87 Marine/Coastal Science (Posters)
GEOLOGIC MAPPING OF BOSTON HARBOR AND APPROACHES
Paper number: 87-6
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Bradford ButmanU.S. Geological Survey, Woods Hole, MA
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Walter BarnhardtU.S. Geological Survey, Woods Hole, MA
Abstract
Six seafloor map units were defined based on bathymetric relief, depth, slope, acoustic backscatter, and analyses of sediment samples and photographs of the sea floor. Boston Harbor is a formerly glaciated landscape with numerous drumlins (harbor islands) separated by submarine channels. The seafloor morphology varies from gently sloping sub-tidal flats to areas of rugged elevated topography. The seabed of the Inner and Outer Harbor is typically fine-grained sediments and has been extensively dredged for navigation purposes. The harbor approaches are characterized by rugged topography created by exposed bedrock and boulders, and areas of smooth topography that are generally composed of sand. Many anthropogenic features (e.g. tunnels, dredge spoil dumps, shipwrecks) are resolved by the high-resolution (2 meters/pixel) data.