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Lingmoor Fell
Lingmoor Fell is a fell in the English Lake District, situated eight kilometres (five miles) west of Ambleside. The fell reaches a height of 469 m (1,540 ft) and divides the valleys of Great Langdale and Little Langdale. The fell's name originates from the Old Norse word ''lyng'' meaning “heather covered”. The actual summit of the fell is named as Brown How on Ordnance Survey maps. Topography Although it is surrounded by higher and better-known fells, Lingmoor Fell is quite separate and distinct with no connecting ridges to other fells, giving it a considerable (for such a small fell) topographic prominence of 245 metres (804 feet), making it a Marilyn hill. Lingmoor Fell has a subsidiary top, known as Side Pike (362 m, 1,187 ft), which lies 1.5 kilometres (0.9 miles) to the north-west. This is a fine rock tower accessible only from the west and south. Walkers wishing to visit Side Pike from Lingmoor Fell are blocked by unassailable crags and must travers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Fell (Lake District)
Black Fell is a fell in the English Lake District. It rises to the north of Tarn Hows, between Coniston and Hawkshead. Topography Black Fell is the high point in the hilly area bounded by Windermere, Langdale and Coniston. It occupies an area of around one mile by two, clad mainly in fell grass with many small outcrops of rock. Despite its modest altitude Alfred Wainwright accorded Black Fell a chapter in his ''Pictorial Guide to the Lakeland Fells'', partly due to its excellence as a view point. It represents the perimeter of the Lakeland Fells proper in his opinion, the land to the south falling within his supplementary volume, ''The Outlying Fells of Lakeland''. Later guidebook writers have also included Black Fell within their remit.Richards, Mark: ''Southern Fells'': Collins (2003): Birkett, Bill: ''Complete Lakeland Fells'': Collins Willow (1994): The fell has no obvious connecting ridges in the manner of higher mountains, but in fact has a pivotal position in this area o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing
Climbing is the activity of using one's hands, feet, or any other part of the body to ascend a steep topographical object that can range from the world's tallest mountains (e.g. the eight thousanders), to small boulders. Climbing is done for locomotion, sporting recreation, and for competition, and is also done in trades that rely on ascension; such as emergency rescue and military operations. Climbing is done indoors and outdoors and on natural (e.g. rock and ice) and artificial surfaces. Professional mountain guides or rock climbing guides (e.g. the UIAGM), were a significant element in developing the popularity of the sport in the natural environment, and remain so today. Since the 1980s, the development of competition climbing and the availability of artificial climbing walls have dramatically increased the popularity of rock climbing as a sport and led to the emergence of professional rock climbers, such as Wolfgang Güllich, Chris Sharma, Lynn Hill and Catherine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyns Of England
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Ireland by height. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,011 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophonous with (Marilyn) '' Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequent British Isles classifications that rely solely on prominence, including the P600s, the HuMPs, and the TuMPs. Topographic prominence is a more difficult to estimate than to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Furness Fells
The Furness Fells are a multitude of hills and mountains in the Furness region of Cumbria, England. Historically part of Lancashire, the Furness Fells or High Furness is the name given to the upland part of Furness, that is, that part of Furness lying north of the line between Ulverston and Ireleth. The hills lie largely within the English Lake District. The term ''Furness Fells'' is also sometimes used as a synonym with ''Coniston Fells'', perhaps partly as a result of the placing of the words "Furness Fells" on some Ordnance Survey 1:250 000 maps. The Coniston Fells properly form only part of the Furness Fells, albeit with all the highest mountains; other fells in Furness are of lower altitude. The Coniston Fells form part of the Southern Fells of the Lake District as defined by Alfred Wainwright. Coniston Fells The Coniston Fells are separated from the Scafell and Bowfell massif to their north by Wrynose Pass, and are surrounded on all other sides by lower ground. Coniston ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry Stone
Dry stone, sometimes called drystack or, in Scotland, drystane, is a building method by which structures are constructed from stones without any mortar to bind them together. Dry stone structures are stable because of their construction method, which is characterized by the presence of a load-bearing façade of carefully selected interlocking stones. Dry stone construction is best known in the context of stone walls, traditionally used for the boundaries of fields and churchyards, or as retaining walls for terracing, but dry stone sculptures, buildings, bridges, and other structures also exist. The term tends not to be used for the many historic styles which used precisely-shaped stone, but did not use mortar, for example the Greek temple and Inca architecture. The art of dry stone walling was inscribed in 2018 on the UNESCO representative list of the intangible cultural heritage of humanity, for dry stone walls in countries such as France, Greece, Italy, Slovenia, Cr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blea Tarn (Langdale)
Little Langdale is a valley in the Lake District, England, containing Little Langdale Tarn and a hamlet also called Little Langdale. A second tarn, Blea Tarn, is in a hanging valley between Little Langdale and the larger Great Langdale to the north. Little Langdale is flanked on the south and southwest by Wetherlam and Swirl How, and to the north and northwest by Lingmoor Fell and Pike of Blisco. The valley descends to join with Great Langdale above Elter Water. Description Langdale was previously known as ''Langdene'' meaning 'far away wooded valley' and referring to its distance along the flint route from Whitley Bay. Historically Little Langdale was at the intersection of packhorse routes leading to Ravenglass, Whitehaven, Keswick, Penrith & Carlisle, Ambleside, Hawkshead, and Coniston, Ulverston, Broughton-in-Furness and Barrow in Furness. Slater's Bridge which crosses the River Brathay in 3 spans supported by a large mid-stream boulder and stone causeways is a 16th-cen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westmorland
Westmorland (, formerly also spelt ''Westmoreland'';R. Wilkinson The British Isles, Sheet The British IslesVision of Britain/ref> is a historic county in North West England spanning the southern Lake District and the northern Dales. It had an administrative function from the 12th century until 1974. Between 1974 and 2023 Westmorland lay within the administrative county of Cumbria. In April 2023, Cumbria County Council will be abolished and replaced with two unitary authorities, one of which, Westmorland and Furness, will cover all of Westmorland (as well as other areas), thereby restoring the Westmorland name to a top-tier administrative entity. The people of Westmorland are known as Westmerians. Early history Background At the beginning of the 10th century a large part of modern day Cumbria was part of the Kingdom of Strathclyde, and was known as '' "Scottish Cumberland" ''. The Rere Cross was ordered by Edmund I (r.939-946) to serve as a boundary marker between England an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elterwater
Elterwater is a village in the English Lake District and the county of Cumbria. The village lies half a mile (800 m) north-west of the lake of Elter Water, from which it derives its name. Both are situated in the valley of Great Langdale. Elterwater Bridge is a Grade II listed structure dating to at least the 18th century. Economic activity In the past, the principal industries have been farming, quarrying for slate and gunpowder manufacture. The first two activities continue, while evidence of the latter survives in the grounds of the Langdale Estate, a holiday development founded in the 1930s and redeveloped as a timeshare in the 1980s. In the present day, tourism is a principal source of income and the village is popular with fell-walkers. Art In the 1880s, the Guild of St George founded by John Ruskin revived small-scale linen spinning and weaving in Langdale, at a cottage in Elterwater, led by Albert Fleming and Marion Twelves and continued by Elizabeth Pepper. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Geological Survey
The British Geological Survey (BGS) is a partly publicly funded body which aims to advance geoscientific knowledge of the United Kingdom landmass and its continental shelf by means of systematic surveying, monitoring and research. The BGS headquarters are in Keyworth, Nottinghamshire, England. Its other centres are located in Edinburgh, Wallingford, Cardiff and London. The current motto of the BGS is: ''Gateway to the Earth''. History and previous names The Geological Survey was founded in 1835 by the Board of Ordnance as the Ordnance Geological Survey, under Henry De la Beche. This was the world's first national geological survey. It remained a branch of the Ordnance Survey for many years. In 1965, it was merged with the Geological Museum and Overseas Geological Surveys, under the name of Institute of Geological Sciences. On 1 January 1984, the institute was renamed the British Geological Survey (and often referred to as the BGS), a name still carried today. Competenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lapilli
Lapilli is a size classification of tephra, which is material that falls out of the air during a volcanic eruption or during some meteorite impacts. ''Lapilli'' (singular: ''lapillus'') is Latin for "little stones". By definition lapilli range from in diameter. A pyroclastic particle greater than 64 mm in diameter is known as a volcanic bomb when molten, or a volcanic block when solid. Pyroclastic material with particles less than 2 mm in diameter is referred to as volcanic ash. Formation Lapilli are spheroid-, teardrop-, dumbbell- or button-shaped droplets of molten or semi-molten lava ejected from a volcanic eruption that fall to earth while still at least partially molten. These granules are not accretionary, but instead the direct result of liquid rock cooling as it travels through the air. Lapilli tuffs are a very common form of volcanic rock typical of rhyolite, andesite and dacite pyroclastic eruptions, where thick layers of lapilli can be deposited during a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
