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The Gulf of Mexico (Spanish: Golfo de México) is an oceanic basin and a marginal sea of the Atlantic Ocean, [3] [4] mostly surrounded by the North American continent. [5] It is bounded on the northeast, north, and northwest by the Gulf Coast of the United States; on the southwest and south by the Mexican states of Tamaulipas, Veracruz, Tabasco, Campeche, Yucatán, and Quintana Roo; and on the ...
The four kinds of navigable water in the Gulf of Mexico. Maritime geography is a collection of terms used by naval military units to loosely define three maritime regions: brown water , green water , and blue water .
Gulf Stream. The Gulf Stream, together with its northern extension, North Atlantic Current, is a powerful, warm, and swift Atlantic Ocean current that originates in the Gulf of Mexico, exits through the Strait of Florida, and follows the eastern coastlines of the United States and Newfoundland to the northeast before crossing the Atlantic Ocean.
The Gulf Stream proper is a western-intensified current, driven largely by wind stress. [10] In 1958, oceanographer Henry Stommel noted, "very little water from the Gulf of Mexico is actually in the stream". [11] The North Atlantic Current, in contrast, is largely driven by thermohaline circulation. Its carrying warm water northeast across the ...
A woman in Washington, D.C., may call it one thing. A guy living off a main square in Mexico City might call it another. But a tug of war over referring to the immense body of water off the coast ...
The main ocean basins are the ones named in the previous section. These main basins are divided into smaller parts. Some examples are: the Baltic Sea (with three subdivisions), the North Sea, the Greenland Sea, the Norwegian Sea, the Laptev Sea, the Gulf of Mexico, the South China Sea, and many more. The limits were set for convenience of ...
The American Mediterranean Sea is a scientific name for the mediterranean dilution basin that includes the Caribbean Sea and the Gulf of Mexico. [1]: 15, 35, 637–643 [2] The name, which has been employed particularly by German oceanographers, is not recognized by the USGS, the International Hydrographic Organization or other international hydrological bodies.
Beneath the sediments of the Gulf of Mexico basin, most of the pre-Triassic basement rocks are believed to be allochthonous thrust sheets sutured during the formation of Pangaea. [3] However, it was during the break-up of the supercontinent that the foundation for the Gulf of Mexico sediments would be laid.