12 Coastal Processes and Geologic Framework: Insights from Geological and Geophysical Surveys across the Continental Margin (Posters)

Thursday, 31 March 2016
8:00 AM - 5:30 PM
Exhibit Hall


REGIONAL FRAMEWORK, PALEODRAIANGE AND HABITAT CHARACTERIZATION OF THE MID-SOUTH CAROLINA CONTINENTAL SHELF: WINYAH BAY TO CAPE ROMAINE

Paper number: 12-5
Program: Theme Sessions
Time: 8:00 AM – 5:30 PM


Authors


Abstract

A regional geophysical survey of the inner continental shelf off central South Carolina was completed on a cooperative cruise between NOAA and Coastal Carolina University in July 2015. An integrated mapping suite comprised of subbottom echosounder, side scan, multibeam and split beam sonars was used to define the regional geologic framework, including paleodrainage patterns across the shelf and to identify potential fish habitat locations that will provide additional inputs to a thematic habitat mapping routine developed by NOAA. Initial results from the thematic mapper characterization suggest that large-scale framework elements such as paleochannel networks may play a role in determining benthic habitat distribution. Several large paleo-fluvial valleys that are likely associated with the ancestral Santee and Pee Dee River systems are observed in the subbottom data and appear to correlate with broad topographic lows identified by the thematic habitat mapping routine. The collective dataset will provide opportunity to locally evaluate and provide a basis to refine the regional habitat mapping routine. Additional geophysical survey is scheduled for summer 2016 to connect the onshore and offshore framework and to further refine channel fill geometries, bottom habitat and Holocene reworking of the shelf system.

Geological Society of America Abstracts with Programs. Vol. 48, No. 3

doi: 10.1130/abs/2016SE-273345

© Copyright 2016 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.