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Brim Fell
Brim Fell is a fell in the English Lake District. It stands to the west of Coniston village in the southern part of the District. Topography The Coniston (or Furness) Fells form the watershed between Coniston Water and the Duddon valley to the west. The range begins in the north at Wrynose Pass and runs south for around 10 miles before petering out at Broughton in Furness on the Duddon Estuary. Alfred Wainwright in his influential ''Pictorial Guide to the Lakeland Fells'' took only the northern half of the range as Lakeland proper, consigning the lower fells to the south to a supplementary work ''The Outlying Fells of Lakeland''. Brim Fell occupies a position in the northern section and therefore qualifies as one of the 214 Wainwrights. Later, guidebook writers have chosen to include the whole range in their main volumes.Richards, Mark: ''Southern Fells'': Collins (2003): Birkett, Bill: ''Complete Lakeland Fells'': Collins Willow (1994): The higher northern part of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Old Man Of Coniston
The Old Man of Coniston is a fell in the Furness Fells in the Cumbria, English Lake District and is the highest point (county top) of the historic county of Lancashire. It is at least high, and lies to the west of the village of Coniston and the lake, Coniston Water. The fell is sometimes known by the alternative name of Coniston Old Man, or simply The Old Man. The mountain is popular with tourists and fell-walkers with a number of well-marked paths to the summit. The mountain has also seen extensive copper and slate mining activity for eight hundred years, and the remains of abandoned mines and spoil tips are a significant feature of the north-east slopes. Height A detailed survey on 24 May 2018 measured the height of the highest visible natural ground to be 802.42 metres (2632'7¼"). The height of the ground on the summit plinth (man-made ground) is 803.53 metres (2636'3"). The same survey also measured the height of nearby Swirl How, and measured it to be also 802.42 metres ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grey Friar
Grey Friar is a fell in the English Lake District, it is one of the Coniston Fells and is situated 13 kilometres west-south-west of Ambleside. It reaches a height of 770 metres (2,526 feet) and stands to the north west of the other Coniston Fells, a little off the beaten track and tends to be the least visited of the group. It is quite a large fell and forms the eastern wall of the Duddon Valley for several kilometres, in fact all drainage from Grey Friar goes to the Duddon Valley and not to Coniston Water. Topography The Coniston (or Furness) Fells form the watershed between Coniston Water and the Duddon valley to the west. The range begins at Wrynose Pass and runs south for around 10 miles before petering out at Broughton in Furness on the Duddon Estuary. Grey Friar is the only major fell in the group not to stand on this main axis, rising to the west of Great Carrs across the depression of Fairfield. Bounded to the north and west by the infant Duddon, Grey Friar has lo ... [...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] |
Levers Water
Levers Water is a small lake in the English Lake District. It is located at the head of the Coppermines Valley, above Coniston village. To its south-west is Raven Tor, a spur of Brim Fell, and to its north-west are Little How Crags and Great How Crags, on the eastern side of the north–south ridge leading to Swirl How. A dam built in 1717 enlarged the existing tarn to provide water for the mines and for the village below. A public footpath on its north-east side connects the Coppermines Valley to Swirl Hawse, while to its south-west, a path leads up Gill Cove to Levers Hawse on the main ridge of the Coniston Fells Coniston may refer to: Australia *Coniston (Northern Territory), a cattle station **Coniston massacre, 1928 *Coniston, New South Wales ** Coniston railway station, New South Wales * Coniston, Tasmania, a town in the Derwent Valley United Kingdo .... References Lakes of the Lake District South Lakeland District {{Cumbria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richard Adams
Richard George Adams (9 May 1920 – 24 December 2016) was an English novelist and writer of the books ''Watership Down'', ''Maia'', ''Shardik'' and ''The Plague Dogs''. He studied modern history at university before serving in the British Army during World War II. Afterwards, he completed his studies, and then joined the British Civil Service. In 1974, two years after ''Watership Down'' was published, Adams became a full-time author. Early life Richard Adams was born on 9 May 1920 in Wash Common, near Newbury, Berkshire, England, the son of Lillian Rosa (Button) and Evelyn George Beadon Adams, a doctor. He attended Horris Hill School from 1926 to 1933, and then Bradfield College from 1933 to 1938. In 1938, he went to Worcester College, Oxford, to read Modern History. In July 1940, Adams was called up to join the British Army. He was commissioned into the Royal Army Service Corps and was selected for the Airborne Company, where he worked as a brigade liaison. He served in Pales ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Plague Dogs
''The Plague Dogs'' is the third novel by Richard Adams, author of ''Watership Down'', about the friendship of two dogs that escape an animal testing facility and are subsequently pursued by both the government and the media. It was first published in 1977, and features a few location maps drawn by Alfred Wainwright, a fellwalker and author. The conclusion of the book involves two real-life characters, Adams' long-time friend Ronald Lockley, and the world-famous naturalist Sir Peter Scott. Having seen a manuscript, both men readily agreed to be identified with the characters and opinions that Adams had attributed to them, as is shown in Adams' preface to the book. Plot This book tells of the escape of two dogs, Rowf and Snitter, from a government research station in the Lake District in England, where they had been horribly mistreated. They live on their own with help from a red fox, or "tod", who speaks to them in a Geordie dialect. After the starving dogs attack some sheep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Copper
Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orange color. Copper is used as a conductor of heat and electricity, as a building material, and as a constituent of various metal alloys, such as sterling silver used in jewelry, cupronickel used to make marine hardware and coins, and constantan used in strain gauges and thermocouples for temperature measurement. Copper is one of the few metals that can occur in nature in a directly usable metallic form ( native metals). This led to very early human use in several regions, from circa 8000 BC. Thousands of years later, it was the first metal to be smelted from sulfide ores, circa 5000 BC; the first metal to be cast into a shape in a mold, c. 4000 BC; and the first metal to be purposely alloyed with another metal, tin, to create ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Head Of The Reservoir
In hydrology, the head is the point on a watercourse up to which it has been artificially broadened and/or raised by an impoundment. Above the head of the reservoir natural conditions prevail; below it the water level above the riverbed has been raised by the impoundment and its flow rate reduced, unless and until banks, barrages, weir sluices or dams are overcome (overtopped), whereby a less frictional than natural course will exist (mid-level and surface rather than bed and bank currents) resulting in flash flooding below. In principle, a distinction must be drawn between the head of a reservoir impounded by a dam, and the head of a works resulting from a barrage or canal locks. Head of a reservoir A head's location varies with the height of the water level against the dam. Since there is only an extremely low flow within the reservoir so no water level gradient, the head can be clearly seen: where the farthest watercourse discharges into the reservoir. Upstream of the ... [...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] |
Barrow-in-Furness
Barrow-in-Furness is a port town in Cumbria, England. Historically in Lancashire, it was incorporated as a municipal borough in 1867 and merged with Dalton-in-Furness Urban District in 1974 to form the Borough of Barrow-in-Furness. In 2023 the borough will merge with Eden and South Lakeland districts to form a new unitary authority; Westmorland and Furness. At the tip of the Furness peninsula, close to the Lake District, it is bordered by Morecambe Bay, the Duddon Estuary and the Irish Sea. In 2011, Barrow's population was 56,745, making it the second largest urban area in Cumbria after Carlisle. Natives of Barrow, as well as the local dialect, are known as Barrovian. In the Middle Ages, Barrow was a small hamlet within the parish of Dalton-in-Furness with Furness Abbey, now on the outskirts of the town, controlling the local economy before its dissolution in 1537. The iron prospector Henry Schneider arrived in Furness in 1839 and, with other investors, opened the Furness Railwa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seathwaite Tarn
Seathwaite Tarn is a reservoir in the Furness Fells within the English Lake District. It is located to the south of Grey Friar and to the west of Brim Fell (on the ridge between The Old Man of Coniston and Swirl How) and north east of the village of Seathwaite on the east of the Duddon Valley. In order to create a source of drinking water the existing tarn was considerably enlarged with a dam in 1904. During the dam construction some of the navvies rioted damaging buildings in the village, several rioters were shot, one dying the next day. The dam is almost long and is concrete cored with slate buttresses, the resulting depth of the tarn being around . Water is not abstracted directly from the tarn, but flows some distance downriver to an off-take weir. On the slopes of Brim Fell, above the head of the reservoir, are the remains of Seathwaite Tarn Mine. This was worked for copper in the mid 19th century, and also appears as a location in the novel ''The Plague Dogs'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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