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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] |
Ben More Assynt
Ben More Assynt ( gd, Beinn Mhòr Asaint) is a mountain in Assynt in the far north-west of Scotland, north-northeast of Ullapool. The name translates as "big mountain of Assynt", and with a height of it is the highest point in Sutherland. The mountain lies in the east of Assynt, set apart from the area's better known and more dramatic (but lower) mountains such as Suilven. It is hidden from the traveller on the A837 road by the adjacent Munro of Conival, and the best views of it are obtained from nearby summits. The higher slopes of the mountain are capped by light coloured quartzite boulders, giving it a distinctive appearance. Over of land around Ben More Assynt have been declared a Site of Special Scientific Interest (SSSI) because of their geology, geological interest and rare plant species. Geography Ben More Assynt is situated on a ridge of high ground which runs roughly north to south on the east side of the A837 road near Inchnadamph. This ridge forms part of the ma ... [...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 . 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] |
Preposition
Prepositions and postpositions, together called adpositions (or broadly, in traditional grammar, simply prepositions), are a class of words used to express spatial or temporal relations (''in'', ''under'', ''towards'', ''before'') or mark various semantic roles (''of'', ''for''). A preposition or postposition typically combines with a noun phrase, this being called its complement, or sometimes object. A preposition comes before its complement; a postposition comes after its complement. English generally has prepositions rather than postpositions – words such as ''in'', ''under'' and ''of'' precede their objects, such as ''in England'', ''under the table'', ''of Jane'' – although there are a few exceptions including "ago" and "notwithstanding", as in "three days ago" and "financial limitations notwithstanding". Some languages that use a different word order have postpositions instead, or have both types. The phrase formed by a preposition or postposition together with its comp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Oykel
The River Oykel ( gd, Òiceall or , ) is a major river in northern Scotland that is famous for its salmon fishing. It rises on Ben More Assynt, a few miles from Ullapool on the west coast of Scotland, and drains into the North Sea via the Kyle of Sutherland. Traditionally it has marked the boundary between Ross to the south and Sutherland to the north. Etymology The name ''Oykel'' is of uncertain derivation, but may be of Pictish origin. Firstly, this an other similar hydronyms may involve the element ''og'', meaning "lively" (c.f River Ogwen, Wales), suffixed by the diminutive ''-ell''. Secondly, ''Oykel'' may represent Pictish ''*ogel'' meaning "ridge", although long rivers are rarely named after minor local features. The hypothesis of a derivation from an equivalent of Welsh ''uchel'' has been suggested, but judged unlikely. Geography The river rises at a height of on the southern side of Ben More Assynt, and flows just over . The upper valley is known as Glen Oykel (''Gle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Breabag
Breabag (815 m) is a mountain in the Northwest Highlands of Scotland, in the Assynt area of Sutherland. A flat-topped summit, it is usually climbed from its western flank, where the Bone Caves of Assynt are located. The nearest settlement is Inchnadamph Inchnadamph is a hamlet in Assynt, Sutherland, Scotland. The name is an anglicisation of the Gaelic name Innis nan Damh meaning 'meadow of the stags'. Assynt is a remote area with a low population density. Inchnadamph contains a few houses, a l .... References Mountains and hills of the Northwest Highlands Marilyns of Scotland Corbetts {{Highland-geo-stub ... [...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] |
Mountain Pass
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 migration, 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 (landform), gap, saddle (landform), saddle, col or notch (landform), 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 pas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polystichum Lonchitis
''Polystichum lonchitis'' is a species of fern known by the common name northern hollyfern, or simply holly-fern. It is native to much of the Northern Hemisphere from Eurasia to Alaska to Greenland and south into mountainous central North America. It has stiff, glossy green, erect fronds and grows in moist, shady, rocky mountain habitats. Description This tufted fern produces several erect, linear fronds up to long. In shadier locations fronds may be held horizontally. The fronds are glossy and stiff, pinnate, with many lance-shaped to oblong pinnae (leaflets) up to long, the longest ones occurring near the midpoint of the frond, the basal ones being smaller and triangular in shape. The pinnae overlap each other slightly and are toothed with prominent outward-pointing spines on the margins. The sori are rounded, with a whitish to gray covering (indusium), and are arranged in two rows on the underside of the pinnae. Hitchcock, C.L. and Cronquist, A. 2018. Flora of the Pacific No ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frog Orchid
''Coeloglossum'' is a genus of flowering plants in the orchid family Orchidaceae. It has long been considered to have only one species, ''Coeloglossum viride'', the frog orchid. Some recent classifications regard ''Coeloglossum'' as part of the larger genus, ''Dactylorhiza'', so that ''C. viride'' becomes ''Dactylorhiza viridis''. Other sources continue to keep ''Coeloglossum viride'' separate. Under either name, the species has a wide distribution across the cooler parts of the Northern Hemisphere, covering much of Europe, non-tropical Asia (Russia, Japan, China, the Himalayas, etc.), much of Canada and parts of the United States (Alaska, Northeast, the Appalachians, Great Lakes Region, Northern Great Plains, and Rocky Mountains). It is typically found growing in moist, rich soil in wet meadows, moist or wet deciduous woods and thickets, and is frequently found on steep slopes. Etymology The generic name ''Coeloglossum'' is derived from the Greek ' meaning "hollow tongue ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dryas Octopetala
''Dryas octopetala'', the mountain avens, eightpetal mountain-avens, white dryas or white dryad, is an Arctic–alpine flowering plant in the family Rosaceae. It is a small prostrate evergreen subshrub forming large colonies. The specific epithet ''octopetala'' derives from Greek ''octo'' 'eight' and ''petalon'' 'petal', referring to the eight petals of the flower, an unusual number in the Rosaceae, where five is the normal number. However, flowers with up to 16 petals also occur naturally. As a floral emblem, it is the official territorial flower of the Northwest Territories and the national flower of Iceland. Description The stems are woody, tortuous, with short, horizontal rooting branches. The leaves are glabrous above, densely white-tomentose beneath. The flowers are produced on stalks long, and have eight creamy white petals – hence the specific epithet ''octopetala''. The style is persistent on the fruit with white feathery hairs, functioning as a wind-dispersal agent. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North West Highlands Geopark
The North West Highlands Geopark is a geopark in the Scottish Highlands. Awarded UNESCO geopark status in 2004, it was Scotland's first geopark, featuring some of the oldest rocks in Europe, around 3,000 million years old. The park contains many notable geological features, such as the Moine Thrust Belt and Smoo Cave and covers an area of around . Geography The park is located in the extreme north-west of Scotland and includes parts of Sutherland and Wester Ross, including Cape Wrath. The area is one of the most sparsely inhabited in Europe, and is largely treeless. The park's eastern boundary generally follows the Moine Thrust Belt, otherwise the park is generally bounded by the north and west coasts of Scotland, with a few islands included in the park, such as the Summer Isles. Notable features The Moine Thrust Belt was formed between 430 and 500 million years ago. The belt includes Precambrian Moine rocks which have been pushed on top of younger Cambrian and Ordovician rock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
