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Gregory Chapel
Gregory Chapel is one of the high points of the fells on the border between Cumbria and North Yorkshire. The summit is marked by a nearby sheep shelter and an unusual and conspicuous cairn - taller and more rectangular than most others locally. (This may, perhaps, be the origin of the curious name "chapel"?) The main rock in the area is limestone, with Millstone Grit outcrops on the tops. There are fine views over to Wild Boar Fell and Swarth Fell 5 km to the west, across the dale of Mallerstang. Hill walkers seem to prefer to give it the name ''Archy Styrigg''; although Ordnance Survey maps show this name along the small plateau at about 680 m elevation to the southwest of the summit, leading over Mallerstang Edge. (This would fit the Norse name, characteristic of this area: ''sty'' = track or path, ''rigg'' = ridge: i.e. path along a ridge). It is classified as a Nuttall and sub-Hewitt, but it has a relatively small prominence, having several other high points nearb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Swarth Fell
Swarth Fell is an approximately 1 mile (1.5 km) stretch of high ground (consisting mainly of limestone capped with millstone grit) situated to the south of Wild Boar Fell, of which it is a continuation. It is mostly within Mallerstang, Cumbria, but the boundary between Cumbria and North Yorkshire (historically Westmorland and the West Riding of Yorkshire) runs along its length, just to the west of the highest points. The summit, (681m, 2234 ft) which is marked by a cairn, and is listed as both a Hewitt and a Nuttall, lies 2.1 km to the south of the summit of Wild Boar Fell, the two fells being separated by a col - where there are several cairns, and a small unnamed tarn. (This small tarn can just be seen in the photograph above right). The name ''"Swarth"'' fell, like most of the names of geographical features in the area, is of Norse origin: ''svartr'', dark in colour. Approximately 1 km south-east of the summit is the fell's other high point, Swarth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of North Yorkshire
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Cumbria
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beck (stream)
Beck David Hansen (born Bek David Campbell; July 8, 1970) is an American musician, singer, songwriter, and record producer. He rose to fame in the early 1990s with his experimental and lo-fi style, and became known for creating musical collages of wide-ranging genres. He has musically encompassed folk, funk, soul, hip hop, electronic, alternative rock, country, and psychedelia. He has released 14 studio albums (three of which were released on indie labels), as well as several non-album singles and a book of sheet music. Born and raised in Los Angeles, Beck grew towards hip-hop and folk in his teens and began to perform locally at coffeehouses and clubs. He moved to New York City in 1989 and became involved in the city's anti-folk movement. Returning to Los Angeles in the early 1990s, he cut his breakthrough single " Loser", which became a worldwide hit in 1994, and released his first major album, ''Mellow Gold'', the same year. ''Odelay'', released in 1996, topped critic po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hugh Seat
Hugh Seat is a mountain, or more accurately a fell, in Mallerstang on the eastern edge of Cumbria, England. It lies on the border between Cumbria and North Yorkshire. Hugh Seat is a high point above Black Fell Moss, an extensive area of peat bog drained by Red Gill Beck, which is the source of the River Eden. At this " watershed of England" two other great rivers, the Ure and the Swale, also rise within a kilometre of the Eden. Although it has a relatively small prominence, having several other high points nearby (and is therefore classified as a "sub- Hewitt" or a Nuttall but not a Marilyn), Hugh Seat nevertheless rises conspicuously above the source of the River Eden. The old name for this peak was Hugh Seat Morvill or sometimes Morvil Hill, (and Daniel Defoe confuses it with Wild Boar Fell in his "Tour"). Near the summit there is a column of cut stones, known as "Lady's Pillar", and the inscription ''AP1664'' can just be made out - for ''Anne Pembroke'', Lady Anne Cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Seat, Yorkshire Dales
High Seat is a fell in the dale of Mallerstang, Cumbria. With a summit at , it is the fourth highest fell in the Yorkshire Dales after Whernside, Ingleborough and Great Shunner Fell. It is in the north-western part of the Dales, overlooking the deep trench of Mallerstang, and is usually climbed from this side. To the south-east is Hugh Seat (whose summit is marked by Lady Anne's Pillar, commemorating Sir Hugh de Morville). On the opposite (western) side of Mallerstang is the more striking (but 1 metre lower) Wild Boar Fell. It is not a Marilyn, having a relative height of 112 m, and therefore may be regarded as a subsidiary top of Great Shunner Fell, to the east. It is, however, a HuMP. Oddly enough, it is the highest point on the main England east-to-west watershed in the Dales, the three higher fells being some distance from the watershed. Three main rivers have their origins in the peat bogs here: the River Eden, the River Swale, and the River Ure. See also * H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hewitt (hill)
This is a list of Hewitt mountains in England, Wales and Ireland by height. Lists of mountains and hills in the British Isles#Hewitts, Hewitts are defined as "Hills in England, Wales and Ireland over two thousand" feet in height, the general requirement to be called a Lists of mountains and hills in the British Isles#Elevation, "mountain" in the British Isles, and with a prominence above ; a mix of imperial measures, imperial and metric system, metric thresholds. The Hewitt classification was suggested by Alan Dawson in his 1992 book, "The Relative Hills of Britain". Dawson originally called his Hewitts "Sweats", from "Summits - Wales and England Above Two thousand", before settling on the label Hewitt. In a series of three booklets edited by Dave Hewitt, the list of English Hewitts was published in 1997, and the list of Welsh Hewitts was also published in 1997, and the list of Irish Hewitts was published in 1998. Hewitts were designed to address one of the criticisms of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Norse
Old Norse, Old Nordic, or Old Scandinavian, is a stage of development of North Germanic languages, North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their Viking expansion, overseas settlements and chronologically coincides with the Viking Age, the Christianization of Scandinavia and the consolidation of Scandinavian kingdoms from about the 7th to the 15th centuries. The Proto-Norse language developed into Old Norse by the 8th century, and Old Norse began to develop into the modern North Germanic languages in the mid-to-late 14th century, ending the language phase known as Old Norse. These dates, however, are not absolute, since written Old Norse is found well into the 15th century. Old Norse was divided into three dialects: Old West Norse, ''Old West Norse'' or ''Old West Nordic'' (often referred to as ''Old Norse''), Old East Norse, ''Old East Norse'' or ''Old East Nordic'', and ''Ol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wild Boar Fell
Wild Boar Fell is a mountain in the Yorkshire Dales National Park, on the eastern edge of Cumbria, England. At , it is either the 4th-highest fell in the Yorkshire Dales or the 5th, depending on whether nearby High Seat (2,326 ft) is counted or not. The nearest high point is Swarth Fell which is a ridge about a mile (1½ km) long to the south, at . To the east, on the opposite side of the narrow dale, are High Seat and Hugh Seat. Wild Boar Fell is on the boundary of the civil parishes of Mallerstang and Ravenstonedale. History According to Wainwright the fell gets its name from the wild boar which inhabited the area over 500 years ago. In earlier times, probably up to the mid 19th century, the Millstone Grit, or gritstone, which forms the flat top of the fell, was used for making millstones. Some partly formed millstones can be seen on the eastern flank of the fell — and also on the corresponding western flank of Mallerstang Edge on the opposite side of the dale. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nuttall (hill)
This is a list of Nuttall mountains in England and Wales by height. Nuttalls are defined as peaks above in height, the general requirement to be called a "mountain" in the British Isles, and with a prominence above ; a mix of imperial and metric thresholds. The Nuttall classification was suggested by Anne and John Nuttall in their 1990 two–volume book, "The Mountains of England and Wales". The list was updated with subsequent revised editions by the Nuttalls. Because of the prominence threshold of only , the list is subject to ongoing revisions. In response, Alan Dawson introduced the Hewitts, with a higher prominence threshold of . This was the prominence threshold that the UIAA set down in 1994 for an "independent" peak. In 2010, Dawson replaced his Hewitts with the fully "metric" Simms, consisting of a height threshold of , and a prominence threshold of . However, both the Nuttall and Hewitt classifications have become popular with peak baggers, and both remain in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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