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A continental shelf is a portion of a continent that ... Sovereign rights over their continental shelves down to a depth of ... UNEP Shelf Programme; GEBCO world map ...
Detailed relief map of the United States continental shelf in south Alaska, including US extended continental shelf claims. In the Bering Sea, the large Bering Shelf dominates the area, stretching over 300 nautical miles from southwest mainland Alaska, at a depth of around 500 metres. [3]
The continental shelf is the relatively shallow water area found in proximity to continents; it is the portion of the continental margin that transitions from the shore out towards to ocean. Continental shelves are believed to make up 7% of the sea floor. [3] The width of continental shelves worldwide varies in the range of 0.03–1500 km. [4]
The Gulf of Maine is considered to be a relatively deep body of water, with an average depth of 490 feet (150 meters) and a maximum depth of 1236 feet (377) meters. Its southern border is defined by the Georges Bank, a shallow underwater plateau located offshore that forms a basin in the central Gulf of Maine.
Continental shelves appear mostly by a depth of 140 meters, mid-ocean ridges by 3000 meters, and oceanic trenches at depths beyond 6000 meters. A seafloor map captured by NASA Bathymetry ( / b ə ˈ θ ɪ m ə t r i / ; from Ancient Greek βαθύς ( bathús ) 'deep' and μέτρον ( métron ) 'measure') [ 1 ] [ 2 ] is the study of ...
The Gulf of Mexico is 41% continental slope, 32% continental shelf, and 24% abyssal plain with the greatest depth of 12,467 feet in the Sigsbee Deep. [43] Seven main areas are given as: [citation needed] Gulf of Mexico basin contains the Sigsbee Deep and can be further divided into the continental rise, the Sigsbee Abyssal Plain, and the ...
It extends from the low tide mark to the edge of the continental shelf, with a relatively shallow depth extending to about 200 meters (660 feet). Above the neritic zone lie the intertidal (or eulittoral) and supralittoral zones; below it the continental slope begins, descending from the continental shelf to the abyssal plain and the pelagic zone.
Outer Continental Shelf limits greater than 200 nautical miles but less than either the 2,500-meter isobath plus 100 nmi or 350 nmi are defined by a line 60 nautical miles (111.1 km; 69.0 mi) seaward of the foot of the continental slope or by a line seaward of the foot of the continental slope connecting points where the sediment thickness ...