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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 islands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Furness Map
Furness ( ) is a peninsula and region of Cumbria in northwestern England. Together with the Cartmel Peninsula it forms North Lonsdale, historically an exclave of Lancashire. 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 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 islands. The Borough of Barrow-in-Furness, which developed when the Furness iron ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. 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.Walney Island His ... [...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] |
River Esk, Cumbria
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. It is one of two Rivers Esk in Cumbria, and not to be confused with the Border Esk which flows into Cumbria from Scotland. Course The Esk rises in the Sca Fell range of mountains at a height of 800 metres, just below Esk Hause, the mountain pass between the fells of Great End and Esk Pike. The infant river then flows southerly through wild and picturesque countryside receiving many streams flowing off the Scafell range, the most significant of which are Calfcove Gill and Little Narrowcove Beck. The river makes several leaps over waterfalls including the Esk Falls before being joined by its first major tributary Lingcove Beck at Lingcove Bridge. Within a few miles the Esk passes Brotherilkeld Farm, which formerly belonged to the monks of Furness Abbey, at this po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coniston Water
Coniston Water in the English county of Cumbria is the third-largest lake in the Lake District by volume (after Windermere and Ullswater), and the fifth-largest by area. It is five miles long by half a mile wide (8 km by 800 m), has a maximum depth of 184 feet (56 m), and covers an area of 1.89 square miles (4.9 km2). The lake has an elevation of 143 feet (44 m) above sea level. It drains to the sea via the River Crake. Geography and administration Coniston Water is situated within Furness, part of the North Lonsdale exclave of the historic county of Lancashire. Since 1974, it is within the administrative county of Cumbria. Coniston Water 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 of Coniston, the highest fell in the Coniston Fells group and the highest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silurian
The Silurian ( ) is a geologic period and system spanning 24.6 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 shortest period of the Paleozoic Era. 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) became fully terrestrialized. A significant evolutionary milestone during ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. 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 period of the Paleozoic Era by the International Union of Geological Sciences, Intern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. 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 direction, over Colwith Force where it falls 40 feet (12 m), before turning north and flowing into the tarn of Elter W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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'', " ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holiday2005b 052
A holiday is a day set aside by custom or by law on which normal activities, especially business or work including school, are suspended or reduced. Generally, holidays are intended to allow individuals to celebrate or commemorate an event or tradition of cultural or religious significance. Holidays may be designated by governments, religious institutions, or other groups or organizations. The degree to which normal activities are reduced by a holiday may depend on local laws, customs, the type of job held or personal choices. The concept of holidays often originated in connection with religious observances or associated with traditions. The intention of a holiday was typically to allow individuals to tend to religious duties associated with important dates on the calendar. In most modern societies, however, holidays serve as much of a recreational functions as any other weekend days or activities. In many societies, there are important distinctions between holidays designated ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 rel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Borough 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 are usually the only permanent residents, though there are eight old fishermen's cottages which are used by sailors or as second homes. 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 Nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
