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Furness
Furness ( ) is a peninsula and region of Cumbria, England. Together with the Cartmel Peninsula it forms North Lonsdale, historically an exclave of Lancashire. On 1 April 2023 it became part of the new unitary authority of Westmorland and Furness. The Furness Peninsula, also known as Low Furness, is an area of villages, agricultural land and low-lying moorland, with the industrial town of Barrow-in-Furness at its head. The peninsula is bordered by the estuaries of the River Duddon to the west and the River Leven in Morecambe Bay to the east. The wider region of Furness consists of the peninsula and the area known as ''High Furness'', which is a relatively mountainous and sparsely populated part of England, extending inland into the Lake District and containing the Furness Fells. The inland boundary of the region is formed by the rivers Leven, Brathay and Duddon, and the lake of Windermere. Off the southern tip of Furness is Walney Island, long, as well as several smaller isl ...
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Walney Island
Walney Island, also known as the Isle of Walney, is an island off the west coast of England, at the western end of Morecambe Bay in the Irish Sea. Within the boundaries of the historic county of Lancashire, it is part of Barrow-in-Furness, separated from the mainland by Walney Channel, which is spanned by the Jubilee Bridge. Walney is the largest island of the Furness Islands group, both in population and size, as well as the largest English island in the Irish Sea. Its population at the 2011 UK Census was 10,651, distributed evenly across the island's two Wards of Walney North and Walney South. Walney Island formed during the last glacial period, when the River Duddon was a large glacial lake, depositing till at its mouth, which became Walney. Some evidence of Neolithic inhabitants has been found in the island's sand dunes, though its name is likely of Norse origin.
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Tarn (lake)
A tarn (or corrie loch) is a mountain lake, pond or pool, formed in a cirque (or "corrie") excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England – predominantly Cumberland and Westmorland (where there are 197), 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 name of the Tjörnin in Reykjavik, Iceland is also from a related word. The specific technical use for a body of water in a glacial corrie comes from the ...
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River Esk (Ravenglass)
The River Esk, sometimes called the Cumbrian Esk, is a river in Cumbria, England. It flows for approximately 25 km (15.5 miles) from its source in the Scafells range of mountains to its estuary at Ravenglass. The valley it flows through is known as Eskdale. It is one of two Rivers Esk in Cumbria, and not to be confused with the Border Esk which flows into Cumbria from Scotland. In his book ''The Origins Of English Place Names'', P. H. Reaney says that the river's name is derived from the Common Brittonic, Brythonic word ''*Iska'' ("abounding in fish") and cognate with the modern Welsh word ''Pysg'' ("fishes"). This derivation applies to many similarly named rivers throughout Britain including the River Axe (other), Axe, River Exe, Exe and River Usk, Usk, the names evolving local distinctions over the centuries. Gives details of etymology (second paragraph). The Esk is, in part, paralleled by the narrow-gauge Ravenglass and Eskdale Railway and as a consequence the ...
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Coniston Water
Coniston Water is a lake in the Lake District in North West England. It is the third largest by volume, after Windermere and Ullswater, and the fifth-largest by area. The lake has a length of , a maximum width of , and a maximum depth of . Its outflow is the River Crake, which drains into Morecambe Bay via the estuary of the River Leven. The lake is in the unitary authority of Westmorland and Furness, and the ceremonial county of Cumbria. Geography and administration Coniston Water is situated within Furness, part of the North Lonsdale exclave of the historic county of Lancashire. It has been within the ceremonial county of Cumbria since 1974, and the Westmorland and Furness district since it replaced South Lakeland in 2023. The lake is an example of a ribbon lake formed by glaciation. The lake sits in a deep U-shaped glaciated valley scoured by a glacier in the surrounding volcanic and limestone rocks during the last ice age. To the north-west of the lake rises the Old Man ...
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Silurian
The Silurian ( ) is a geologic period and system spanning 23.5 million years from the end of the Ordovician Period, at million years ago ( Mya), to the beginning of the Devonian Period, Mya. The Silurian is the third and shortest period of the Paleozoic Era, and the third of twelve periods of the Phanerozoic Eon. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out. One important event in this period was the initial establishment of terrestrial life in what is known as the Silurian-Devonian Terrestrial Revolution: vascular plants emerged from more primitive land plants, dikaryan fungi started expanding and diversifying along with glomeromycotan fungi, and three groups of arthropods ( myriapods, arachnids and hexapods) ...
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Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years from the end of the Cambrian Period Megaannum, Ma (million years ago) to the start of the Silurian Period Ma. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official per ...
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River Brathay
The Brathay is a river of north-west England. Its name comes from Old Norse and means ''broad river''. It rises at a point 1289 feet (393 m) above sea level near the Three Shire Stone at the highest point of Wrynose Pass () in the Lake District. Its catchment area includes the northern flanks of Wetherlam, Great Carrs and others of the Furness Fells, as well as a substantial area of the Langdale Fells. It flows through Elter Water, marking the division between its upper and lower catchments. Upper Brathay catchment The small stream at the top of Wrynose quickly gathers pace as it descends some 930 feet (283 m) in a distance of about two miles (3.2 km), running roughly parallel to, and south of, the Wrynose Pass road. Before flowing into Little Langdale Tarn it subsumes Bleamoss Beck, the outflow from Blea Tarn. Little Langdale Tarn is also replenished by the Greenburn Beck. The Brathay drains Little Langdale Tarn at its eastern side. It continues in an easterly dir ...
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Wrynose Pass
The Wrynose Pass is a mountain pass in the Lake District National Park in Cumbria, England between the Duddon Valley and Little Langdale. Etymology The unusual name of the pass is taken from that of the adjacent Wrynose hill, also called Wrynose Fell. The name was recorded in 12th-century documents as "Wrenhalse" and in the 16th century as "Wrenosse Hill". It is thought, based on a suggestion by Eilert Ekwall, to mean "stallion's ridge", being formed on the Old Norse words ''(v)reini'' ("stallion", probably here used as a byname for an individual), and ''hala''.Mills, ''The place-names of Lancashire'', Batsford, 1976, p.153 It is one of a number of place names of Scandinavian origin in the area. Although most academic sources characterise "Vreini" in this context as a personal name, it has also been explained as suggesting "the horse power needed to climb it".Cooper, ''The Tarns of Lakeland'', Warne, 1960, p. 201 Other suggested origins are from Old Norse ''ravn hals'', "p ...
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Holiday2005b 052
A holiday is a day or other period of time set aside for festivals or recreation. ''Public holidays'' are set by public authorities and vary by state or region. Religious holidays are set by religious organisations for their members and are often also observed as public holidays in religious majority countries. Some religious holidays, such as Christmas, have become secularised by part or all of those who observe them. In addition to secularisation, many holidays have become commercialised due to the growth of industry. Holidays can be thematic, celebrating or commemorating particular groups, events, or ideas, or non-thematic, days of rest that do not have any particular meaning. In Commonwealth English, the term can refer to any period of rest from work, such as vacations or school holidays. In American English, "the holidays" typically refers to the period from Thanksgiving to New Year's (late November to January 1), which contains many important holidays in American culture. ...
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Rampside
Rampside is a village in Cumbria, England. Historically in Lancashire, it is located a few miles south-east of the town of Barrow-in-Furness, in the north-western corner of Morecambe Bay on the Furness peninsula. History There is evidence that the village was inhabited as early as 1292, in the records of the monks of Furness Abbey, though Viking and Roman artefacts have been found in the village's church. As well as agriculture, the village acted as a small port, with shipping trade coming to Furness Abbey through Roa Island, which itself was defended by the fortified Piel Island, both around one mile south of Rampside.''Barrow and District'' by Fred Barnes, Barrow-in-Furness Corporation, Barrow-in-Furness (Lancs) 1968 Thomas Lawson, a herbalist and botanist, was born at Rampside in 1630 and became minister at the village church. He invited George Fox to preach from the pulpit after one Sunday service, and subsequently became a Quaker himself in 1653. He published various ...
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Piel Island
Piel Island lies in Morecambe Bay, around off the southern tip of the Furness peninsula in the administrative county of Cumbria, England. It is one of the Islands of Furness, three of which sit near to Piel at the mouth of Walney Channel. The island is the location of Piel Castle, built by the monks of Furness Abbey in the fourteenth century. Historically within Lancashire, the island today is owned by the town of Barrow-in-Furness, having been given to the people by the Duke of Buccleuch in 1922. The council's administrative duties also include the selection of the "King" of Piel, who is the landlord of the island's public house, the Ship Inn. Piel is about in size. The landlord and their family and three others who live in the old Ship's pilots' cottages are the island's only permanent residents. History In the Middle Ages Piel was known as Fowdray (or Fouldrey or Fowdrey) island. This name would seem to be derived from the Old Norse words ', meaning "fodder", and ' o ...
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