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Seeing the Bottom Provides a New Perspective and Complements Multibeam Surveys
The Massachusetts Bay segment of the ISABEL S. cruise was sandwiched within a longer (2-week) cruise carried out by Page to obtain similar observations in the Stellwagen Bank National Marine Sanctuary. Laura Hayes, Jeremy Malczyk, Nancy Soderberg, and David Walsh were also participants in the Mass Bay leg. The objective of the cruise was to provide direct observations of the sea floor to help interpret the backscatter and shaded-relief images produced by multibeam surveys. The video observations changed the way we think about the sea floor in Mass Bay. High-backscatter areas ranged from gravel pavement, cobbles, boulders, pipe clay, coarse sand with large bedforms, dumps of dredge and construction material, to clay fragments beneath a smooth surface, etc. Some of these interpretations could be made from the spatial patterns of the backscatter, but some were a surprise.
One of the advantages of differential GPS and calm weather was that we were able to investigate some of the 10- to 100-m-scale features shown in the multibeam backscatter and shaded-relief images. Prior to the cruise, we hypothesized some of the meandering channels to be glacial outwash streams formed at lower stands of sea level. The video observations showed that they were floored with rounded cobbles, confirming the hypothesis. Offshore of Scituate, high-backscatter features trending downslope turned out to be extremely coarse well-sorted sand (the sediment had the texture of grapenuts!) that was formed into large megaripples; the transition between these features and the adjacent muddy bottom occurred over a few meters. The processes that form and maintain these features are unclear. What appeared to be 'pinnacles' in the shaded-relief images turned out to be spectacular outcropping bedrock. All of the submerged 'drumlins' shallower than about 25 m had a distinctly different biological communitypurple and yellow calcareous algae, kelp, etc.compared to those deeper than 25 m. In short, the backscatter data from multibeam show the spatial patterns, but interpretation benefits greatly from seeing the bottoma picture is worth a thousand words (well maybe a few pixels)! The direct visual observations complement the multibeam data and demonstrate the value of using different tools that image at different spatial scales.
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