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Howgills
The Howgill Fells are uplands in Northern England between the Lake District and the Yorkshire Dales, lying roughly within a triangle formed by the town of Sedbergh and the villages of Ravenstonedale and Tebay.The Howgill Fells in Cumbria ''www.visitcumbria.com'' The name Howgill derives from the word ''haugr'' meaning a hill or barrow, plus ''gil'' meaning a narrow valley. Geography The Howgill Fells are bounded by the (and the |
The Calf
The Calf, at an elevation of , is the highest point in the Howgill Fells, an area of high ground in north-west England. It is in the north-west of the Yorkshire Dales in Westmorland and Furness in the county of Cumbria (historically it was on the West Riding of Yorkshire/Westmorland boundary). It can be ascended from the town of Sedbergh to the south, by way of Cautley Spout from the east, or up the long valley of Langdale from the north. The Sedbergh ascent is the most popular, and has the distinction of being on good paths all the way. The summit commands an extensive panorama, although foreground detail is obscured by the extreme flatness of the plateau. A twenty-mile skyline of the Lakeland peaks can be seen, as well as the Yorkshire Three Peaks and many of the nearer Howgill Fells. Alfred Wainwright, in his ''Walks on the Howgill Fells'', describes a route from Sedbergh to Calders and The Calf as "the classic high-level walk on the Howgill Fells". He includes a drawing of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tranearth Group
The Tranearth Group is a Silurian lithostratigraphic group (a sequence of rock strata) in the southern Lake District and Howgill Fells of the Pennines of northern England. The name is derived from the locality of Tranearth near Torver in Cumbria. The Group is included within the Windermere Supergroup. It comprises laminated hemipelagites and siltstones and some sandstones and 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) ... which achieve a thickness of between . It is divided into a lower Brathay Formation which is overlain by the Birk Riggs Formation (not present in the Howgills) and then by an upper Coldwell Formation. References * {{Refend Silurian System of Europe Geology of England Geological groups of the United Kingdom Geologic formations of the United ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Raisbeck
Raisbeck is a hamlet in the civil parish of Orton, in the Westmorland and Furness district of Cumbria, England. The surname Raisbeck originates from the hamlet. The name of the hamlet derives from Hrridarr, a personal name and beck, a stream or river. There is also the smaller hamlet of Sunbiggin nearby. Circa 1870, it had a population of 214 as recorded in the Imperial Gazetteer of England and Wales The ''Imperial Gazetteer of England and Wales'' is a substantial topographical dictionary first published between 1870 and 1872, edited by the Reverend John Marius Wilson. It contains a detailed description of England and Wales. Its six volumes h .... Northwest of the hamlet is the Gamelands stone circle.Aubrey Burl (2005) ''A Guide to the Stone Circles of Britain, Ireland and Brittany'', page 80. See also * Listed buildings in Orton, Westmorland and Furness References External links Cumbria County History Trust: Orton(nb: provisional research only – see Talk p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yorkshire
Yorkshire ( ) is an area of Northern England which was History of Yorkshire, historically a county. Despite no longer being used for administration, Yorkshire retains a strong regional identity. The county was named after its county town, the city of York. The south-west of Yorkshire is densely populated, and includes the cities of Leeds, Sheffield, Bradford, Doncaster and Wakefield. The north and east of the county are more sparsely populated, however the north-east includes the southern part of the Teesside conurbation, and the port city of Kingston upon Hull is located in the south-east. York is located near the centre of the county. Yorkshire has a Yorkshire Coast, coastline to the North Sea to the east. The North York Moors occupy the north-east of the county, and the centre contains the Vale of Mowbray in the north and the Vale of York in the south. The west contains part of the Pennines, which form the Yorkshire Dales in the north-west. The county was historically borde ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stockdale Group
The Stockdale Group is a Silurian lithostratigraphic group (a sequence of rock strata) in the southern Lake District and Howgill Fells of the Pennines of northern England. The name is derived from the locality of Stockdale near the top of Longsleddale in Cumbria. It is included within the Windermere Supergroup. The rocks of the Group have also previously been referred to as the Stockdale Shales or Stockdale Subgroup. The group comprises limestones and oolites and some sandstones and shale Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of Clay mineral, clay minerals (hydrous aluminium phyllosilicates, e.g., Kaolinite, kaolin, aluminium, Al2Silicon, Si2Oxygen, O5(hydroxide, OH)4) and tiny f ...s which reach a maximum thickness of 120m in the area. It is divided into a lower Skelgill Formation which is overlain by an upper Browgill Formation. References * {{Refend Silurian System of Europe Geology of England Geological groups of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dent Group
The Dent Group is a group of Upper Ordovician sedimentary and volcanic rocks in north-west England. It is the lowermost part of the Windermere Supergroup, which was deposited in the foreland basin formed during the collision between Laurentia and Avalonia. It lies unconformably on the Borrowdale Volcanic Group. This unit was previously known as the Coniston Limestone Group or Coniston Limestone Formation and should not be confused with the significantly younger (uppermost Silurian) Coniston Group. Distribution The Dent Group is exposed in four areas, the southern Lake District as a narrow strip across the whole width of the outcrop, in the Cautley and Dent inliers, the Cross Fell inlier and the Craven inliers. Lake District outcrop In the main Lake District outcrop, the group consists of calcareous siltstones and mudstones of the basal Kirkley Bank Formation, micritic limestones of the Broughton Moor Formation and dark blue-gray shales of the Ashgill Formation. Locally volca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashgill (age)
The Ordovician ( ) is a geologic period and system, the second of six periods of the Paleozoic Era, and the second of twelve periods of the Phanerozoic Eon. The Ordovician spans 41.6 million years from the end of the Cambrian Period Ma (million years ago) to the start of the Silurian Period Ma. The Ordovician, named after the Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Geological Congress. Life continued to flourish du ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inliers And Outliers (geology)
An inlier is an area of older rocks surrounded by younger rocks. Inliers are typically formed by the erosion of overlying younger rocks to reveal a limited exposure of the older underlying rocks. Faulting or folding may also contribute to the observed outcrop pattern. A classic example from Great Britain is that of the inlier of folded Ordovician and Silurian rocks at Horton in Ribblesdale in North Yorkshire which are surrounded by the younger flat-lying Carboniferous Limestone. The location has long been visited by geology students and experts. Another example from South Wales is the Usk Inlier in Monmouthshire where Silurian age rocks are upfolded amidst Old Red Sandstone rocks of Devonian age. A similar outcrop pattern which results from movement on a thrust fault followed by erosion may be termed a window. Conversely an outlier is an area of younger rock surrounded by older rocks. An outlier is typically formed when sufficient erosion of surrounding rocks has taken plac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeozoic
The Paleozoic ( , , ; or Palaeozoic) Era is the first of three geological eras of the Phanerozoic Eon. Beginning 538.8 million years ago (Ma), it succeeds the Neoproterozoic (the last era of the Proterozoic Eon) and ends 251.9 Ma at the start of the Mesozoic Era. The Paleozoic is subdivided into six geologic periods (from oldest to youngest), Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Some geological timescales divide the Paleozoic informally into early and late sub-eras: the Early Paleozoic consisting of the Cambrian, Ordovician and Silurian; the Late Paleozoic consisting of the Devonian, Carboniferous and Permian. The name ''Paleozoic'' was first used by Adam Sedgwick (1785–1873) in 1838 to describe the Cambrian and Ordovician periods. It was redefined by John Phillips (1800–1874) in 1840 to cover the Cambrian to Permian periods. It is derived from the Greek ''palaiós'' (παλαιός, "old") and ''zōḗ'' (ζωή, "life") meaning "ancient l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orton Fells
The Orton Fells is an upland area in Northern England, mostly consisting of limestone hills, plateaus and moorlands. Historically in Westmorland, the area lies within the modern county of Cumbria and is bounded by the Lake District to the west, the Eden Valley to the north and east, and the Yorkshire Dales and Howgill Fells to the south. The area mostly falls within the boundaries of the Yorkshire Dales National Park while a small part of the western fells is in the Lake District National Park. The fells are one of 159 National Character Areas defined by Natural England. Most settlements are in the lower land of the central upland region and the area is bounded by the villages of Orton, Great Asby, Little Asby, Crosby Ravensworth and Crosby Garret. Other settlements in the area include Ravenstonedale, Soulby, Maulds Meaburn, King's Meaburn, Morland, and Cliburn, and many of the settlements have conservation area status. Abrasion by glaciers and natural weathering of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
