Barrier-island
landforms are common on many wave-dominated shoreline systems around the world,
and ancient analogs form important petroleum reservoirs. In this study, Seminack and Buynevich
use ground-penetrating radar (GPR), sediment cores and dating to understand the
facies architecture and evolution of shoreline and inlet systems of Assateague
Island, MD, and to test the notion that it is related to the historical Green
Run Inlet, located approximately 3 km to the south. The authors suggest that a ‘traditional’ survey of relict
inlets would have overlooked the study site due, to its lack of surficial
evidence of inlet existence, and that the results illustrate the value of a
multi-technique approach to study of inlet dynamics. These results illustrate how reconstructing the facies
architecture and evolutionary pathways of inlet-barrier island systems provide
enhanced understanding of their geological evolution and stratigraphic framework,
as well as their possible influence on coastal hazards.
Sedimentological and Geophysical Signatures of A Relict Tidal Inlet Complex Along A Wave-Dominated Barrier: Assateague Island, Maryland, U.S.A. by Christopher T.
Seminack and Ilya V. Buynevich
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