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Slioch From Loch Maree
, photo = Slioch_from_Loch_Maree.jpg , photo_caption = Slioch seen from the shores of Loch Maree. , elevation_m = 981 , elevation_ref = , prominence_m = 626 , prominence_ref = , parent_peak = Sgurr Mor , listing = Munro, Marilyn , translation = the spear , language = Gaelic , pronunciation = , location = Wester Ross, Scotland , range = , grid_ref_UK = NH004688 , topo = OS ''Landranger'' 19, OS ''Explorers'' 433, 435 , first_ascent = , easiest_route = Slioch ( gd, Sleaghach) is a mountain in the Scottish Highlands situated in Wester Ross, eight kilometres north of the village of Kinlochewe. Slioch reaches a height of 981 metres (3218 feet) and towers above the south east end of Loch Maree to give one of the best known and most photographed sights (from the A832 road) in the Highlands. VisitScotland, the Scottish national tourist agency, has used video footage of Slioch in its television advertisements. The mountain is composed of Torridonian sands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drumblade
Drumblade is a hamlet in north-western Aberdeenshire, Scotland, which lies 4¾ miles east of the town of Huntly. Schools Drumblade Primary School is a primary school with a nursery unit, and a total roll of 53 as of 2013. It is a feeder school for The Gordon Schools, Huntly. It made the national news in 2012 when its pet ducks disappeared, presumed stolen. History Drumblade Stone Circle, or Ston(e)yfield, is the remains of an ancient stone circle. It is about east of Huntly. Drumblade is the site of the Battle of Slioch in December 1307, involving Robert the Bruce. Notable residents *William Garden Blaikie minister, later Free Church moderator *George Ramsay Davidson George Ramsay Davidson (1801–1890) was a Scottish minister in the 19th century who was senior minister of the influential Lady Glenorchy's Church and Lady Glenorchy's Free Church. Life He was born in Brechin in 1801 the son of David D ... minister of Drumblade from 1828 to 1842 References Ham ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Torridonian
In geology, the term Torridonian is the informal name for the Torridonian Group, a series of Mesoproterozoic to Neoproterozoic arenaceous and argillaceous sedimentary rocks, which occur extensively in the Northwest Highlands of Scotland. The strata of the Torridonian Group are particularly well exposed in the district of upper Loch Torridon, a circumstance which suggested the name Torridon Sandstone, first applied to these rocks by James Nicol. Stratigraphically, they lie unconformably on gneisses of the Lewisian complex and their outcrop extent is restricted to the Hebridean Terrane. Rock type The rocks are mainly red and brown sandstones, arkoses 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 surface the Torridonian strata ... [...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 repo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ken Wilson (mountaineering Writer)
Kenneth John Wilson (7 February 1941 – 11 June 2016) was a British writer, publisher and editor of books and magazines about climbing and mountaineering. The British Mountaineering Council's ''Summit Magazine'' described him as "one of the most influential voices in British climbing". In 1974 he edited and contributed to the first editions of the book ''Hard Rock'' which ''The Guardian'' considered was "among the most influential climbing books of the 20th century." Early life Wilson was born in Solihull to Blanche (née Colman) and John Wilson, a salesman of stationery. He attended Birmingham College of Art where he studied architecture and photography before working for the architectural photographer Henk Snoek for four years in London. During this time he met his future wife Gloria – they married in 1971 and had two children. Based on his experience from the early 1950s with a holiday in the Lake District and with climbing and walking with the scouts, in 1968 he took u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Torridon Hills
The Torridon Hills surround Torridon village in the Northwest Highlands of Scotland. The name is usually applied to the mountains to the north of Glen Torridon. They are among the most dramatic and spectacular peaks in the British Isles and made of some of the oldest rocks in the world. Many are over 3000 feet high, so are considered Munros. Rock types These are mainly made of a type of sandstone, known as Torridonian sandstone (see Geology of Great Britain), which over time has become eroded to produce the unique characteristics of the Torridon Hills. In geology, Torridonian describes a series of proterozoic arenaceous sedimentary rocks of Precambrian age. They are amongst the oldest rocks in Britain, and sit on yet older rocks, Lewisian gneiss. Some of the highest peaks, such as Beinn Eighe are crowned by white Cambrian quartzite, which gives those peaks a distinctive appearance. Some of the quartzite contains fossilized worm burrows and known as pipe rock. It is circ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dundonnell And Fisherfield Forest
Fisherfield Forest The Dundonnell and Fisherfield Forest covers a large mountainous area of Wester Ross in the Northwest Highlands of Scotland, lying between Loch Maree and Little Loch Broom. It is sometimes nicknamed ''The Great Wilderness'', as the area is entirely devoid of permanent settlements. Although termed a ''forest'' the area has very few trees. It is in fact a deer forest; an area maintained by the owners primarily for deer stalking. Three estates cover the principal area of the forest. Dundonnell Estate (134 km2) covers the northwest part of the forest, including the northwestern flanks of An Teallach, whilst Eilean Darach estate covers 262 km2 in the northeast, including the northeast flank of An Teallach. The majority of the area, including all the southern and central sections, forms the 323 km2 Letterewe estate. Mountains Three of the most famous mountains in the area are An Teallach, which lies to the southwest of Dundonnell, A' Mhai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trig Point
A triangulation station, also known as a trigonometrical point, and sometimes informally as a trig, is a fixed surveying station, used in geodetic surveying and other surveying projects in its vicinity. The nomenclature varies regionally: they are generally known as trigonometrical stations or triangulation stations in North America, trig points in the United Kingdom, trig pillars in Ireland, trig stations or trig points in Australia and New Zealand, and trig beacons in South Africa. Use The station is usually set up by a government with known coordinates and elevation published. Many stations are located on hilltops for the purposes of visibility. A graven metal plate on the top of a pillar may provide a mounting point for a theodolite or reflector, often using some form of kinematic coupling to ensure reproducible positioning. Trigonometrical stations are grouped together to form a network of triangulation. Positions of all land boundaries, roads, railways, bridges and ot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wild Goat
The wild goat (''Capra aegagrus'') is a wild goat species, inhabiting forests, shrublands and rocky areas ranging from Turkey and the Caucasus in the west to Turkmenistan, Afghanistan and Pakistan in the east. It has been listed as near threatened on the IUCN Red List and is threatened by destruction and degradation of habitat. It is one of the ancestors of the domestic goat (''C. hircus''). Taxonomy ''Capra aegagrus'' was the scientific name proposed by Johann Christian Polycarp Erxleben in 1777 for the wild goat populations of the Caucasus and Taurus Mountains. ''Capra blythi'' proposed by Allan Octavian Hume in 1874 were wild goat horns from Sindh. The following wild goat subspecies are considered valid taxa: *Bezoar ibex ''C. a. aegagrus'' * Sindh ibex ''C. a. blythi'' * Chiltan ibex ''C. a. chialtanensis'' * Turkmen wild goat ''C. a. turcmenica'' *''Capra aegagrus pictus'' The kri-kri was once thought to be a subspecies of the wild goat, but is now considered to be a ... [...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 ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")