|
|
Physical Agents of Land Loss: Sediment Budget
Changes in Sediment SupplySeveral thousand years ago the principal suppliers of sediment to most non-cliffed coasts were either rivers that delivered sand directly to the beach or nearshore currents that transported sand onshore from the continental shelf. Once at the coastline the sand was redistributed by alongshore currents. The presence of sandy beach-ridges and barrier islands on both Atlantic and Gulf coasts indicate that sand supply was plentiful and beaches were building seaward as sea level approached its current position several thousand years ago. Since then, sediment supplied by some coastal rivers and the continental shelf has naturally diminished as a result of climatic changes and adjustments of the inner shelf profile. Humans have also contributed significantly to the deficit in sediment supply by damming rivers, building seawalls, groins, and jetties, and dredging tidal inlets. These natural and artificial reductions in coastal sediment supply have resulted in the erosion of many beaches, barrier islands, and deltas. Today the only remaining source of sediment for many coastal compartments is local erosion of nearby beaches and bluffs. |