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    Constraining the Stratigraphy and Depth to Bedrock at the Forest River Salt Marsh in Salem, MA

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    Title
    Constraining the Stratigraphy and Depth to Bedrock at the Forest River Salt Marsh in Salem, MA
    Author
    Carpi, Katelyn
    Date
    May 2021
    Subject
    Geology
    Seismic Refraction
    Stratigraphy
    
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    URI
    http://hdl.handle.net/20.500.13013/1516
    Abstract
    The stratigraphy and depth to bedrock at the Forest River salt marsh in Salem, MA was constrained using seismic refraction methods. A ~2 m layer of peat was found on top of a layer of glaciomarine clay, with a transition layer in between. The depth to bedrock was constrained to greater than 19.5 m. Two surveys were completed and each had different p-wave velocities for both of the materials. The tide and weather conditions were then researched. It was concluded that the change in p-wave velocity from one survey to the next was due to a change in density caused by an increase of moisture in the area.
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    Hubeny, Bradford
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