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  "Title": "GeoTIFF image of the backscatter intensity of the sea floor of the Hudson Shelf Valley (12-m resolution, Mercator, WGS 84) ",
  "Author": "Butman, Bradford, Danforth, W.W., Clarke, J.E.H., and Signell, R.P.",
  "Comments": "The GeoTIFF image of backscatter intensity provides qualitative information on the sediment texture and roughness of the sea floor. Backscatter intensity, a measure of the strength of the acoustic return from the sea floor, is a function of the properties of the surficial sediments and of the bottom roughness. Generally high backscatter intensity (strong return), shown as light gray tones, is associated with rock or coarse-grained sediment, and low backscatter intensity (weak return), shown as dark gray tones, with fine-grained sediments. The image merges backscatter intensity data obtained in 1996, 1998, and 2000. \n\nSuggested citation: Butman, Bradford, Danforth, W.W., Clarke, J.E.H., and Signell, R.P., 2017, Bathymetry and backscatter intensity of the sea floor of the Hudson Shelf Valley: U.S. Geological Survey data release, https://doi.org/doi:10.5066/F7C53J1Z. ",
  "Subject": "Hudson Shelf Valley backscatter intentisy image merged from 1996, 1998, and 2000 data.",
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  "Keywords": "backscatter, Hudson Shelf Valley"
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