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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 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 ...
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.
The system's new description for the Gulf, an ocean basin that shares nearly equal lengths of shoreline with the U.S. and Mexico, reads: "The Gulf of America, formerly known as the Gulf of Mexico ...
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 ...
Oceanography (from Ancient Greek ὠκεανός (ōkeanós) 'ocean' and γραφή (graphḗ) 'writing'), also known as oceanology, sea science, ocean science, and marine science, is the scientific study of the ocean, including its physics, chemistry, biology, and geology.
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.
The Pacific Ocean is also an active, shrinking oceanic basin, even though it has both spreading ridge and oceanic trenches. Perhaps the best example of an inactive oceanic basin is the Gulf of Mexico, which formed in Jurassic times and has been doing nothing but collecting sediments since then. [15]