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Near the southern tip of the Picayune Bluffs, a great deal of alluvial fan soil and several interconnected, eroding dunes have been displaced by Hurricane Katrina to form an anomalous sand ridge. When measured from the ground, this ridge is almost as wide as the Mississippi River Delta and more than three times the width of the Mississippi as it flows along a southeastern Gulf of Mexico shoreline, leaving little room for the river to carve a channel into it. In fact, the tallest bluff is called “the Pier” and overlooks the Mississippi River Terminal.

Sand ridges form from long-standing, underlying alluvial deposits, which have accumulated through the slow weathering of the underlying rock. As the sediment-laden water from the primary river courses fills the basin and rises above the level of the surrounding uplands (e.g., land between a river and the sea), the sediment becomes compressed and accumulated into an often bowl-shaped mound or dune, which eventually reaches its present height. The sand of an alluvial fan can also accumulate on the downwind side of bluffs and dunes, and in upland lake drainages, thereby lengthening and increasing the size of this coastal ridge.

Coastal sedimentary features like dunes, bluffs, alluvial fans, and beach ridges have been created throughout the Great Lakes region. Small in comparison to some of the features in the Gulf Coast’s Mississippi River Delta, these coastal deposits add to the dramatic beauty

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