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Foreland Basins
Foreland may refer to: * a landform projecting into the sea, such as a headland or a promontory * an area of land in front of something **Foreland basin, in geology, the zone that receives sediment from an adjacent mountain chain **Glacier foreland, the area between the leading edge of a glacier and the moraines of the last maximum Places * Foreland, Isle of Wight, a promontory on the Isle of Wight in England * Foreland Island in the South Shetland Islands, Antarctica * Foreland Point, a headland in Devon, England * Alpine Foreland, a region in Southern Germany * North and South Foreland North Foreland (TR 39860 69616 ) and South Foreland (TR 35909 43307 {{Coord, 51.14040, 1.37110, display=inline, format=dms) are two chalk headlands on the Kent coast of southeast England. See: *North Foreland *South Foreland South Forelan ..., two headlands on the coast of Kent, England See also * Nils Tore Føreland (born 1957), Norwegian politician {{Disambiguation, geo ...
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Headland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ...
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Promontory
A promontory is a raised mass of land that projects into a lowland or a body of water (in which case it is a peninsula). Most promontories either are formed from a hard ridge of rock that has resisted the erosive forces that have removed the softer rock to the sides of it, or are the high ground that remains between two river valleys where they form a confluence. A headland, or head, is a type of promontory. Promontories in history Located at the edge of a landmass, promontories offer a natural defense against enemies, as they are often surrounded by water and difficult to access. Many ancient and modern forts and castles have been built on promontories for this reason. One of the most famous examples of promontory forts is the Citadel of Namur in Belgium. Located at the confluence of the Meuse and Sambre rivers, the citadel has been a prime fortified location since the 10th century. The surrounding rivers act as a natural moat, making it difficult for enemies to access th ...
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Foreland Basin
A foreland basin is a structural basin that develops adjacent and parallel to a mountain belt. Foreland basins form because the immense mass created by crustal thickening associated with the evolution of a mountain belt causes the lithosphere to bend, by a process known as lithospheric flexure. The width and depth of the foreland basin is determined by the flexural rigidity of the underlying lithosphere, and the characteristics of the mountain belt. The foreland basin receives sediment that is eroded off the adjacent mountain belt, filling with thick sedimentary successions that thin away from the mountain belt. Foreland basins represent an endmember basin type, the other being rift basins. Space for sediments (accommodation space) is provided by loading and downflexure to form foreland basins, in contrast to rift basins, where accommodation space is generated by lithospheric extension. Types of foreland basin Foreland basins can be divided into two categories: * Periph ...
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Glacier Foreland
The region between the current leading edge of the glacier and the moraines of latest maximum is called glacier foreland or glacier forefield. In the Alps this maximum was in 1850 and since then the region has become ice free due to deglaciation. Because of this relative recent development of vegetation Vegetation is an assemblage of plant species and the ground cover they provide. It is a general term, without specific reference to particular taxa, life forms, structure, spatial extent, or any other specific botanical or geographic character ... and morphodynamic the glacier foreland differs considerably from the surrounding landscape. See also * Glaciology Glacial landforms {{glaciology-stub ...
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Foreland, Isle Of Wight
Foreland or Forelands, and the adjacent Foreland Fields (), is the easternmost point of the Isle of Wight, part of the village of Bembridge. It is located about 6.5 miles due south of the city of Portsmouth on the British mainland, separated by the eastern reaches of the Solent. It is characterised by a pub called the Crab and Lobster Inn and various beach huts plus a beach cafe and a coast guard lookout. In the sea are the reefs of Bembridge Ledge which is rich in edible crabs, lobsters and spider crabs and shoals of mackerel. In the Crab & Lobster Inn are photographs of the many shipwrecks, which included the submarine HMS Alliance, now a museum ship at Gosport and the First World War troopship the S.S. Mehndi carrying troops from South Africa, with great loss of life. Foreland Fields includes Bembridge ledge, an area formerly popular with shipwrecks and smuggling, but also for crab and lobster fishing; there is a Coastguard Station. The channel through the interior of the ...
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Foreland Island
Foreland Island is an island east-southeast of Taylor Point, off the east side of King George Island, in the South Shetland Islands The South Shetland Islands are a group of Antarctic islands with a total area of . They lie about north of the Antarctic Peninsula, and between southwest of the nearest point of the South Orkney Islands. By the Antarctic Treaty of 1 .... This island was known to sealers as early as 1821 and takes its name from North Foreland, the prominent cape to the northwest. See also * List of antarctic and sub-antarctic islands References Islands of King George Island (South Shetland Islands) {{KingGeorgeIslandAQ-geo-stub ...
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South Shetland Islands
The South Shetland Islands are a group of Antarctic islands with a total area of . They lie about north of the Antarctic Peninsula, and between southwest of the nearest point of the South Orkney Islands. By the Antarctic Treaty of 1959, the islands' sovereignty is neither recognized nor disputed by the signatories and they are free for use by any signatory for non-military purposes. The islands have been claimed by the United Kingdom since 1908 and as part of the British Antarctic Territory since 1962. They are also claimed by the governments of Chile (since 1940, as part of the Antártica Chilena province) and Argentina (since 1943, as part of Argentine Antarctica, Tierra del Fuego Province). Several countries maintain research stations on the islands. Most of them are situated on King George Island, benefitting from the airfield of the Chilean base Eduardo Frei. There are sixteen research stations in different parts of the islands, with Chilean stations being ...
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Foreland Point
Foreland Point is a rocky headland in Devon near Lynmouth, and is the most northerly point along the Devon and Exmoor coast. The highest cliff is above the high tide, although the highest point of the entire headland is near Countisbury (a village around a mile away) at . The headland is owned by the National Trust; some areas are open to public access all year, as part of the South West Coast Path, while other areas have limited access. The Trinity House-operated Lynmouth Foreland Lighthouse is also located here. The area of the sea between Bideford and Foreland Point is a Marine Conservation Zone A Marine Conservation Zone (MCZ) is a type of marine nature reserve in UK waters. They were established under the Marine and Coastal Access Act (2009) and are areas designated with the aim to protect nationally important, rare or threatened habit .... References Headlands of Devon Bristol Channel Protected areas of Devon National Trust properties in Devon {{Dev ...
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Alpine Foreland
The Alpine Foreland, less commonly called the Bavarian Foreland,Dickinson, Robert E (1964). ''Germany: A regional and economic geography'' (2nd ed.). London: Methuen, pp. 585-586. . Bavarian Plateau or Bavarian Alpine Foreland (german: Bayerisches Alpenvorland), refers to a triangular region of plateau and rolling foothills in Southern Germany, stretching from Lake Constance in the west to beyond Linz on the Danube in the east, with the Bavarian Alps forming its south boundary and the Danube its northern extent. Geography The Alpine Foreland has been shaped under the influence of the ice ages and has a rich variety of landforms. A molasse basin of extensive Tertiary and Quaternary sediments —silt and clay, sand and sedimentary rocks from Alpine erosion— overlay the Alpine nappes. Features such as the morainic hills, gravel sandar and lakes have left a record of various glaciation stages in this region. The Alpine Foreland is crossed by the rivers Iller, Wertach, Lech, Isar a ...
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North And South Foreland
North Foreland (TR 39860 69616 ) and South Foreland (TR 35909 43307 {{Coord, 51.14040, 1.37110, display=inline, format=dms) are two chalk headlands on the Kent coast of southeast England. See: * North Foreland *South Foreland South Foreland is a chalk headland on the Kent coast of southeast England. It presents a bold cliff to the sea, and commands views over the Strait of Dover. It is centred northeast of Dover and 15 miles south of North Foreland. It includes ... Headlands of Kent ...
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