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The Sandettie Bank (French: Banc de Sandettié) is an elongated sandbank in the North Sea, more specifically about in the middle of the eastern entrance of the Strait of Dover. North-western of it are the most dangerous Goodwin Sands, south of it the sandbank Ruytingen. The shoal represents a significant threat to the major shipping lanes in the Strait of Dover. From 1902 to 1989 it was marked by a succession of French lightships, all bearing the name ''Sandettié'' while deployed there. The last such manned lightship is now a museum ship at the Port Museum of Dunkirk at anchor.〔:fr:Sandettié (bateau-feu)〕 Today the British authority Trinity House maintains an unmanned lightship, the Sandettie Light Vessel Automatic there. The ship also has an Automatic Weather Station.〔http://www.trinityhouse.co.uk/lighthouses/light_vessels/sandettie_lightvessel.html〕 == Geology == Tertiary strata form the basement in the Sandettie Bank. In the northwest part of the area erosion cut a basin in the Tertiary strata. This basin is filled with a sequence of late Pleistocene sands overlain by Holocene sands which form the major topographic features of the Sandettie. The surface of the banks are moulded into transverse ridges up to 10m in amplitude and 200m in wavelength. There are three types of ridges present: # At the north end, linear transverse ridges of irregular amplitude and wavelength occur with a flint gravel base grading up into medium sand. These ridges are fossil features of Preboreal-Subboreal age. # At the south end are symmetrical sandwaves of regular amplitude and wavelength which appear to be stable. # To the west of Sandettie Bank there are south-facing asymmetrical sandwaves which are potentially mobile and which later sedimentological investigations revealed to be moving southwards in one area.〔(R. Kirby and E. Oele: The Geological History of the Sandettie-Fairy Bank Area, Southern North Sea ); 30. August 2014〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Sandettie Bank」の詳細全文を読む スポンサード リンク
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