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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.

Louisiana is bordered by Arkansas to the north, Mississippi to the east, Texas to the west, and the Gulf of Mexico to the south.

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.

In general, the northern terraces have had sufficient time for rivers to cut deep channels, while the newer terraces tend to be much flatter. Their origin can be traced back to the early Gulf of Mexico, when the shallow ocean had high rates of evaporation.

There are several hundred salt domes in the state; one of the most familiar is Avery Island.

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).

The oldest rocks date back to the early Cenozoic Era, some 60 million years ago.