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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.These contain a rich southern biota; typical examples include birds such as ibis and egrets.Many came from peoples of the same region of West Africa, thus concentrating their culture.In the post-Civil War environment, Anglo-Americans increased the pressure for Anglicization, and in 1921, English was for a time made the sole language of instruction in Louisiana schools before a policy of multilingualism was revived in 1974.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.Louisiana's capital is Baton Rouge and its largest city is New Orleans. The largest parish by population is East Baton Rouge Parish, and the largest by total area is Plaquemines.
The breadth of the alluvial region along the Mississippi is from 10 to 60 miles (15 to 100 km), and along the other rivers, the alluvial region averages about 10 miles (15 km) across.
Before the American purchase of the territory in 1803, the current Louisiana State had been both a French colony and for a brief period, a Spanish one.
In addition, colonists imported numerous African people as slaves in the 18th century.
The sediments were carried from north to south by the Mississippi River.
In between the Tertiary rocks of the north, and the relatively new sediments along the coast, is a vast belt known as the Pleistocene Terraces.