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See also:MEXICO, GULF OF , a mediterranean gulf almost surrounded by the coasts of the See also:United States and Mexico, and forming the See also:northern See also:division of the See also:extension westward of the See also:west See also:Atlantic See also:trench (see ATLANTIC OCEAN). Its See also:southern boundary is defined by the partly submerged See also:ridge which extends eastwards from the See also:peninsula of See also:Yucatan, and on which the See also:island of See also:Cuba is situated: to the See also:east it communicates directly with the Atlantic by the Strait of See also:Florida. On the western See also:side of Yucatan a southerly embayment is formed by the Gulf of Campeachy. The United States See also:coast closely follows the parallel of 30° N., while the parallel of 200 N. cuts across the Gulf of Campeachy: the greatest length—See also:Vera Cruz to. Florida—is 1120 m., and greatest width—See also:Galveston to Campeachy—68o m. The See also:total See also:area is approximately 716,000 sq. in. The deepest See also:part of the Gulf of Mexico, the so-called " Sigsbee deep, lies below the See also:line of 2000 fathoms, between 23° and 251° N., and 842° to 95° W. It is widest to the west, where the breadth is about 120 m., and narrows to 25 M. at its greatest See also:depth (2119 fathoms) between 86° and 88° W., widening again to some 8o m. farther eastward. The See also:continental shelf is for the most part narrow: its breadth is 6 m. at Cape Florida, 120 M. along the west coast of Florida, ro m. at the See also:south pass of the See also:Mississippi, 130 M. near the boundary of See also:Texas and See also:Louisiana, and 15 M. off Vera Cruz. The shores are See also:low, sandy and marshy, the coast-line being frequently doubled by lagoons. There are no islands except the " Keys " of Florida and Yucatan, and Cuba. The tides in the Gulf of Mexico are of comparatively small range (springs rarely exceed 4 ft. and neaps 21 ft.), but a remarkable feature is the exaggeration of the diurnal inequality to such an extent as almost to extinguish the semi-diurnal See also:tide in the inner parts of the gulf, giving high and low See also:water only once daily. The mean level of the water in the Gulf of Mexico was formerly given as about 40 in. .above that of mean See also:sea-level at New See also:York, but later reports on precise levellings from New York to See also:Biloxi through St See also: Additional information and CommentsThere are no comments yet for this article.
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