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Great Shunner Fell
Great Shunner Fell is the third-highest mountain in the Yorkshire Dales, North Yorkshire, England, and the highest point in Wensleydale; at 716 metres above sea level. In clear weather the summit affords views of Wensleydale to the south, Ribblesdale to the southwest and Swaledale to the north, as well as views into Cumbria and County Durham beyond the A66. The Pennine Way passes over its summit, on the way from Hawes to Keld. The popularity of this route had eroded vegetation from a strip 70 m wide across the moor, which has been alleviated since 1996 by the construction of a path made of flagstones. The summit holds a cross-shaped windbreak of which the triangulation pillar has been built into the northern 'arm'. Great Sleddale Beck, which becomes the River Swale after its confluence with Birkdale Beck, has its sources on the northern slopes of Great Shunner Fell, while the southern slopes drain into the River Ure and Wensleydale. The dominating rock type in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cross Fell
Cross Fell is the highest mountain in the Pennines of Northern England and the highest point in England outside the Lake District. It is located in the North Pennines Area of Outstanding Natural Beauty. It lies within the county of Cumbria and the historic county boundaries of Cumberland. The summit, at , is a stony plateau, part of a ridge running north-west to south-east, which also incorporates Little Dun Fell at and Great Dun Fell at . The three adjoining fells form an escarpment that rises steeply above the Eden Valley on its south-western side and drops off more gently on its north-eastern side towards the South Tyne and Tees Valleys. Cross Fell summit is crowned by a cross-shaped dry-stone shelter. On a clear day there are excellent views from the summit across the Eden Valley to the mountains of the Lake District. On the northern side of Cross Fell there are also fine views across the Solway Firth to the Southern Uplands of Scotland. The fell is prone to dense h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keld, North Yorkshire
Keld is a village in the English county of North Yorkshire. It is in Swaledale, and the Yorkshire Dales National Park. The name derives from the Viking word ''Kelda'' meaning a spring and the village was once called ''Appletre Kelde'' – the spring near the apple trees. From 1974 to 2023 it was part of the district of Richmondshire, it is now administered by the unitary North Yorkshire Council. Keld is the crossing point of the Coast to Coast Walk and the Pennine Way long-distance footpaths at the head of Swaledale, and marks the end of the Swale Trail, a 20 km mountain bike trail which starts in Reeth. At the height of the lead-mining industry in Swaledale in the late 19th century, several notable buildings – now Grade II listed – were erected: they include the Congregational and Methodist chapels, the school and the Literary Institute. A tea room and small shop operate at Park Lodge from Easter to autumn. Out of season, local volunteers provide a self servi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyns Of England
This is a list of Marilyn hills and mountains in the United Kingdom, Ireland and surrounding islands and sea stacks. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,010 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophonous with (Marilyn) ''Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequent British Isles classifications that rely solely on prominence, including the P600s, the HuMPs, and the TuMPs. Topographic prominence is more difficult to estim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Peaks In The Yorkshire Dales
This is a list of the peaks in the Yorkshire Dales. To avoid the list becoming infinitely long and arbitrary, only hills with more than 30 m relative height are included. This includes all Marilyns and Hewitts as well as many other hills. Marilyns are peaks in the British Isles with 150 m of relative height; Hewitts are peaks in England, Ireland and Wales over 2000 ft (610 m) elevation, with at least 30 m relative height. There are 22 Marilyns and 28 Hewitts in the Yorkshire Dales National Park. Topographically, the boundaries of the Yorkshire Dales trace the flow of streams from the lowest points between it and the neighbouring regions of the Lake District, North Pennines, Forest of Bowland, South Pennines and North York Moors. Hills are grouped as topographically as possible, according to their 'parent Marilyn'. The parent Marilyn of hill A can be found by dividing the nearby area into territories, by tracing the runoff from the key col of each Mar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saxifraga Hirculus
''Saxifraga hirculus'' is a species of saxifrage, commonly called marsh saxifrage, yellow marsh saxifrage, or bog saxifrage. It is a perennial herb with yellow flowers and red stem, 5–30 cm high, found on bog landscape. ''Saxifraga hirculus'' is a known food source for the generalist fungus species '' Mycosphaerella tassiana'' and the pathogenic fungus Pathogenic fungi are fungi that cause disease in humans or other organisms. Although fungi are eukaryotic, many pathogenic fungi are microorganisms. Approximately 300 fungi are known to be pathogenic to humans; their study is called "medical mycolo ... species '' Melampsora hirculi''.Helgi Hallgrímsson & Guðríður Gyða Eyjólfsdóttir (2004)''Íslenskt sveppatal I - smásveppir'' [Checklist of Icelandic Fungi I - Microfungi Fjölrit Náttúrufræðistofnunar. Náttúrufræðistofnun Íslands [Icelandic Institute of Natural History]. ISSN 1027-832X References External linksPhoto gallery hirculus Plants described ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Millstone Grit
Millstone Grit is any of a number of coarse-grained sandstones of Carboniferous age which occur in the British Isles. The name derives from its use in earlier times as a source of millstones for use principally in watermills. Geologists refer to the whole suite of rocks that encompass the individual limestone beds and the intervening mudstones as the Millstone Grit Group. The term Millstone Grit Series was formerly used to refer to the rocks now included within the Millstone Grit Group together with the underlying Edale Shale Group. The term gritstone describes any sandstone composed of coarse angular grains, and specifically refers to such sandstones within the Pennines and neighbouring areas of Northern England. Geographical occurrence Rocks assigned to the Millstone Grit Group occur over a wide area of Northern England, where they are a hugely important landscape-forming element of the rock succession. They also occur in parts of northeast Wales and northwest Ireland. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
River Ure
The River Ure in North Yorkshire, England, is about long from its source to the point where it becomes the River Ouse. It is the principal river of Wensleydale, which is the only major dale now named after a village rather than its river. The old name for the valley was Yoredale after the river that runs through it. The Ure is one of many rivers and waterways that drain the Dales into the River Ouse. Tributaries of the Ure include the River Swale and the River Skell. Name The earliest recorded name of the river is in about 1025, probably an error for , where represents the Old English letter wynn or 'w', standing for ("water"). By 1140 it is recorded as ''Jor'', hence Jervaulx (Jorvale) Abbey, and a little later as ''Yore''. In Tudor times, antiquarians John Leland and William Camden used the modern form of the name. The name probably means "the strong or swift river". This is on the assumption that the Brittonic name of the river was ''Isurā'', because the Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Birkdale, North Yorkshire
Birkdale (sometimes written out as Birk Dale) is a dale in the Yorkshire Dales National Park, in North Yorkshire, England. It lies at the far western end of Swaledale, close to the border with Cumbria. The dale is one of the smallest of the Yorkshire Dales. The hamlet of Birkdale is in the lower part of the dale, west of Keld. The area forms part of the civil parish of Muker. Birkdale Tarn is north of the hamlet of Birkdale across the B6270 road at a height of above sea level. The tarn covers and area of and has an average depth of . The tarn has been heavily modified, being a smaller upland lake that was converted into a larger body of water to ensure a constant supply of water for the lead industry in the area. Birkdale Beck flows through the dale draining an upland area of . At the eastern end of the dale the beck joins Great Sleddale Beck to become the River Swale. The dale suffered depopulation in the 1960s (like Grisedale, near to Garsdale Garsdale is a dale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Swale
The River Swale in Yorkshire, England, is a major tributary of the River Ure, which becomes the River Ouse, Yorkshire, River Ouse, that empties into the North Sea via the Humber Estuary. The river gives its name to Swaledale, the valley through which it flows. The river and its valley are home to many types of flora and fauna typical to the Yorkshire Dales. Like similar rivers in the region, the river carves through several types of rock and has features typical of both River erosion, river and glacial erosion. The River Swale has been a contributory factor in the settlements that have been recorded throughout its history. It has provided water to aid in the raising of crops and livestock, but also in the various mining activities that have occurred since Roman times and before. The river is said to be the fastest flowing in England and its levels have been known to rise in 20 minutes. Annual rainfall figures average 1800 mm p.a. in the headwaters and 1300 mm p.a. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triangulation Pillar
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 station is usually set up by a mapping organisation with known coordinates and elevation published. Numerous stations are installed on summits for purposes of visibility and prominence. 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. Use Trigonometrical stations form networks of triangulation. Positions of land boundaries, roads, railways, bridges and other infrastructure can be accurately located by the network, a task essential to the construction of modern infrastructure. Apart from the known stations set up by government, some temporary trigonometrical stations are set up near construction sites for monitoring the precision and progress ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
