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- W113454767 abstract "Washover sands deposited by storm surge during Superstorm Sandy along the bay side of Fire Island at Tiana Beach, NY were cored and sampled for grain size analysis. Washover sands at all coring sites exhibited an overall coarsening upward trend, with mean grain sizes varying from 0.25 mm (2 phi) to 0.5 mm (1 phi) from the base to the top of the overwash lobe. Comparison of grain size distributions between washover sands and sands collected from foreshore, berm, backshore, and dune features on the modern ocean beach shows that washover sands are most similar in grain size characteristics to dune sands, particularly near the base of the lobe, but become increasingly similar to beach sands near the top of the lobe. Four sand intervals within a core collected through pre-Sandy marsh deposits at Tiana Beach can be ascribed to overwash from three historical storms (1938 and 1954 hurricanes, 1965 nor’easter) and one unidentified storm based on historical air photographs of the coring site and grain size characteristics. Comparison of grain size characteristics between the historical washover sand layers in core and recent Superstorm Sandy washover sands shows that they share consistent grain size trends that can be used to distinguish washover sands in sediment core from sands deposited by other processes in this and similar barrier island depositional systems." @default.
- W113454767 created "2016-06-24" @default.
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- W113454767 date "2015-01-01" @default.
- W113454767 modified "2023-09-22" @default.
- W113454767 title "Recognizing Past Storm Events in Sediment Cores Based on Comparison to Recent Overwash Sediments Deposited by Superstorm Sandy" @default.
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- W113454767 doi "https://doi.org/10.1016/b978-0-12-801520-9.00007-9" @default.
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