|
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] |
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] |
West Riding Of Yorkshire
The West Riding of Yorkshire is one of three historic subdivisions of Yorkshire, England. From 1889 to 1974 the administrative county County of York, West Riding (the area under the control of West Riding County Council), abbreviated County of York (WR), was based closely on the historic boundaries. The lieutenancy at that time included the City of York and as such was named West Riding of the County of York and the County of the City of York. Its boundaries roughly correspond to the present ceremonial counties of West Yorkshire, South Yorkshire and the Craven, Harrogate and Selby districts of North Yorkshire, along with smaller parts in Lancashire (for example, the parishes of Barnoldswick, Bracewell, Brogden and Salterforth became part of the Pendle district of Lancashire and the parishes of Great Mitton, Newsholme and Bowland Forest Low became part of the Ribble Valley district also in Lancashire), Cumbria, Greater Manchester and, since 1996, the unitary East Riding of ... [...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] |
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] |
Grisedale
Grisedale (sometimes Grisdale, or Grizedale rchaic is a south east facing Dale in Cumbria, England, east of Sedbergh, and west of Hawes. Grisedale Beck, which drains Baugh Fell, flows down the dale eastwards, and on reaching the valley floor at Garsdale, forms the River Clough before turning westwards towards the Irish Sea. A small part of the north-eastern side of the dale is in North Yorkshire, however, until 1974, all of the area around, and including Grisedale, was part of the West Riding of Yorkshire. The dale was largely depopulated of its working farmers during the 20th century, however, some of the houses have been re-occupied by non-agricultural inhabitants. The subject of the farm workers moving out prompted Yorkshire Television to commission a film about the last farmer in the dale (''The Dale that Died''), with its director, Barry Cockcroft, remarking that Grisedale was "the most romantic dale in all of Yorkshire." History Grisedale is a south-east facing Dale ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yorkshire Dales
The Yorkshire Dales is an upland area of the Pennines in the Historic counties of England, historic county of Yorkshire, England, most of it in the Yorkshire Dales National Park created in 1954. The Dales comprise river valleys and the hills rising from the Vale of York westwards to the hilltops of the Pennine Drainage divide, watershed. In Ribblesdale, Dentdale and Garsdale, the area extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of York, into the River Ouse, Yorkshire, Ouse and the Humber. The extensive limestone cave systems are a major area for caving in the UK and numerous walking trails run through the hills and dales. Etymology The word ''Dale (landform), dale'', like ''dell'', is derived from the Old English word ''dæl''. It has cognates in the North Germanic languages, Nordic/Germanic languages, Germanic words for valley (''dal'', ''tal''), and occurs in valley names across Yorkshire and Northern England. Usage here may have ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baugh Fell
Baugh Fell (, or ) is a large, flat-topped hill in the northern Pennines of England. It lies in the north-western corner of the Yorkshire Dales National Park, immediately to the east of the Howgill Fells and to the north of Whernside, the highest of the Yorkshire Three Peaks. Formerly in the West Riding of Yorkshire, since 1974 it has been part of the county of Cumbria. Topography Baugh Fell is bounded by Garsdale to the south and by the valley of the River Rawthey to the west; on the north-eastern side it adjoins Swarth Fell and Wild Boar Fell. The fell sprawls over a wide area, roughly in size, with generally steep slopes on the Garsdale side and gentler slopes to the west. The Rawthey rises high up on the summit plateau (where it is called Rawthey Gill) and initially flows north, before turning south to form the hill's western boundary. The eastern limit of the fell is marked by Grisedale Beck, the main tributary of the Clough River which flows through Garsdale. The sum ... [...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] |
Tarn (lake)
A tarn (or corrie loch) is a Proglacial lake, proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is toponymy, derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The specific technical use for a body of water in a glacial corrie comes from high number of tarns found in corries in the Lake District, an upland area in Cumbria. Nonetheless, there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
