Bottom simulating reflector imaged in 2014 by the USGS along a seismic line acquired south of Hudson Canyon during the Extended Continental Shelf cruise. Image provided by D. Hutchinson and reproduced from USGS Fact Sheet 3080.
Images
Woods Hole Coastal and Marine Science Center images
Bottom simulating reflector imaged in 2014 by the USGS along a seismic line acquired south of Hudson Canyon during the Extended Continental Shelf cruise. Image provided by D. Hutchinson and reproduced from USGS Fact Sheet 3080.
Researchers pull in a cable containing underwater microphones
Researchers pull in a cable containing underwater microphonesRob Thieler (left), Laura Brothers, and David Foster pull in a cable containing underwater microphones after completing a seismic survey in 2014.
Researchers pull in a cable containing underwater microphones
Researchers pull in a cable containing underwater microphonesRob Thieler (left), Laura Brothers, and David Foster pull in a cable containing underwater microphones after completing a seismic survey in 2014.
Map showing distribution of physiographic zones in Buzzards Bay, MA
Map showing distribution of physiographic zones in Buzzards Bay, MAMap showing the distribution of physiographic zones within the Buzzards Bay study area. The physiographic zone classification is adapted from Kelley and others (1998), and the zones are delineated on the basis of sea-floor morphology and the dominant texture of surficial material.
Map showing distribution of physiographic zones in Buzzards Bay, MA
Map showing distribution of physiographic zones in Buzzards Bay, MAMap showing the distribution of physiographic zones within the Buzzards Bay study area. The physiographic zone classification is adapted from Kelley and others (1998), and the zones are delineated on the basis of sea-floor morphology and the dominant texture of surficial material.
A flow tripod (taller, right) and sonar tripod (smaller, left) at the dock before being loaded onto a ship and taken to a site off Fire Island for deployment.
A flow tripod (taller, right) and sonar tripod (smaller, left) at the dock before being loaded onto a ship and taken to a site off Fire Island for deployment.
Locations of the 97 beaches and barrier islands where our partners used the iPlover app to collect and record information on landcover characteristics at piping plover nesting locations during the breeding seasons of 2014-2016.
Locations of the 97 beaches and barrier islands where our partners used the iPlover app to collect and record information on landcover characteristics at piping plover nesting locations during the breeding seasons of 2014-2016.
USGS staff and Tribal GIS workshop participants
Split-beam (EK60) sonar image of bubbles (green) in the water column at a seep site overlooking Baltimore Canyon on the U.S. Atlantic margin. Although the bubbles appear to nearly reach the sea surface, the methane contained in the bubbles would have dissolved and been replaced by other gases by the time the bubbles rise several hundred meters.
Split-beam (EK60) sonar image of bubbles (green) in the water column at a seep site overlooking Baltimore Canyon on the U.S. Atlantic margin. Although the bubbles appear to nearly reach the sea surface, the methane contained in the bubbles would have dissolved and been replaced by other gases by the time the bubbles rise several hundred meters.
Offshore Sediment texture and Geomorphology
Offshore Sediment texture and Geomorphology
Aerial shot of Nauset Beach in Orleans, Massachusetts.
Aerial shot of Nauset Beach in Orleans, Massachusetts.
Tribal GIS Workshop participanats.
Bottom lander deployed south of Martha's Vineyard, MA
Bottom lander deployed south of Martha's Vineyard, MAAn instrumented bottom lander is deployed south of Martha's Vineyard, MA in 2014 as part of the “Bottom Stress and the Generation of Vertical Vorticity Over the Inner Shelf” project.
Bottom lander deployed south of Martha's Vineyard, MA
Bottom lander deployed south of Martha's Vineyard, MAAn instrumented bottom lander is deployed south of Martha's Vineyard, MA in 2014 as part of the “Bottom Stress and the Generation of Vertical Vorticity Over the Inner Shelf” project.
Deployment of an instrumented quadrapod off Martha’s Vineyard
Deployment of an instrumented quadrapod off Martha’s VineyardDeployment of an instrumented quadrapod off Martha’s Vineyard, November 2014.
Deployment of an instrumented quadrapod off Martha’s Vineyard
Deployment of an instrumented quadrapod off Martha’s VineyardDeployment of an instrumented quadrapod off Martha’s Vineyard, November 2014.
Seismic Lab aboard R/V Marcus G. Langseth
Seismic Lab aboard R/V Marcus G. Langseth
Timeline of past drilling activities conducted by countries, private sector firms, government agencies, and academe that have helped to refine global gas hydrate estimates and possible future drilling and production testing
Timeline of past drilling activities conducted by countries, private sector firms, government agencies, and academe that have helped to refine global gas hydrate estimates and possible future drilling and production testing
Airgun array aboard R/V Marcus G. Langseth
Airgun array aboard R/V Marcus G. Langseth
Schematic showing the general setting of seeps on the US Atlantic margin and related processes, such as gas hydrate degradation, groundwater seepage, leakage through fractured rocks, or emissions from the seafloor overlying salt diapirs. Pockmarks shown in white, and the nominal updip limit of gas hydrate stability is represented by the dashed black line.
Schematic showing the general setting of seeps on the US Atlantic margin and related processes, such as gas hydrate degradation, groundwater seepage, leakage through fractured rocks, or emissions from the seafloor overlying salt diapirs. Pockmarks shown in white, and the nominal updip limit of gas hydrate stability is represented by the dashed black line.
Sample preparation and processing area in the K.O. Emery Geotechnical Wing at the Woods Hole Coastal and Marine Science Center, Woods Hole, MA
Sample preparation and processing area in the K.O. Emery Geotechnical Wing at the Woods Hole Coastal and Marine Science Center, Woods Hole, MA
Marinna Martini prepares to deploy a NIMBBLE from the R/V Connecticut
Marinna Martini prepares to deploy a NIMBBLE from the R/V ConnecticutMarinna Martini prepares to deploy a NIMBBLE from the R/V Connecticut south of Martha's Vineyard
Marinna Martini prepares to deploy a NIMBBLE from the R/V Connecticut
Marinna Martini prepares to deploy a NIMBBLE from the R/V ConnecticutMarinna Martini prepares to deploy a NIMBBLE from the R/V Connecticut south of Martha's Vineyard
Jen Suttles collects water samples from a salt marsh tidal creek (East Falmouth, MA) for laboratory analysis of total organic carbon. These samples will be compared to data recorded by instrumentation deployed in an adjacent tidal creek as part of research efforts to quantify carbon dynamics in coastal ecosystems
Jen Suttles collects water samples from a salt marsh tidal creek (East Falmouth, MA) for laboratory analysis of total organic carbon. These samples will be compared to data recorded by instrumentation deployed in an adjacent tidal creek as part of research efforts to quantify carbon dynamics in coastal ecosystems
Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay, MA
Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay, MAThe Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay National Estuarine Research Reserve serves as an important platform for research in coastal salt marshes. Infrastrucutre in this marsh allows researchers to access sites while maintaining habitat and platform health.
Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay, MA
Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay, MAThe Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay National Estuarine Research Reserve serves as an important platform for research in coastal salt marshes. Infrastrucutre in this marsh allows researchers to access sites while maintaining habitat and platform health.
A Sontek IQ ADCP measures depth and velocity of a salt marsh creek
A Sontek IQ ADCP measures depth and velocity of a salt marsh creekA Sontek IQ ADCP measures depth and velocity of a salt marsh creek (Cape Cod, MA)
A Sontek IQ ADCP measures depth and velocity of a salt marsh creek
A Sontek IQ ADCP measures depth and velocity of a salt marsh creekA Sontek IQ ADCP measures depth and velocity of a salt marsh creek (Cape Cod, MA)