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The southern coast of Louisiana in the United States is among the fastest-disappearing areas in the world.This has largely resulted from human mismanagement of the coast (see Wetlands of Louisiana).

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The Gulf of Mexico did not exist 250 million years ago when there was but one supercontinent, Pangea.

As Pangea split apart, the Atlantic Ocean and Gulf of Mexico opened.

There has never been an official language in Louisiana, and the state constitution enumerates "the right of the people to preserve, foster, and promote their respective historic, linguistic, and cultural origins," whether English, French, Spanish, or otherwise.

The suffix -ana (or -ane) is a Latin suffix that can refer to "information relating to a particular individual, subject, or place." Thus, roughly, Louis ana carries the idea of "related to Louis." Once part of the French Colonial Empire, the Louisiana Territory stretched from present-day Mobile Bay to just north of the present-day Canada–United States border, including a small part of what is now the Canadian provinces of Alberta and Saskatchewan.

In the uplands and hills, the elevations rise to Driskill Mountain, the highest point in the state at only 535 feet (163 m) above sea level. The state also has political jurisdiction over the approximately 3-mile (4.8 km)-wide portion of subsea land of the inner continental shelf in the Gulf of Mexico.

Through a peculiarity of the political geography of the United States, this is substantially less than the 9-mile (14 km)-wide jurisdiction of nearby states Texas and Florida, which, like Louisiana, have extensive Gulf coastlines.Much of the state's lands were formed from sediment washed down the Mississippi River, leaving enormous deltas and vast areas of coastal marsh and swamp.These contain a rich southern biota; typical examples include birds such as ibis and egrets.The oldest rocks date back to the early Cenozoic Era, some 60 million years ago.The history of the formation of these rocks can be found in D. The youngest parts of the state were formed during the last 12,000 years as successive deltas of the Mississippi River: the Maringouin, Teche, St.Bernard, Lafourche, the modern Mississippi, and now the Atchafalaya.

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