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Morecambe Bay
Morecambe Bay is a large estuary in northwest England, just to the south of the Lake District National Park. It is the largest expanse of intertidal mudflats and sand in the United Kingdom, covering a total area of . In 1974, the second largest gas field in the UK was discovered west of Blackpool, with original reserves of over 7 trillion cubic feet (tcf) (200 billion cubic metres). At its peak, 15% of Britain's gas supply came from the bay but production is now in decline. It is also one of the homes of the high brown fritillary butterfly. Natural features The rivers Leven, Kent, Keer, Lune and Wyre drain into the Bay, with their various estuaries making a number of peninsulas within the bay. Much of the land around the bay is reclaimed, forming salt marshes used in agriculture. Morecambe Bay is also an important wildlife site, with abundant birdlife and varied marine habitats, and there is a bird observatory at Walney Island. The bay has rich cockle beds, which have been ...
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Ramsar Convention
The Ramsar Convention on Wetlands of International Importance Especially as Waterfowl Habitat is an international treaty for the conservation and sustainable use of Ramsar sites (wetlands). It is also known as the Convention on Wetlands. It is named after the city of Ramsar in Iran, where the convention was signed in 1971. Every three years, representatives of the contracting parties meet as the Conference of the Contracting Parties (COP), the policy-making organ of the convention which adopts decisions (resolutions and recommendations) to administer the work of the convention and improve the way in which the parties are able to implement its objectives. COP12 was held in Punta del Este, Uruguay, in 2015. COP13 was held in Dubai, United Arab Emirates, in October 2018. List of wetlands of international importance The list of wetlands of international importance included 2,331 Ramsar sites in May 2018 covering over . The countries with most sites are the United Kingdo ...
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Cockle (bivalve)
A cockle is an edible marine bivalve mollusc. Although many small edible bivalves are loosely called cockles, true cockles are species in the family Cardiidae. MolluscaBase eds. (2022). MolluscaBase. Cardiidae Lamarck, 1809. Accessed through: World Register of Marine Species at: https://www.marinespecies.org/aphia.php?p=taxdetails&id=229 on 2022-02-09 True cockles live in sandy, sheltered beaches throughout the world. The distinctive rounded shells are bilaterally symmetrical, and are heart-shaped when viewed from the end. Numerous radial, evenly spaced ribs are a feature of the shell in most but not all genera (for an exception, see the genus ''Laevicardium'', the egg cockles, which have very smooth shells). The shell of a cockle is able to close completely (i.e., there is no "gap" at any point around the edge). Though the shell of a cockle may superficially resemble that of a scallop because of the ribs, cockles can be distinguished from scallops morphologically in that co ...
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River Ribble
The River Ribble runs through North Yorkshire and Lancashire in Northern England. It starts close to the Ribblehead Viaduct in North Yorkshire, and is one of the few that start in the Yorkshire Dales and flow westwards towards the Irish Sea (the Dee in Dentdale and the Twiss in Kingsdale being notable others). Etymology The name ''Ribble'' may be a Brittonic compound-formation. The second element is the noun ''*pol'', with connotations including "puddle, pond, upland-stream" (Welsh ''pwll''). The first is ''rö-'', an intensive prefix, with nouns meaning "great" (Welsh ''rhy-'', Cornish re-). Ribble may once have been known as ''*Bremetonā-'', underlying the name ''Bremetenacum'', the Roman fort at Ribchester. Involved here is the Brittonic root ''*breμ–'', meaning "roaring" (c.f. Welsh ''brefu''), as observed at the river-names Breamish in Northumberland, Braan in Scotland and Brefi in Wales. History Neolithic to Saxon finds from along the River Ribble during the ...
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Ptolemy
Claudius Ptolemy (; grc-gre, Πτολεμαῖος, ; la, Claudius Ptolemaeus; AD) was a mathematician, astronomer, astrologer, geographer, and music theorist, who wrote about a dozen scientific treatises, three of which were of importance to later Byzantine, Islamic, and Western European science. The first is the astronomical treatise now known as the '' Almagest'', although it was originally entitled the ''Mathēmatikē Syntaxis'' or ''Mathematical Treatise'', and later known as ''The Greatest Treatise''. The second is the ''Geography'', which is a thorough discussion on maps and the geographic knowledge of the Greco-Roman world. The third is the astrological treatise in which he attempted to adapt horoscopic astrology to the Aristotelian natural philosophy of his day. This is sometimes known as the ''Apotelesmatika'' (lit. "On the Effects") but more commonly known as the '' Tetrábiblos'', from the Koine Greek meaning "Four Books", or by its Latin equivalent ''Quadrip ...
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Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ...
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Outwash Plain
An outwash plain, also called a sandur (plural: ''sandurs''), sandr or sandar, is a plain formed of glaciofluvial deposits due to meltwater outwash at the terminus of a glacier. As it flows, the glacier grinds the underlying rock surface and carries the debris along. The meltwater at the snout of the glacier deposits its load of sediment over the outwash plain, with larger boulders being deposited near the terminal moraine, and smaller particles travelling further before being deposited. Sandurs are common in Iceland where geothermal activity accelerates the melting of ice flows and the deposition of sediment by meltwater. Formation Sandurs are found in glaciated areas, such as Svalbard, Kerguelen Islands, and Iceland. Glaciers and icecaps contain large amounts of silt and sediment, picked up as they erode the underlying rocks when they move slowly downhill, and at the snout of the glacier, meltwater can carry this sediment away from the glacier and deposit it on a broad plai ...
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Morecambe Bay OS Map
Morecambe ( ) is a seaside town and civil parish in the City of Lancaster district in Lancashire, England. It is in Morecambe Bay on the Irish Sea. Name The first use of the name was by John Whitaker in his ''History of Manchester'' (1771), when he refers to the "æstury of Moricambe". It next appears four years later in ''Antiquities of Furness'', where the bay is described as "the Bay of Morecambe". That name is derived from the Roman name ''Moriancabris Æsturis'' shown on maps prepared for them by ''Claudius Ptolemœus'' (Ptolemy) from his original Greek maps. At this distance in time it is impossible to say if the name was originally derived from an earlier language (e.g. Celtic language) or from Greek. The Latin version describes the fourth inlet north from Wales on the west coast of England as Moriancabris Æsturis. Translated, this gives a more accurate description than the present name of Morecambe Bay as the Latin refers to multiple estuaries on a curved sea, not a ...
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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 ...
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Roa Island
Roa Island lies just over half a mile (1 km) south of the village of Rampside at the southernmost point of the Furness Peninsula in Cumbria, though formerly in the county of Lancashire north of the sands. It is located at ( OS grid ref. SD 233650). It is one of the Islands of Furness in northern England. It has an area of about three hectares. For local government purposes Roa Island is within the Borough of Barrow-in-Furness. The island's population stands at around 100, making it the 15th most populated island in England. __TOC__ History Until 1847 Roa Island was a true island, being accessible only by boat, or on foot across the sands at low tide. John Abel Smith, a London banker, bought Roa in 1840. He built a causeway to the mainland, completed in 1846, and an 810-foot (247 m) deep-water pier known as ''Piel Pier'' from where steamers sailed to Fleetwood. The pier connected with the Furness Railway line to Kirkby via Furness Abbey, making use of the causeway. Initia ...
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Foulney Island
Foulney Island is a low-lying grass and shingle area 1 mile (1.6 km) to the south-east of Roa Island, off the southern tip of the Furness Peninsula in Cumbria, England. Foulney Island is one of the Islands of Furness in Morecambe Bay, northern England. For local government purposes the island is in the borough of Barrow-in-Furness. It has an area of about 40 acres (16 ha). In earlier times it was known as ''Fowle Island''. The island is connected to the mainland via a shingle and rock causeway which was built in Victorian times as a tidal protection measure. The Foulney causeway leaves the Roa Island causeway halfway along its length on the eastern side. The maximum elevation on the island is no more than 10 feet (3 metres) above the high tide level. At the time of highest tides much of the island can be inundated. There are no permanent inhabitants on the island. Bird sanctuary Foulney is a bird sanctuary and is included in the South Walney & Piel Channel Flats Site of Spec ...
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Chapel Island
Chapel Island is a limestone outcrop that lies in the Leven estuary of Morecambe Bay in England, less than from the shoreline at Bardsea in the area known as Ulverston Sands. It is located at ( OS grid ref. SD 321759). It is one of the Islands of Furness in the county of Cumbria, in the area of the historic county of Lancashire ("Lancashire north of the sands"). The island is approximately long and just over at its widest. Its area is about . Chapel Island, known as Harlesyde Isle in 1593, got its present name in 1795. The name was coined by Mrs. Radcliffe in her book ‘Tour of the Lakes’.Farrer and Brownbill, 1914, The Victoria History of the County of Lancashire, Vol. 8, p.276. In the 14th century Augustinian canons from nearby Conishead Priory built a small chapel on the island to serve the needs of travellers and fishermen working in the Leven fisheries. The Island lies on the path of the ancient crossing from Cartmel to Conishead and would have been a place of have ...
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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 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 ...
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