Sonography of a glaciated continental shelf
Abstract
Sonographs of the inner continental shelf off Halifax, Nova Scotia, show a large part of the inner shelf area consisting of exposed bedrock in which the inferred sequence of structural events is clearer than the record on land. Ribbed moraines overlie eroded drumlins and provide new information on the deglaciation history. Morphologic features allow a precise definition of the maximum postglacial lowstand of sealevel at -65 to -70 m. A 1000 km2 area in eastern Canada was surveyed with a multibeam sounder EM100, manufactured by Simrad of Norway. A 100% coverage of the sea floor was achieved with 50 to 100 m track spacing, and position control was achieved using the differential global positioning system (DGPS) with an accuracy of 1-2 m.
Data were corrected for ship motion, gridded at a 10 m spacing, and displayed as obliquely illuminated relief image. The sonograph revealed characteristics of the sea bed in detail for the interpretation of bedrock and surficial structures and processes. The bathymetric images may be more useful for geologic mapping than air photographs and satellite images on nearby land, where vegetation commonly obscures the geologic features.
Department
Center for Coastal and Ocean Mapping
Publication Date
8-1-1994
Journal Title
Geology
Publisher
Geological Society of America
Digital Object Identifier (DOI)
https://dx.doi.org/10.1130/0091-7613(1994)022<0747:SOAGCS>2.3.CO;2
Document Type
Article
Recommended Citation
Loncarevic, B.D., Courtney, R.C., Fader, Giles, Piper, Costello, Hughes Clarke, and Stea, 1994, Sonography of a glaciated continental shelf: Geology, v.22, p.747-750.