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]   |
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Ben More Assynt
Ben More Assynt () is a mountain in Assynt in the far northwest 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 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 main north–south watershed ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 4,411 ft (1,345 m). 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 (reference date), epoch event of modern peak bagging. The list has been the subject of subsequent variation and , the Scottish Mountaineering Club has listed 282 Munros and 226 Munro Tops. "Munro bagging" is the activity of climbing all the listed Munros. , 7,654 people had rep ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Preposition
Adpositions are a part of speech, class of words used to express spatial or temporal relations (''in, under, towards, behind, ago'', etc.) or mark various thematic relations, semantic roles (''of, for''). The most common adpositions are prepositions (which precede their complement) and postpositions (which follow their complement). An adposition typically combines with a noun phrase, this being called its complement (grammar), complement, or sometimes object (grammar), object. English language, 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 (like Turkic languages) or have both types (like Finnish language, Finnish). The phrase form ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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River Oykel
The River Oykel ( 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, Scotland, Ross (parish of Kincardine (Ardgay and District), Kincardine) to the south and Sutherland (parish of Creich, Sutherland, Creich) to the north. Etymology The name ''Oykel'' is of uncertain derivation, but may be of Pictish language, Pictish origin. Firstly, this and other similar hydronyms may involve the element ''og'', meaning "lively" (cf. 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 language, Welsh ''uchel'' has been suggested, but judged unlikely. Geography The riv ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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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]   |
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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since mountain ranges can present 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 minimum high point between two valleys and the lowest point along a ridge. On a topographic map, passes can be identified 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 o ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 N ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Frog Orchid
''Dactylorhiza viridis'', the frog orchid, is a species of flowering plant in the orchid family Orchidaceae. It has also been treated as the only species ''Coeloglossum viride'' of the monotypic genus ''Coeloglossum''. Description The plant arises from fleshy, forked roots and ranges in height from 10 to 55 cm. The leaves of ''D. viridis'' are 5–14 cm long and 2–7 cm wide; leaves at the base of the orchid are obovate to elliptical, while leaves higher on the stem become lanceolate. Two to six leaves are found on one plant, and leafing is alternate. The inflorescence of the orchid is a dense raceme (spike-like cluster) containing 7 to 70 small flowers. Flowers are greenish in color, and often tinged with purple, reddish, or red-brown color. The flowers are subtended by conspicuous long, tapering bracts which are 1–6 cm long, with the lower bracts longer and typically greatly exceeding the length of the flower. The sepals are oval with little or no ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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North West Highlands Geopark
The North West Highlands Geopark is a International Network of Geoparks, geopark in the Scottish Highlands. Awarded UNESCO geopark status in 2004, it was Scotland's first geopark, featuring some of the oldest rock (geology), 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 Supergroup, Moine rocks w ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |