2003 Seattle Annual Meeting (November 2–5, 2003)
Paper No. 180-13
Presentation Time: 4:30 PM-4:45 PM

MESOSCALE RESPONSE OF A MOBILE SEDIMENTARY SHORELINE: BASIS FOR NEW DIRECTIONS IN COASTAL MANAGEMENT AT THE COMMUNITY LEVEL; FALMOUTH, MA

WILBER, R. Jude, Capella Consulting Group, Woods Hole Road, Woods Hole, MA 02543, rjwilber@adelphia.net and BUSH, David M., Department of Geosciences, State Univ of West Georgia, Carrollton, GA 30118

Falmouth, MA, on the southern tip of Cape Cod, is a peninsular town with nearly 70 miles of salt-water coast including the south-facing (Vineyard Sound) shore; the west-facing (Buzzards Bay) shore; and numerous salt-water embayments with variable shoreline orientation. The Falmouth South Shore (FSS) presents a classic "river-of-sand" system with source area at glacio-tectonic uplands in the western sector. Littoral drift is uni-modal (west-to-east), delivering sand along the south-dipping, low-gradient, Mashpee outwash plain. This plain is dissected by numerous spring-sapped valleys which have been drowned during Holocene sea-level rise, enlarged to Carolina Bay-type entities by littoral "sculpting," and barred by lateral transport of sand.

In 1900, the FSS was a sedimentologically-responsive coast with clearly-defined meso-scale dynamics related to local forcing factors. The geophysical systematics and derivative organismal habitats have been severely altered in the 20th Century by continued building of coastal engineering structures; the current shoreline presents a condition of near-total armoring. Structures have impacted the river-of-sand in three ways: 1) shore-parallel structures (seawalls, revetment) "lock-out" sand at source areas; 2) groin fields "hold-out" sand from normal littoral transport and; 3) jetty pairs (at stabilized inlets, "cut-out" sand from the littoral stream on ebb tides.

A recent change in thinking may lead to entirely different directions in coastal zone management on the local and community scale. Along the entire 15-mile segment of the "open" south shore and the 5-mile system of Great Pond - Falmouth’s largest salt-water embayment, recommendations call for a phased, long-range plan of "whole-coastal restoration" designed to re-establish the shoreline to pre-1900 conditions. The Falmouth plans are closely aligned with and (in part) modeled on Martha’s Vineyard’s island-wide pre-facto "no-build buffer zone". If restoration proceeds, it will be the first time that coastal engineering structures have been removed from a significant stretch of stabilized and degraded USA shoreline in an effort to improve both aesthetic and environmental conditions.

2003 Seattle Annual Meeting (November 2–5, 2003)
Session No. 180
From the Abyss to the Beach: In Honor of Orrin H. Pilkey
Washington State Convention and Trade Center: 615/616/617
1:30 PM-5:30 PM, Tuesday, November 4, 2003

Geological Society of America Abstracts with Programs, Vol. 35, No. 6, September 2003, p. 469

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