Item talk:Q239475
From geokb
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"abstract": "The U.S. Geological Survey and the National Oceanographic and Atmospheric Administration conducted\r\ngeophysical and hydrographic surveys, respectively, along the inner-continental shelf of Fenwick and\r\nAssateague Islands, Maryland and Virginia over the last 40 years. High resolution bathymetry and backscatter\r\ndata derived from surveys over the last decade are used to describe the morphology and presence of sand ridges\r\non the inner-continental shelf and measure the change in the position of smaller-scale (10\u2013100 s of meters)\r\nseafloor features. Bathymetric surveys from the last 30 years link decadal-scale sand ridge migration patterns to\r\nthe high-resolution measurements of smaller-scale bedform features. Sand ridge morphology on the inner-shelf\r\nchanges across-shore and alongshore. Areas of similar sand ridge morphology are separated alongshore by\r\nzones where ridges are less pronounced or completely transected by transverse dunes. Seafloor-change analyses\r\nderived from backscatter data over a 4\u20137 year period show that southerly dune migration increases in\r\nmagnitude from north to south, and the east-west pattern of bedform migration changes ~ 10 km north of the\r\nMaryland-Virginia state line. Sand ridge morphology and occurrence and bedform migration changes may be\r\nconnected to observed changes in geologic framework including topographic highs, deflated zones, and sand\r\navailability. Additionally, changes in sand ridge occurrence and morphology may help explain changes in the\r\nlong-term shoreline trends along Fenwick and Assateague Islands. Although the data presented here cannot\r\nquantitatively link sand ridges to sediment transport and shoreline change, it does present a compelling\r\nrelationship between inner-shelf sand availability and movement, sand ridge occurrence and morphology,\r\ngeologic framework, and shoreline behavior.",
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