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Carl Side
Carl Side is a fell in the English Lake District, forming a part of the Skiddaw "family" near the town of Keswick and prominently visible from its streets. It is listed in Alfred Wainwright's ''Pictorial Guides to the Lakeland Fells'' as one of the Northern Fells. Summit The summit is a predominantly grassy plateau smoothly sloping away on all sides except to the north, where some shattered crags look down upon Southerndale. A small cairn marks the highest point. The view southward down Derwentwater is excellent, backed by a wide vista of fells from Clough Head to Sale Fell. Tewet Tarn on High Rigg is the only other significant visible body of water. Nearer at hand the grey flanks of Skiddaw and Little Man loom above the summit. Topography A ridge, known as Longside Edge, descends south-westward from the summit plateau of Skiddaw before swinging around to the west and finally north, descending the three fells of Carl Side, Long Side and Ullock Pike. Between Longside Edge a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skiddaw
Skiddaw is a mountain in the Lake District National Park in England. Its summit is the sixth-highest in England. It lies just north of the town of Keswick, Cumbria, and dominates the skyline in this part of the northern lakes. It is the simplest of the Lake District mountains of this height to ascend (as there is a well-trodden tourist track from a car park to the north-east of Keswick, near the summit of Latrigg) and, as such, many walking guides recommend it to the occasional walker wishing to climb a mountain. This is the first summit of the fell running challenge known as the Bob Graham Round when undertaken in a clockwise direction. The mountain lends its name to the surrounding areas of Skiddaw Forest and Back o' Skidda, and to the isolated Skiddaw House, situated to the east, formerly a shooting lodge and subsequently a youth hostel. It also provides the name for the slate derived from that region: Skiddaw slate. Skiddaw slate has been used to make tuned percussi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clough Head
Clough Head () (meaning: ''hill-top above the ravine'') is a fell, or hill, in the English Lake District. It marks the northern end of the main ridge of the Helvellyn range and is often walked as part of the ridge walk. The fell stands south of the village of Threlkeld and the A66 road, and it forms the steep eastern side of the tranquil valley of St John's in the Vale. On its western side the fell displays a dark mass of rocky crags and a deep-set rocky ravine. On the other side it has smooth grassy slopes. Beneath the north face is the steep valley or clough from which Clough Head gets its name. Also beneath the steep northern face lies the lower hill of Threlkeld Knotts, a granite hill which has been much quarried round its margin. A number of different types of rock are found on and around Clough Head, which were formed in very different circumstances. These include deep-sea sedimentation, effusive volcanic lava flows, explosive volcanism, an intrusion of granite, mineralis ... [...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] |
Skiddaw Little Man
Skiddaw Little Man also called Little Man is a fell in the English Lake District, it is situated four kilometres north of the town of Keswick and reaches a height of 865 m (2,837 ft). Topography Little Man is often overlooked and disregarded as an independent and distinct fell due to its name which makes it sound like a minor top of its parent fell Skiddaw which in fact lies 1.5 kilometres to the north west. With a topographical prominence of 61 metres, Little Man qualifies comfortably as a Hewitt and Nuttall hill and is regarded as a separate fell by renowned mountain writers Alfred Wainwright and Bill Birkett. The fell is actually called Little Man on Ordnance Survey maps and by many guide books. To the north and east Little Man is connected to the Skiddaw massif, Lonscale Fell being the nearest separate fell to the east, 2.5 kilometres away. To the south and the west the fell falls away steeply with fast flowing streams draining the fell into the River Derwent. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bassenthwaite Lake
Bassenthwaite Lake is one of the largest water bodies in the English Lake District. It is long and narrow, approximately long and wide, but is also extremely shallow, with a maximum depth of about . It is the only body of water in the Lake District to use the word ''"lake"'' in its name, all the others being ''"waters"'' (for example, Derwentwater), ''"meres"'' (for example, Windermere) or ''"tarns"'' (for example, Dock Tarn). It is fed by, and drains into, the River Derwent. The lake lies at the foot of Skiddaw, near the town of Keswick. Some maps dating from the 18th century do in fact mark this lake with the name ''Bassenwater'', and the use of the name ''Broadwater'' for this lake is also attested. The A66 dual carriageway runs roughly north–south along the western side of the lake. The lay-bys are popular spots for photographers and bird watchers looking for osprey. The section running south towards Keswick was built along the course of the former Cockermouth, K ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A Pictorial Guide To The Lakeland Fells
''A Pictorial Guide to the Lakeland Fells'' is a series of seven books by A. Wainwright, detailing the fells (the local word for hills and mountains) of the Lake District in northwest England. Written over a period of 13 years from 1952, they consist entirely of reproductions of Wainwright's manuscript, hand-produced in pen and ink with no typeset material. The series has been in print almost continuously since it was first published between 1955 and 1966, with more than 2 million copies sold. It is still regarded by many walkers as the definitive guide to the Lakeland mountains. The 214 fells described in the seven volumes have become known as the Wainwrights. the LDWA register of those who have climbed all the fells listed 674 names. The Wainwright Society maintains a "register of current Society members who have climbed all 214 fells". First editions The first five books were originally published by Wainwright's friend, Henry Marshall, Chief Librarian of Kendal and West ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forestry Commission
The Forestry Commission is a non-ministerial government department responsible for the management of publicly owned forests and the regulation of both public and private forestry in England. The Forestry Commission was previously also responsible for Forestry in Wales and Scotland. However, on 1 April 2013, Forestry Commission Wales merged with other agencies to become Natural Resources Wales, whilst two new bodies (Forestry and Land Scotland and Scottish Forestry) were established in Scotland on 1 April 2019. The Forestry Commission was established in 1919 to expand Britain's forests and woodland, which had been severely depleted during the First World War. The Commission bought large amounts of agricultural land on behalf of the state, eventually becoming the largest manager of land in Britain. Today, the Forestry Commission is divided into three divisions: Forestry England, Forestry Commission and Forest Research. Over time the purpose of the Commission broadened to includ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dodd (Lake District)
Dodd is a small fell in the Lake District, Cumbria, England, four kilometres north-west of Keswick. It forms part of the Skiddaw range in the northern part of the national park and the slopes are heavily wooded. Forestry Dodd lies on Forestry England land known as Dodd Wood; for many years it was extensively planted with conifers right up to the summit which obstructed the view. However, Forestry England started a programme of tree clearance from the top of the fell in 2001 and the summit of the fell is now clear; it is hoped that it will revert to heather moorland in years to come. Influential guidebook author Alfred Wainwright voiced strong opposition to the afforestation of Dodd in his Pictorial Guides to the Lakeland Fells in 1962; it took 40 years for his wishes to come true. Height The fell has a height of 502 metres, though the Ordnance Survey's 1:50,000 ''Landranger'' series marks a spot height of 491 metres. This height in fact refers to a point ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arête
An arête ( ) is a narrow ridge of rock which separates two valleys. It is typically formed when two glaciers erode parallel U-shaped valleys. Arêtes can also form when two glacial cirques erode headwards towards one another, although frequently this results in a saddle-shaped pass, called a col. The edge is then sharpened by freeze-thaw weathering, and the slope on either side of the arête steepened through mass wasting Mass wasting, also known as mass movement, is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in ... events and the erosion of exposed, unstable rock. The word ''arête'' () is actually French for "edge" or "ridge"; similar features in the Alps are often described with the German language, German equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver' ... [...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] |
Ullock Pike
Ullock Pike is a fell situated in northern part of the English Lake District. It is located seven kilometres north west of Keswick and achieves a height of 691 metres (2264 feet). The fell sits on Skiddaw’s south western ridge along with two other fells ( Long Side and Carl Side), this ridge is regarded as the finest way to ascend Skiddaw, with Alfred Wainwright commenting: ‘There is no doubt in my mind that by far the best approach to the top of Skiddaw is by way of its north-west ridge. This offers a fine expedition along a narrow crest in exciting surroundings and provides excellent views throughout … for the collector of summits here are three waiting to be picked off in addition to Skiddaw’. Name The fell’s name comes from the Old Norse language and translates as ‘The peak where the wolves play’. With úlfr meaning wolf and leikr meaning play, there are records that the fell was called Ulvelaik in the 13th century. Topography Ullock Pike drops away steeply ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
