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Portion of the 1-meter (m) contours in quadrangle 5 of the Stellwagen Bank Survey Area offshore of Boston, Massachusetts based on bathymetry data collected by the U.S. Geological Survey from 1994-1996

Dates

Publication Date
Start Date
1994
End Date
1996

Citation

Valentine, P.C., and Cross, V.A., 2024, Geospatial datasets of seabed topography, sediment mobility, and the distribution of geologic substrates in quadrangle 5 of the Stellwagen Bank National Marine Sanctuary region offshore of Boston, Massachusetts: U.S. Geological Survey data release, https://doi.org/10.5066/P9W9BN3S.

Summary

The U.S. Geological Survey (USGS), in cooperation with the National Marine Sanctuary Program of the National Oceanic and Atmospheric Administration (NOAA), has conducted seabed mapping and related research in the Stellwagen Bank National Marine Sanctuary (SBNMS) region since 1993. The interpretive datasets and source information presented here are for quadrangle 5, which is one of 18 similarly sized segments of the 3,700 square kilometer (km2) SBNMS region. The seabed of the SBNMS region is a glaciated terrain that is topographically and texturally diverse. Quadrangle 5 includes the shallow, rippled, coarse-grained sandy crest and upper eastern and western flanks of southern Stellwagen Bank, its fine-grained sandy lower western flank, [...]

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Attached Files

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

Shapefile: q5_1m_contours.zip
q5_1m_contours.cpg 5 Bytes
q5_1m_contours.dbf 850 Bytes
q5_1m_contours.prj 167 Bytes
q5_1m_contours.shp
“Data in shapefile format.”
520.57 KB
q5_1m_contours.shx 548 Bytes
q5_1m_contours_browse.png
“Image of the portion of 1-meter contours assisting the substrate interpretation.”
thumbnail 421.65 KB

Purpose

The purpose of this dataset is to release the 1-meter (m) contours that are used in quadrangle 5 Stellwagen Bank geologic interpretation maps that aid in interpretation. The 1-m contours indicate the more hummocky relief of the seabed in areas dominated by gravel deposits and small boulder ridges. The one meter contours accentuate low-relief topographic complexity in these areas. The contours represent a close approximation of seabed microtopography, as the resolution of the multibeam echo sounder data used to generate these data is on the order of 1 m. By contrast, 1-m contours are not shown in areas where the seabed is relatively smooth and not dominated by gravel features. Any topographic complexity in these areas is beyond the resolution of the multibeam echosounder (< 1 meter in relief) and cannot be accurately depicted by the 1-m bathymetric contours.

Additional Information

Shapefile Extension

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