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The shallow subsurface of Grand Marais headland beach, located along the southern shore of Lake Superior, Michigan, was imaged using ground penetrating radar (GPR) to determine how seasonal storm impacts are manifested in subsurface depositional architectures. This study was designed to evaluate the implications of the 1883 emplacement of a jetty system that allows for accumulation of sand from the westerly Grand Sable dunes, which would otherwise be transported further east as a result of longshore drift. Due to the jetty and previous research, there is an indication that the beach is growing.

GPR EXAMINATION OF MULTI-YEAR SEASONAL STORM IMPACTS ON SUBSURFACE DEPOSITIONAL ARCHITECTURES ON A BEACH IN GRAND MARAIS, MI