erratics has since disproved this hypothesis. The ... [...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. These rocks are of Archaean and Paleoproterozoic age, ranging from 3.0–1.7 billion years ( Ga). They form the basement on which the Torridonian and Moine Supergroup sediments were deposited. The Lewisian consists mainly of 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 Lewis, from which the complex takes its name. It is also exposed on several islands of the Inner Hebrides, small islands north of the Scottish mainland and forms a coastal strip on the mainland from ... [...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 British Isle mountain and hill classifications. By definition, P600s have a height above , the requirement to be called a "mountain" in the British Isles. The "P" terminology is an international classification, along with P1500 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 282 Scottish Munros, and 10 of the 34 Non-Scottish Munros (or Furths), all of which have prominences above , and are sometimes called the "Super-Majors". The list also contained the highest mountains in Scotland, Wales, Ireland, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunatak
A nunatak (from Inuit language, Inuit ''nunataq'') 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 are also called glacial islands. Examples are natural pyramidal peaks. When rounded by glacial action, smaller rock promontories 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 is typically used in areas where a permanent ice sheet is present and the nunataks protrude 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 nunataks are isolated, sometimes they form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, which hampers the formation of glacial i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sutherland
Sutherland ( gd, Cataibh) is a historic county, registration county and lieutenancy area in the Highlands of Scotland. Its county town is Dornoch. Sutherland borders Caithness and Moray Firth to the east, Ross-shire and Cromartyshire (later combined into Ross and Cromarty) to the south and the Atlantic to the north and west. Like its southern neighbour Ross-shire, Sutherland has some of the most dramatic scenery in Europe, especially on its western fringe where the mountains meet the sea. These include high sea cliffs, and very old mountains composed of Precambrian and Cambrian rocks. The name ''Sutherland'' dates from the era of Norwegian Viking rule and settlement over much of the Highlands and Islands, under the rule of the jarl of Orkney. Although it contains some of the northernmost land in the island of Great Britain, it was called ' ("southern land") from the standpoint of Orkney and Caithness. In Gaelic, the area is referred to according to its traditional areas: ' ( ... [...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-Ordovician lim ... [...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 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] |
Marilyn (hill)
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 tha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
