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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 south west 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 hil ... [...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, in the district of Richmondshire 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. 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 service café for visitors in the village’s Public Hall. Keld’s Youth Hostel closed in 2008 and has ... [...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 ... [...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. Approximately 300 fungi are known to be pathogenic to humans. Markedly more fungi are known to be pathogenic to plant life than those of the animal kingdom. The study of fu ... 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 i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Britain
Great Britain is an island in the North Atlantic Ocean off the northwest coast of continental Europe. With an area of , it is the largest of the British Isles, the largest European island and the ninth-largest island in the world. It is dominated by a maritime climate with narrow temperature differences between seasons. The 60% smaller island of Ireland is to the west—these islands, along with over 1,000 smaller surrounding islands and named substantial rocks, form the British Isles archipelago. Connected to mainland Europe until 9,000 years ago by a landbridge now known as Doggerland, Great Britain has been inhabited by modern humans for around 30,000 years. In 2011, it had a population of about , making it the world's third-most-populous island after Java in Indonesia and Honshu in Japan. The term "Great Britain" is often used to refer to England, Scotland and Wales, including their component adjoining islands. Great Britain and Northern Ireland now constitute the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal Measure
In lithostratigraphy, the coal measures are the coal-bearing part of the Upper Carboniferous System. In the United Kingdom, the Coal Measures Group consists of the Upper Coal Measures Formation, the Middle Coal Measures Formation and the Lower Coal Measures Formation. The group records the deposition of fluvio-deltaic sediments which consists mainly of clastic rocks (claystones, shales, siltstones, sandstones, conglomerates) interstratified with the beds of coal. In most places, the coal measures are underlain by coarser clastic sequences known as Millstone Grit, of Namurian age. The top of the coal measures may be marked by an unconformity, the overlying rocks being Permian or later in age. In some parts of Britain, however, the coal measures grade up into mainly coal-barren red beds of late Westphalian and possibly Stephanian age. Within the Pennine Basin these barren measures are now referred to as the Warwickshire Group, from the district where they achieve their thickest dev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Ure
The River Ure in North Yorkshire, England is approximately 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 the 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'', becaus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Birkdale, North Yorkshire
Birkdale 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 Beck flows through the dale. At the eastern end of the dale the beck joins Great Sleddale Beck to become the River Swale The River Swale in Yorkshire, England, is a major tributary of the River Ure, which becomes the 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. Th .... Valleys of North Yorkshire Yorkshire Dales {{Richmondshire-geo-stub ... [...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, 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 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. in the lower waters over a drop of 14 ... [...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 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 other ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
