skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Shoreline erosion and wetland loss in Mississippi

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:6053348
 [1];
  1. Mississippi State Univ., Mississippi State (USA)

Set within a geologic framework that includes Pleistocene and Holocene barrier complexes, estuarine bays, and fluvio-deltaic tidal wetlands, coastal Mississippi shares environmental problems of shoreline erosion and wetland loss with her neighboring Gulf Coast states. The mainland coast consists of several Pleistocene headlands and barrier complexes interspersed with the St. Louis Bay and Back Bay of Biloxi estuaries. Tidal wetlands are found in the protected bays and tributary streams, as well as in the Pleistocene/Holocene deltaic environments associated with the Escatawpa, Pascagoula, Pearl, and Mississippi fluvial systems. Four barrier islands, formed by erosion and modification of a late Pleistocene/Holocene beach ridge, lie 6 to 12 mi offshore. Historically, these islands with a combined length of 30 mi have both migrated westward in response to prevailing longshore currents and also transgressed across the shallow platform of Mississippi Sound. Wave erosion, both normal and storm-induced, has historically caused shoreline retreat on both the barrier islands and on the mainland. Erosion rates in excess of 30 ft/yr have been measured at the updrift ends of the barrier islands while accretion has characterized the downdrift ends. Net shoreline retreat rates of 6 ft/yr have been measured on the Gulf side of the islands, although the Sound side rates are nearly as high. Since the earliest accurate maps were made in 1848, Mississippi's barrier islands have experienced a 20% reduction in area, amounting to about 2,000 acres (800 ha). Mainland shoreline retreat rates are similarly high, except for along the more stable and now artificially nourished beaches of Harrison County. Erosion rates exceeding 10 ft/yr since 1940 have been noted at the Point aux Chenes headland and the Grand Batture Islands. These islands, which formerly sheltered valuable oyster grounds and protected fragile marshes, have been reduced to shoals over the last several decades.

OSTI ID:
6053348
Report Number(s):
CONF-9010204-; CODEN: AABUD
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (USA), Vol. 74:9; Conference: Gulf Coast Association of Geological Societies and Gulf Coast Section of SEPM (Society of Economics, Paleontologists, and Mineralogist) meeting, Lafayette, LA (USA), 17-19 Oct 1990; ISSN 0149-1423
Country of Publication:
United States
Language:
English

Similar Records

Late Holocene coastal wetlands change, Mississippi Sound, Alabama: Short-term vs. long-term patterns and processes
Conference · Tue Mar 01 00:00:00 EST 1994 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:6053348

Gulf coastal Pleistocene units and time stratigraphy; reevaluation and problems of Atlantic correlation
Conference · Mon Mar 01 00:00:00 EST 1993 · Geological Society of America, Abstracts with Programs; (United States) · OSTI ID:6053348

Development of tidal inlet on Mississippi River deltaic plain
Conference · Thu Sep 01 00:00:00 EDT 1983 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:6053348