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Hindscarth
Hindscarth is a mountain between the valleys of Buttermere and Newlands, in the north-western part of the English Lake District. The fell's name is derived from two words from the Old Norse language, ''Hind'' and ''Skarth'', and means the pass used by the red deer. Topography The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north-south axis. Two roads cross from east to west, dividing the fells into three convenient groups. Hindscarth stands in the southern sector. The principal ridge in this group of fells runs east from Buttermere, climbing over Robinson, Hindscarth and Dale Head. It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells. The ridge from Robinson to Dale Head forms the heads of Little Dale and Newlands, bypassing the intervening summit of Hindscarth. This stands off to the north, forming the dividing wall between the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Robinson (Lake District)
Robinson seen from the Ard Crags ridge, with Hindscarth to the left Robinson is a fell in the English Lake District, its southern slopes descending to Buttermere, while its northern side is set in the Newlands Valley. Paths lead to the summit from the village of Buttermere, from the nearby summit Dale Head and from various locations in the valleys to the north. Name According to influential guidebook author Alfred Wainwright,Alfred Wainwright: ''A Pictorial Guide to the Lakeland Fells, Book 6, The North Western Fells'': Westmorland Gazette (1964): the name Robinson comes from a Richard Robinson who purchased estates in the Buttermere area many centuries ago. These included this unnamed hill which was then called "Robinson's Fell", later shortened to Robinson. Topography The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north–south axis. Two roads cross from east to west, dividing the fells ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newlands Horseshoe
The Newlands horseshoe is a circular walk in the Lake District, incorporating the main peaks surrounding the Newlands Valley. Standard round The regular horseshoe covers six peaks, and approximately 9.4 miles or 15.1 kilometers of walking. It includes the fells Catbells, Maiden Moor,(1687 ft), High Spy (2143 ft), Dale Head (2473 ft), Hindscarth (2385 ft), and Robinson. The walk may be extended by another five or so miles, and by four more peaks, by including an extra traverse from Knott Rigg to Causey Pike; but the Horseshoe proper - culminating in what Wainwright called “the deep trench confined by Maiden Moor and Hindscarth” - surrounds and encloses Upper Newlands itself. Wainwright’s version Wainwright himself favoured a slightly reduced round, beginning at Cat’s Bells but omitting Robinson in favour of a descent via Hindscarth and Scope End. Apart from the beauty of the track itself, the latter descent (in his opinion) “earns full marks because of the lovely vie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newlands Valley
The Newlands Valley is in the Lake District National Park in Cumbria, England. It is regarded as one of the most picturesque and quiet valleys in the national park, even though it is situated very close to the popular tourist town of Keswick and the busy A66 road. The valley forms part of the civil parish of Above Derwent, within the Borough of Allerdale. Early history The earliest signs of human settlement in the valley have been found at Ullock, where evidence of a Bronze Age burial site has been found. The remains of a Celtic workshop were also found at Portinscale. Viking herdsmen arrived in Cumbria after 800 AD. Many of the present day place names in the Newlands valley have their origins from these early Norse settlers. The valley area was originally called Rogersat or Rogersyde which was derived from the Old Norse “Roger-Saetr”, which translates as ''Summer pasture belonging to Roger''. The present day Newlands valley settlements of Keskadale, Skelgill, Birk Rigg, Hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dale Head
Dale Head is a fell in the north-western sector of the Lake District, in northern England. It is 753 metres or 2,470 feet above sea level and stands immediately north of Honister Pass, the road between Borrowdale and Buttermere. Topography The North-Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north-south axis. Two roads cross from east to west, dividing the fells into three convenient groups. Dale Head is the highest fell in the southern sector. Dale Head is the apex of two hill ridges. The principal ridge descends from Dale Head to the north-east and forms several other fells, each given a chapter by Alfred Wainwright in his Pictorial Guides to the Lakeland Fells. These are High Spy, Maiden Moor and Catbells (alternative spelling, Cat Bells). This ridge forms the western side of Borrowdale and overlooks Derwent Water. The other ridge descends to the north-west and includes the fells o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Wainwrights
Wainwrights are the 214 English peaks (known locally as ''fells'') described in Alfred Wainwright's seven-volume ''Pictorial Guide to the Lakeland Fells'' (1955–66). They all lie within the boundary of the Lake District National Park in Cumbria, and all but one (Castle Crag) are over in height. Over two million copies of the ''Pictorial Guides'' have been sold since their publication. In 1974, Wainwright published a supplementary volume ''The Outlying Fells of Lakeland'' (1974), which includes another 116 summits (described in 56 walks); these are the Wainwright Outlying Fells. Summiting all of the Wainwrights is a popular form of peak bagging in the Lake District, along with the Birketts. Because both lists are based on historical books, unlike, for example, the Munros, their constituents remain fixed, regardless of revisions to height or other metrics. In this regard, they are similar to the Scottish lowlands, Donalds. There are 214 Wainwrights, of which 209 are also c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catbells
Cat Bells is a fell in the English Lake District in the county of Cumbria. It has a height of and is one of the most popular fells in the area. It is situated on the western shore of Derwentwater within of the busy tourist town of Keswick. Its distinctive shape catches the attention of many visitors to the Lakes who feel compelled to climb to the summit after seeing it from the viewpoint of Friars' Crag on the opposite side of Derwentwater. The Lake District writer and walker Alfred Wainwright acknowledges the popularity of Cat Bells among fellwalkers of all abilities by saying: Name The fell's unusual name may well have come from a distortion of "Cat Bields" meaning shelter of the wild cat, although this is not certain. The fell's name is sometimes written as Catbells. Topography Cat Bells is the last fell on the ridge separating Derwentwater from the Newlands valley. It rises due south from Hawse End, reaching the summit in two distinct steps. The lower top is named Skelgi ... [...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] |
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] |
North Western Fells
The North Western Fells are a group of hills in the English Lake District. Including such favourites as Catbells and Grisedale Pike, they occupy an oval area beneath the Buttermere and Borrowdale valley systems. The North Western Fells are characterised by soaring east-west ridges and an absence of mountain tarns. Partition of the Lakeland Fells The Lake District is a National Park in the north west of the country which, in addition to its lakes, contains a complex range of hills. These are known locally as fells and range from low hills to the highest ground in England. Hundreds of tops exist and many writers have attempted to draw up definitive lists. In doing so the compilers frequently divide the range into smaller areas to aid their description. The most influential of all such authors was Alfred Wainwright whose ''Pictorial Guide to the Lakeland Fells'' series has sold in excess of 2 million copies, [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mudstone
Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, W. H. Freeman, 2nd ed, 529 pp. The term ''mudstone'' is also used to describe carbonate rocks (limestone or dolomite) that are composed predominantly of carbonate mud. However, in most contexts, the term refers to siliciclastic mudstone, composed mostly of silicate minerals. The NASA Curiosity rover has found deposits of mudstone on Mars that contain organic substances such as propane, benzene and toluene. Definition There is not a single definition of mudstone that has gained general acceptance,Boggs 2006, p.143 though there is wide agreement that mudstones are fine-grained sedimentary rocks, composed mostly of silicate grains with a grain size less than . Individual grains this size are too small to be disting ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olistostrome
An olistostrome is a sedimentary deposit composed of a chaotic mass of heterogeneous material, such as blocks and mud, known as olistoliths, that accumulates as a semifluid body by submarine gravity sliding or slumping of the unconsolidated sediments. It is a mappable stratigraphic unit which lacks true bedding, but is intercalated amongst normal bedding sequences, as in the Cenozoic basin of central Sicily. The term olistostrome is derived from the Greek ''olistomai'' (to slide) and ''stroma'' (accumulation).Ernesto Abbate, et al., "Olistostromes and olistoliths", ''Sedimentary Geology'', 4 (1970), 521-557. See also *Submarine landslide Submarine landslides are marine landslides that transport sediment across the continental shelf and into the deep ocean. A submarine landslide is initiated when the downwards driving stress (gravity and other factors) exceeds the resisting str ... References Sedimentary rocks {{Geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mining
Mining is the extraction of valuable minerals or other geological materials from the Earth, usually from an ore body, lode, vein, seam, reef, or placer deposit. The exploitation of these deposits for raw material is based on the economic viability of investing in the equipment, labor, and energy required to extract, refine and transport the materials found at the mine to manufacturers who can use the material. Ores recovered by mining include metals, coal, oil shale, gemstones, limestone, chalk, dimension stone, rock salt, potash, gravel, and clay. Mining is required to obtain most materials that cannot be grown through agricultural processes, or feasibly created artificially in a laboratory or factory. Mining in a wider sense includes extraction of any non-renewable resource such as petroleum, natural gas, or even water. Modern mining processes involve prospecting for ore bodies, analysis of the profit potential of a proposed mine, extraction of the desired materials, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
