The oldest deposits in Louisiana date from the Eocene Epoch, marked by the darkest gold color. Narrow strips of younger rocks crop out along their southern edge, dating from Oligocene (light tan) and Miocene (dark tan) times. The speckled yellow pattern marks areas of Pliocene rocks of terrestrial origin, older versions of the wide Pleistocene terraces (lightest yellow) that cover southern Louisiana.
The older outcrops dip downward toward the sea owing to the steady subsidence of the land, and the coast is very young indeed. You can see how much the Holocene alluvium of the Mississippi River (gray) covers the state. The Holocene represents only the latest 10,000 years of Earth history, and in the 2 million years of Pleistocene time before that the river has wandered over the whole coastal region many times.
Human engineering has temporarily tamed the river, most of the time, and it's no longer dumping its sediment all over the place. As a result, coastal Louisiana is sinking out of sight, starved of fresh material. This is not permanent country.
More Louisiana resources on About.com:
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Louisiana Geography, State Symbols & Facts
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Louisiana French
Louisiana Hotels
Louisiana Archaeology


