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Bathymetry of the Hudson Shelf Valley (12-m resolution Esri binary grid and 32-bit GeoTIFF, Mercator, WGS 84)

Dates

Publication Date
Start Date
1996-11-23
End Date
2000-05-04

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.

Summary

The Hudson Shelf Valley is the submerged seaward extension of the ancestral Hudson River drainage system and is the largest physiographic feature on the Middle Atlantic continental shelf. The valley begins offshore of New York and New Jersey at about 30-meter (m) water depth, runs southerly and then southeasterly across the Continental Shelf, and terminates on the outer shelf at about 85-m water depth landward of the head of the Hudson Canyon. Portions of the 150-kilometer-long valley were surveyed in 1996, 1998, and 2000 using a Simrad EM1000 multibeam echosounder mounted on the Canadian Coast Guard ship Frederick G. Creed. The purpose of the multibeam echosounder surveys was to map the bathymetry and backscatter intensity of the [...]

Contacts

Attached Files

Click on title to download individual files attached to this item.

hsv_bath12m_browsegraphic.jpg
“Browse graphic.”
thumbnail 33.3 KB image/jpeg
hsv_bath12m.zip
“Data and metadata download.”
76.8 MB application/zip
Extension: HSV_12m_bathymetry.zip
thumbnail.png thumbnail 3.64 KB

Purpose

The bathymetry shows the shape of the sea floor. Of particular interest are the shape of the valley and features that may indicate sediment deposition or transport. The grid merges bathymetry data obtained in 1996, 1998, and 2000.

Additional Information

ArcGIS Service Definition Extension

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