|
Beinn A' Chuallaich
Beinn a' Chuallaich is a Scottish hill, four kilometres northeast of the village of Kinloch Rannoch in the Perth and Kinross council area. It is part of the high ground between Strath Tummel and Glen Errochty. Overview Beinn a’ Chuallaich is a sizeable and extensive hill which can seem quite inconspicuous when viewed from certain places, especially from the south. This is mainly because of the close proximity of the more eye catching and higher Schiehallion which lies seven km to the SE across Dunalastair Water and dominates Strath Tummel. However Beinn a' Chuallaich is well seen from the head of Glen Errochty where it shows its long NE ridge and its craggy eastern corrie. The hill reaches a height of 892 metres (2926 feet) and qualifies as a Corbett and a Marilyn. Etymology The hill's name translates from the Scottish Gaelic language as “Hill of the Herding” and this refers to the fact that it lies on the route of one of the main north-south ancient drovers' roads ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dunalastair Water
Dunalastair Water (Scottish Gaelic: "Loch Dhùn Alastair") is an entirely man made reservoir in Scotland which lies between Loch Rannoch and Loch Tummel in Strath Tummel in Perth and Kinross council area. The loch provides water power for the Tummel hydroelectricity power station and has the reputation as one of the best wild trout fishing locations in the United Kingdom. Overview Dunalastair Water lies at the approximate grid reference of it has an area of 165 hectares, being 2.5 km long and 800 metres wide at its broadest point. It was formed by the damming of the River Tummel by the Grampian Electric Supply Company in 1933 as part of the Tummel hydro-electric power scheme. The reservoir is narrow at its head, taking the form of a slender wooded glen with the Dunalastair estate situated on the northern bank. The reservoir has roads running on both its northern and southern shores, the B846, which is the road between Pitlochry and Rannoch railway station runs on the north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Victorian Era
In the history of the United Kingdom and the British Empire, the Victorian era was the period of Queen Victoria's reign, from 20 June 1837 until her death on 22 January 1901. The era followed the Georgian period and preceded the Edwardian period, and its later half overlaps with the first part of the '' Belle Époque'' era of Continental Europe. There was a strong religious drive for higher moral standards led by the nonconformist churches, such as the Methodists and the evangelical wing of the established Church of England. Ideologically, the Victorian era witnessed resistance to the rationalism that defined the Georgian period, and an increasing turn towards romanticism and even mysticism in religion, social values, and arts. This era saw a staggering amount of technological innovations that proved key to Britain's power and prosperity. Doctors started moving away from tradition and mysticism towards a science-based approach; medicine advanced thanks to the adoption ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Prominence
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key Saddle point, saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting pat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bothy
A bothy is a basic shelter, usually left unlocked and available for anyone to use free of charge. It was also a term for basic accommodation, usually for gardeners or other workers on an estate. Bothies are found in remote mountainous areas of Scotland, Northern England, Ulster and Wales. They are particularly common in the Scottish Highlands, but related buildings can be found around the world (for example, in the Nordic countries there are wilderness huts). A bothy was also a semi-legal drinking den in the Isle of Lewis. These, such as ''Bothan Eòrapaidh'', were used until recent years as gathering points for local men and were often situated in an old hut or caravan. In Scots law, bothies are defined in law as: a building of no more than two storeys which— (a)does not have any form of— (i)mains electricity, (ii)piped fuel supply, and (iii)piped mains water supply, (b)is 100 metres or more from the nearest public road (within the meaning of section 151 of the Roads (S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crags Under Beinn A Chuallaich
Crag may refer to: * Crag (climbing), a cliff or group of cliffs, in any location, which is or may be suitable for climbing * Crag (dice game), a dice game played with three dice * Crag, Arizona, US * Crag, West Virginia, US * Crag and tail, a geological formation caused by the passage of a glacier over an area of hard rock * Crag Group, a geological group outcropping in East Anglia, UK ** Coralline Crag Formation ** Norwich Crag Formation ** Red Crag Formation ** Wroxham Crag Formation, see Cromer Forest Bed * Crag Hotel, Penang, Malaysia * Crag Jones (born 1962), Welsh climber * USS ''Crag'' (AM-214), a 1943 US Navy ''Admirable''-class minesweeper * The Crag, the final event in the Nickelodeon Guts action sports program * Club de Radioaficionados de Guatemala, an amateur radio organization in Guatemala * Constitutional Reform and Governance Act 2010, concerning United Kingdom constitutional law See also * * Cragg (other) Cragg may refer to: People * Cragg Hines, ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rannoch Moor
Rannoch Moor (, gd, Mòinteach Raineach/Raithneach) is an expanse of around of boggy moorland to the west of Loch Rannoch in Scotland, where it extends from and into westerly Perth and Kinross, northerly Lochaber (in Highland), and the area of Highland Scotland toward its south-west, northern Argyll and Bute. Rannoch Moor is designated a Site of Special Scientific Interest (SSSI) and a Special Area of Conservation. Much of the western part of the moor lies within the Ben Nevis and Glen Coe National Scenic Area, one of 40 such areas in Scotland. It is notable for its wildlife, and is particularly famous as being the sole British location for the Rannoch-rush, named after the moor. It was frequently visited by Horace Donisthorpe who collected many unusual species of ants on the moor and surrounding hilly ground. Today it is still one of the few remaining habitats for ''Formica exsecta'', the "narrow-headed ant", although recent surveys have failed to produce any sign of ''Formi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Truncated Spur
A truncated spur is a spur, which is a ridge that descends towards a valley floor or coastline from a higher elevation, that ends in an inverted-V face and was produced by the erosional truncation of the spur by the action of either streams, waves, or glaciers. Truncated spurs can be found within mountain ranges, along the walls of river valleys, or along coastlines.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Thornbury, W. D., 1954, ''Principles of Geomorphology.'' John Wiley and Sons, Inc. New York. 618 pp. A faceted spur is also a spur that ends in a triangular face, known as a triangular facet, with a broad base and an apex pointing upward. As typically used in geology, the triangular facet is usually a remnant of a fault plane and it and its associated faceted spur are the result of faulting. The term ''faceted spur'' is also applied to inverted-V rock faces ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tummel Hydro-electric Power Scheme
The Tummel hydro-electric power scheme is an interconnected network of dams, power stations, aqueducts and electric power transmission in the Grampian Mountains of Scotland. Roughly bounded by Dalwhinnie in the north, Rannoch Moor in the west and Pitlochry in the east it comprises a water catchment area of around and primary water storage at Loch Ericht, Loch Errochty, Loch Rannoch and Loch Tummel, in Perth and Kinross. Water, depending on where it originates and the path it takes, may pass through as many as five of the schemes nine power stations as it progresses from north-west to south-east. The scheme was constructed in the 1940s and 50s incorporating some earlier sites. It is currently managed by SSE plc. Early Development With a growing need for electricity in the central belt of Scotland individual power stations at Rannoch and Tummel Bridge plus associated dams and infrastructure were constructed in the 1930s for the privately owned Grampian Electric Supply Company. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catchwater
A catchwater device is a large-scale man-made device for catching surface runoff from hills and the sky from precipitation by channeling it to reservoirs for commercial and domestic use later. Freshwater is a scarce natural resource due to pollution, droughts, and overpopulation. Catchwater is a sustainable mechanism to increase freshwater in areas facing droughts or polluted waterways. Types Catchwater drains Catchwater drains may take the form of concrete canals, such as in Hong Kong, where there are many. Alternatively, they may take the form of a large concrete sheet, smothering a hill, and preventing rainfall from entering the rock strata, with a smaller channeling system for transport of the water to the storage tank - this latter system is in operation in Gibraltar. In Hong Kong there are approximately 120 km of concrete channels, used as gutters built along hillsides in order to direct freshwater runoff into reservoirs for local water consumption. These catchwate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tay
The River Tay ( gd, Tatha, ; probably from the conjectured Brythonic ''Tausa'', possibly meaning 'silent one' or 'strong one' or, simply, 'flowing') is the longest river in Scotland and the seventh-longest in Great Britain. The Tay originates in western Scotland on the slopes of Ben Lui ( gd, Beinn Laoigh), then flows easterly across the Highlands, through Loch Dochart, Loch Iubhair and Loch Tay, then continues east through Strathtay (see Strath), in the centre of Scotland, then southeasterly through Perth, where it becomes tidal, to its mouth at the Firth of Tay, south of Dundee. It is the largest river in the British Isles by measured discharge. Its catchment is approximately , the Tweed's is and the Spey's is . The river has given its name to Perth's Tay Street, which runs along its western banks for . Course The Tay drains much of the lower region of the Highlands. It originates on the slopes of Ben Lui (''Beinn Laoigh''), around from the west coast town of Oban, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
