Open-File Report 2013-1020
High-Resolution Geophysical Data Collected Aboard the U.S. Geological Survey Research Vessel Rafael to Supplement Existing Datasets From Buzzards Bay and Vineyard Sound, Massachusetts
This report contains high-resolution geophysical data from approximately 70 square-kilometers (km2) of the sea floor surrounding the eastern Elizabeth Islands and northern coast of Martha's Vineyard, and on sand shoals in Vineyard Sound, Massachusetts (fig. 1). Adding to the series of geophysical data reports (Barnhardt and others, 2006, 2009, 2010; Ackerman and others, 2006; Andrews and others, 2010, 2012; Pendleton and others, 2012; Turecek and others, 2012) published through a cooperative mapping program (http://woodshole.er.usgs.gov/project-pages/coastal_mass/) between the U.S. Geological Survey (USGS) and the Massachusetts Office of Coastal Zone Management (CZM), this collection of relatively small surveys was conducted to supplement seismic-survey data and to fill gaps among existing National Oceanic and Atmospheric Administration (NOAA) hydrographic surveys and other USGS geophysical surveys of Vineyard Sound and Buzzards Bay (fig. 2).
Vineyard Sound is between Martha's Vineyard and the Elizabeth Islands, which trail off the southwestern corner of Cape Cod at Woods Hole, Massachusetts, and separate Vineyard Sound from Buzzards Bay (fig. 1). The Elizabeth Islands are composed of remnants of the Buzzards Bay Moraine that formed about 20 thousand years before present during the waning stage of the last glaciation (Oldale, 1982; Balco, 2011). As sea-level rose throughout the Holocene following deglaciation, parts of the Buzzards Bay Moraine became submerged, isolating the Elizabeth Islands from Cape Cod (Mather and others, 1942; Larson, 1982; Oldale and O’Hara, 1984; Uchupi and others, 1996). The nearshore surveyed areas off the Elizabeth Islands outline the surficial extent of the original moraine deposits and changeover to modern marine and estuarine deposits as tracklines move offshore into Buzzards Bay. In Vineyard Sound, water depths increase quickly off the Elizabeth Islands, where deep tidal channels scour into glacial deposits. The sand shoals surveyed in Vineyard Sound, which rise as much as 25 meters (m) above the surrounding channels, are associated with ice-contact deposits and are usually covered in bedforms. The largest sand bodies, such as Middle Ground, Hedge Fence, and L'Hommedieu, have persisted in approximately their present locations since the first nautical charts of the area were made in the late 1700s. These shoals demonstrate the role that strong currents and marine processes have played in reworking glacial sediments since the Holocene marine transgression. |