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Dale (landform)
A dale is an open valley. ''Dale'' is a synonym of the word ''valley''. The name is used when describing the physical geography of an area. It is used most frequently in the Lowlands of Scotland and in the North of England; the term "fell" commonly refers to the mountains or hills that flank the dale. Etymology The word ''dale'' comes from the Old English word ''dæl'', from which the word " dell" is also derived. It is also related to Old Norse word ''dalr'' (and the modern Icelandic word ''dalur''), which may perhaps have influenced its survival in northern England. The Germanic origin is assumed to be *''dala-''. ''Dal-'' in various combinations is common in placenames in Norway. Modern English valley and French vallée are presumably not related to dale. A distant relative of ''dale'' is currency unit dollar, stemming from German ''thaler'' or ''daler'', short for joachimsthaler coins manufactured in the town of Joachimsthal in Bohemia.Falk, Hjalmar (1991). ''Etymologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eskdale, North Yorkshire
Eskdale is a valley running west to east from Westerdale on the North York Moors to Whitby on the Yorkshire Coast of England. Formed during the last major ice age, it has a classic U-shaped valley formation caused by the action of glaciers carving away the rock. Eskdale is named after its river which in Celtic means water or stream. The dale carries the River Esk from the "Esklets" above Westerdale to the sea at Whitby. The tops of its steep-sided valleys are noted for their heather moorland, whilst below the land is mainly split between pasture for cows and Swaledale sheep and arable crops such as Oil seed rape. The Esk Valley Walk is a walk covering starting from the head of the Esk through the valley and down to Whitby. Eskdale School in Whitby is named after the valley. The Esk Valley Line runs through Eskdale from Commondale eastwards towards Whitby and is named after the dale. The river flows through the narrow valley that the water has cut into the soft shale of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eskdale, Dumfries And Galloway
Eskdale ( gd, Eisgeadal, IPA: ˆeʃkʲət̪əɫ̪ is a glen and former lordship in the county of Dumfriesshire, Scotland. The River Esk flows through Eskdale to its estuary at the Solway Firth The Solway Firth ( gd, Trà chd Romhra) is a firth that forms part of the border between England and Scotland, between Cumbria (including the Solway Plain) and Dumfries and Galloway. It stretches from St Bees Head, just south of Whitehaven in .... In 1620, when 13 continuous days of snow occurred in Scotland, on Eskdale Moor only 35 of a flock of 20,000 sheep survived. Sources Glens of Scotland Landforms of Dumfries and Galloway Annandale and Eskdale {{DumfriesGalloway-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eskdale, Cumbria
Eskdale is a glacial valley and civil parish in the western Lake District National Park in Cumbria, England. It forms part of the Borough of Copeland, and in 2001 had a population of 264, increasing to 304 at the 2011 Census. One of the Lake District's most popular tourist attractions, the Ravenglass and Eskdale Railway, runs through the valley, though along with other western valleys of the Lake District, Eskdale is notably quieter during the high summer season than the more accessible eastern areas. Topography The River Esk flows through the valley to its estuary at Ravenglass. The valley is notable in being one of few major valleys in the Lake District not to have its own lake, although several tarns are perched above the valley sides. The main access to the valley is from the western end; however, there is also a steep pass with a motor road leading out of the valley to the east over Hardknott Pass, as well as a road with beautiful views leading southwards over Birker ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coquetdale
The River Coquet runs through the county of Northumberland, England, discharging into the North Sea on the east coast at Amble. It rises in the Cheviot Hills on the border between England and Scotland, and follows a winding course across the landscape ("Coquetdale"). The upper reaches are bordered by the Otterburn Training Area, Otterburn Ranges military training ground, and are crossed by a number of bridges built in the 20th century. It passes a number of small villages and hamlets, and feeds one of the lakes created by extraction of gravel that form the Caistron Nature Reserve, before reaching the town of Rothbury, where it is crossed by a grade II listed bridge. Below the town is Thrum Mill, Rothbury, Northumberland, Thrum Mill, the restoration of which was featured on Channel 4 television. It loops around Brinkburn Priory, founded in the 1130s for Augustinians, Augustinian Canons, and its associated mill. At Felton, Northumberland, Felton it is crossed by two bridges, one ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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