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Heron Pike
Heron Pike is a fell in the English Lake District, two kilometres east of Grasmere. It is part of the Fairfield group in the Eastern Fells. It should not be confused with the Heron Pike that forms part of Sheffield Pike, although it appears that, by coincidence, both Heron Pikes are exactly the same height. Topography Not a fell of great significance, Heron Pike is a slight grassy rise on the long southern ridge of its parent fell Fairfield. Just cresting the 2,000 foot mark at 612 m (2,008 ft), it is mostly climbed as part of the Fairfield horseshoe walk and it lies between the adjoining fells of Nab Scar and Great Rigg. Heron Pike’s eastern side features Erne Crag and Blind Cove as it falls away quite steeply towards Rydal Beck. At the base of Erne Crag is an old quarry, the mouth of a cavern quite easy to locate.Richards, Mark: ''Near Eastern Fells'': Collins (2003): The fell's western flank drops towards Grasmere and has the small Alcock Tarn on its low ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Rigg
Great Rigg is a fell in the English Lake District, 7 kilometres (4½ miles) north-west of Ambleside and reaching a height of 766 metres (2,513 feet). It is most often climbed as part of the Fairfield horseshoe, a 16-km circular walk which starts and finishes in Ambleside. The fell's name originates from the Old English "Rigg", meaning a bumpy or knobbly ridge. Topography Great Rigg is mostly without merit, being just an undulation on one of Fairfield's southern ridges; with 31 metres of prominence it just qualifies as a Hewitt. It is best seen from the south-west near Grasmere where from that angle its summit seems to dominate the valley. The fell is rocky on its eastern side as Stone Cove drops to Rydal Beck; on its western flank it is mostly grassy as it falls away to Tongue Gill; to the north and south are ridges which continue to other fells, with Fairfield being 1.5 kilometres (0.9 miles) away to the north while Heron Pike lies 2.5 kilometres (1.6 miles) to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Wainwright
Alfred Wainwright MBE (17 January 1907 – 20 January 1991), who preferred to be known as A. Wainwright or A.W., was a British fellwalker, guidebook author and illustrator. His seven-volume ''Pictorial Guide to the Lakeland Fells'', published between 1955 and 1966 and consisting entirely of reproductions of his manuscript, has become the standard reference work to 214 of the fells of the English Lake District. Among his 40-odd other books is the first guide to the Coast to Coast Walk, a 182-mile long-distance footpath devised by Wainwright which remains popular today. Life Alfred Wainwright was born in Blackburn, Lancashire, into a family which was relatively poor, mostly because of his stonemason father's alcoholism. He did very well at school (first in nearly every subject) although he left at the age of 13. While most of his classmates were obliged to find employment in the local mills, Wainwright started work as an office boy in Blackburn Borough Engineer's Department. He ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fells Of The Lake District
A fell (from Old Norse ''fell'', ''fjall'', "mountain"Falk and Torp (2006:161).) is a high and barren landscape feature, such as a mountain or moor-covered hill. The term is most often employed in Fennoscandia, Iceland, the Isle of Man, parts of northern England, and Scotland. Etymology The English word "fell" comes from Old Norse ''fell'' and ''fjall'' (both forms existed). It is cognate with Danish ''fjeld'', Faroese ''fjall'' and ''fjøll'', Icelandic ''fjall'' and ''fell'', Norwegian ''fjell'' with dialects ''fjøll'', ''fjødd'', ''fjedd'', ''fjedl'', ''fjill'', ''fil(l)'', and ''fel'', and Swedish ''fjäll'', all referring to mountains rising above the alpine tree line.Bjorvand and Lindeman (2007:270–271). British Isles In northern England, especially in the Lake District and in the Pennine Dales, the word "fell" originally referred to an area of uncultivated high ground used as common grazing usually on common land and above the timberline. Today, gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nuttalls
Nuttall may refer to: People * Nuttall (name) * Nuttall baronets Nature * Nuttall's oak, a fast-growing large deciduous oak tree native to North America * Nuttall's woodpecker, a species of woodpecker found in oak woodlands of California * Nuttall sandstone, a very hard type of sandstone; see New River Gorge National River * Nuttall's toothwort, a species of cardamine flower. Places * Nuttall, Virginia, United States * Nuttall railway station, Nuttall village, Nasirabad, Balochistan, Pakistan * Nuttalls, hills in England and Wales that are over with a prominence above Other uses * BAM Nuttall, a British construction company * Blackman–Nuttall window, a mathematical function used in signal processing—see Window function * Codex Zouche-Nuttall, a pre-Columbian piece of Mixtec writing * Geiger–Nuttall law, a rule in nuclear physics stating that short-lived isotopes emit more energetic alpha particles than long-lived ones * Nuttall Ornithological Club, the oldest ornitho ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Fells
The Central Fells are a group of hills in the English Lake District. Reaching their highest point at High Raise (2,500 ft or 762 metres), they occupy a broad area to the east of Borrowdale. The Central Fells are generally lower than the surrounding hills, the Lake District's dome-like structure having a slight dip in the middle. The range extends from the boggy ridge between Derwentwater and Thirlmere in the north, to the rock peaks of the Langdale Pikes in the south. 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 locally known 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, who ... [...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] |
Windermere
Windermere (sometimes tautology (language), tautologically called Windermere Lake to distinguish it from the nearby town of Windermere, Cumbria (town), Windermere) is the largest natural lake in England. More than 11 miles (18 km) in length, and almost 1 mile (1.5 km) at its widest, it is a ribbon lake formed in a glacial trough after the retreat of ice at the start of the current interglacial period. It has been one of the country's most popular places for holidays and summer homes since the arrival of the Kendal and Windermere Railway's branch line in 1847. Forming part of the border between the historic counties of Lancashire and Westmorland, Windermere is today within the administrative county of Cumbria and the Lake District National Park. Etymology The word 'Windermere' is thought to translate as "'Winand or Vinand's lake'... The specific has usually been identified with an Old Swedish personal name 'Vinandr', genitive singular 'Vinandar'"... although "the pers ... [...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] |
Dacite
Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained (aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhyolite. It is composed predominantly of plagioclase feldspar and quartz. Dacite is relatively common, occurring in many tectonic settings. It is associated with andesite and rhyolite as part of the subalkaline volcanic rock, subalkaline tholeiite, tholeiitic and calc-alkaline magma series. Composition Dacite consists mostly of plagioclase feldspar and quartz with biotite, hornblende, and pyroxene (augite or enstatite). The quartz appears as rounded, corroded phenocrysts, or as an element of the ground-mass. The plagioclase in dacite ranges from oligoclase to andesine and labradorite. Sanidine occurs, although in small proportions, in some dacites, and when abundant gives rise to rocks that form rhyodacite, transitions to the rhyolites. The rel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
