Figure 9.
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Schematic representation during the formation of Lake
Pontchartrain as sea-level rose. (A) The Louisiana area was emergent during the late Wisconsinan lowstand, ~18k yrs BP; (B) as sea-level rise neared present levels the Pine Island Barrier developed, ~6k yrs BP; (C) sea-level rise slows and a relatively short stillstand initiates development of the Pine Island Spit and forming the Pontchartrain Embayment, ~5k yrs BP; and (D) a subdelta of the Mississippi River the St. Bernard progrades across the area (E) forming Lake Pontchartrain and associated lakes. |
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