|
Varne Sandbank
The Varne Bank or Varne Shoal is a long sand bank in the Strait of Dover, lying southwest of Dover in Kent, England. With the Lobourg Channel running along it, the Varne bank lies immediately south-west of the deepest point in the strait of Dover. Its rectilinear shape is similar to other banks in the strait such as South Falls bank bordering the Lobourg Channel on the east, the Colbart bank (a.k.a. the Ridge) and others. Rectilinear-shaped banks are only present on the English side of the strait. Lying almost in the middle of the south/west international traffic English-side channel of the English Channel, the Varne Bank is a constant concern for both British coastguards and shipping. The sea above it presents strong rippling, especially when strong tides occur, and is noted for its extra roughness during bad weather.Ogden C. K.''Sailing directions for the north coast of France from cape Griz-Nez to cape Levi'' 1908. (search for the words "Varne shoal".) ''archive.org/stre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand Bank
In oceanography, geomorphology, and geoscience, a shoal is a natural submerged ridge, bank, or bar that consists of, or is covered by, sand or other unconsolidated material and rises from the bed of a body of water to near the surface. It often refers to those submerged ridges, banks, or bars that rise near enough to the surface of a body of water as to constitute a danger to navigation. Shoals are also known as sandbanks, sandbars, or gravelbars. Two or more shoals that are either separated by shared troughs or interconnected by past or present sedimentary and hydrographic processes are referred to as a shoal complex.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. The term ''shoal'' is also used in a number of ways that can be either similar or quite different from how it is used in geologic, geomorphic, and oceanographic literature. Sometimes, this term refe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Channel Tunnel
The Channel Tunnel (french: Tunnel sous la Manche), also known as the Chunnel, is a railway tunnel that connects Folkestone (Kent, England, UK) with Coquelles ( Hauts-de-France, France) beneath the English Channel at the Strait of Dover. It is the only fixed link between the island of Great Britain and the European mainland. At its lowest point, it is deep below the sea bed and below sea level. At , it has the longest underwater section of any tunnel in the world, and is the third longest railway tunnel in the world. The speed limit for trains through the tunnel is . The tunnel is owned and operated by the company Getlink, formerly "Groupe Eurotunnel". The tunnel carries high-speed Eurostar passenger trains, the Eurotunnel Shuttle for road vehicles and international freight trains. It connects end-to-end with the high-speed railway lines of the LGV Nord in France and High Speed 1 in England. In 2017, through rail services carried 10.3 million passengers and 1.2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thanet , in the ICS Geologic timescale, the latest age or uppermost stratigraphic stage of the Paleocene Epoch
{{disambiguation ...
Thanet may refer to: *Isle of Thanet, a former island, now a peninsula, at the most easterly point of Kent, England *Thanet District, a local government district containing the island *Thanet College, former name of East Kent College *Thanet Canal, a short branch of the Leeds and Liverpool Canal *Earl of Thanet, a title in the Peerage of England created in 1628 *Thanet Formation, a geological formation found in the London Basin of southeastern England * HMS ''Thanet'' (H29), an S-class destroyer of the Royal Navy See also *Thanetian The Thanetian is, in the ICS Geologic timescale, the latest age or uppermost stratigraphic stage of the Paleocene Epoch or Series. It spans the time between . The Thanetian is preceded by the Selandian Age and followed by the Ypresian Age ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dover District
Dover is a local government district in Kent, England. The port town of Dover is its administrative centre. It was formed on 1 April 1974 by the merger of the boroughs of Deal, Dover, and Sandwich along with Dover Rural District and most of Eastry Rural District. Settlements There are three towns within the district: Deal, Dover and Sandwich; and the parishes below: * Alkham * Ash * Aylesham * Capel-le-Ferne * Denton with Wootton * Eastry * Eythorne * Goodnestone * Great Mongeham * Guston * Hougham Without * Langdon * Lydden * Nonington * Northbourne * Preston * Ringwould with Kingsdown * Ripple * River * Shepherdswell with Coldred * Sholden * St Margaret's at Cliffe * Staple * Stourmouth * Sutton * Temple Ewell * Tilmanstone * Walmer * Whitfield * Wingham * Woodnesborough * Worth The northern boundary of the district is the River Stour; on its western side is the district of Canterbury; to the south the parish of Capel-le-Ferne; and to the east the St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Kent
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dune
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called '' ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pas De Calais
The Strait of Dover or Dover Strait (french: Pas de Calais - ''Strait of Calais''), is the strait at the narrowest part of the English Channel, marking the boundary between the Channel and the North Sea, separating Great Britain from continental Europe. The shortest distance across the strait, at approximately 20 miles (32 kilometres), is from the South Foreland, northeast of Dover in the English county of Kent, to Cap Gris Nez, a cape near to Calais in the French département of Pas-de-Calais. Between these points lies the most popular route for cross-channel swimmers. The entire strait is within the territorial waters of France and the United Kingdom, but a right of transit passage under the United Nations Convention on the Law of the Sea allows vessels of other nations to move freely through the strait. On a clear day, it is possible to see the opposite coastline of England from France and vice versa with the naked eye, with the most famous and obvious sight being the Wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natura 2000
Natura 2000 is a network of nature protection areas in the territory of the European Union. It is made up of Special Areas of Conservation and Special Protection Areas designated under the Habitats Directive and the Birds Directive, respectively. The network includes both terrestrial and Marine Protected Areas. History In May 1992, the governments of the European Communities adopted legislation designed to protect the most seriously threatened habitats and species across Europe. The Habitats Directive complements the Birds Directive adopted earlier in 1979 and together they make up the Natura 2000 network of protected areas. The Birds Directive requires the establishment of Special Protection Areas for birds. The Habitats Directive similarly requires Sites of Community Importance which upon the agreement of the European Commission become Special Areas of Conservation to be designated for species other than birds, and for habitat types (e.g. particular types of forest, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Battle Of Dover Strait (1917)
The Second Battle of Dover Strait was a naval battle of the First World War, fought in the Dover Strait in April 1917 and should not be confused with the major Battle of Dover Strait in 1916. Two Royal Navy destroyers defeated a superior force of German ''Kaiserliche Marine'' torpedo boats. Two German torpedo boats were sunk; the British suffered damage to both destroyers. Background On 20 April 1917, two groups of torpedo boats of the German Navy raided the Dover Strait to bombard Allied positions on shore and to engage warships patrolling the Dover Barrage— the field of floating mines that prevented German ships from getting into the English Channel. Six torpedo boats bombarded Calais and another six bombarded Dover just before midnight. Battle Two flotilla leaders of the Royal Navy — and — were on patrol near Dover and engaged six of the German ships early on 21 April near the Goodwin Sands. In a confusing action, ''Swift'' torpedoed . ''Broke'' rammed , and the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Battle Of Dungeness
The naval Battle of Dungeness took place on 30 November 1652 (10 December in the Gregorian calendar) during the First Anglo-Dutch War near the cape of Dungeness in Kent. Background In September 1652 the government of the Commonwealth of England, the Council of State, mistakenly believing that the United Provinces after their defeat at the Battle of the Kentish Knock would desist from bringing out a fleet so late in the season, sent away ships to the Mediterranean and the Baltic. At the same time the largest English vessels remained in repair and active ships were undermanned as sailors deserted or rioted because their wages were in arrears. This left the English weakened and badly outnumbered in home waters. Meanwhile, the Dutch were making every effort to reinforce their fleet. Dutch trade interests demanded that their navy would make a final effort to convoy merchantmen to the south. Battle On 21 November 1652 Old Style, 1 December New Style, Lieutenant-Admiral Maar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Battle Of Dover (1652)
The naval Battle of Dover (also known as the Battle of Goodwin Sands), fought on 19 May 1652 (29 May 1652 Gregorian calendar), was the first engagement of the First Anglo-Dutch War between the navies of the Commonwealth of England and the United Provinces of the Netherlands. Background The English Parliament had passed the first of the Navigation Acts in October 1651, aimed at hampering the shipping of the highly trade-dependent Dutch. Agitation among the Dutch merchants had been further increased by George Ayscue's capture in early 1652 of 27 Dutch ships trading with the royalist colony of Barbados in contravention of an embargo. Both sides had begun to prepare for war, but conflict might have been delayed if not for an unfortunate encounter on 29 May 1652 (19 May in the Julian calendar then in use in England) near the Straits of Dover between a Dutch convoy escorted by 40 ships under Lieutenant-Admiral Maarten Tromp and an English fleet of 25 ships under General-at-Sea Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Landforms Of Kent")
