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Woods Hole Coastal and Marine Science Center images

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Split-beam (EK60) sonar image of bubbles (green) in the water column at a seep site overlooking Baltimore Canyon
Split-beam (EK60) sonar image of bubbles
Split-beam (EK60) sonar image of bubbles
Split-beam (EK60) sonar image of bubbles

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the bubbles appear to nearly reach the sea surface, the methane contained in the bubbles would have dissolved and been replaced by other gases by the time the bubbles rise several hundred meters.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the bubbles appear to nearly reach the sea surface, the methane contained in the bubbles would have dissolved and been replaced by other gases by the time the bubbles rise several hundred meters.

Preview image of multi-channel seismic data collected by the USGS
Multi-channel seismic data preview image
Multi-channel seismic data preview image
Multi-channel seismic data preview image

Preview image of multi-channel seismic data collected by the USGS off the US Seaboard Atlantic as part of the US Extended Continental Shelf project.

Map showing the distribution of physiographic zones within the Buzzards Bay study area
Map showing distribution of physiographic zones in Buzzards Bay, MA
Map showing distribution of physiographic zones in Buzzards Bay, MA
Map showing distribution of physiographic zones in Buzzards Bay, MA

Map 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 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
Oceanographic Tripods on the Dock
Oceanographic Tripods on the Dock
Oceanographic Tripods on the Dock

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.

Bottom simulating reflector
Bottom simulating reflector
Bottom simulating reflector
Bottom simulating reflector

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.

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.

3 researchers on the deck of a ship, with the sea in the background, are pulling on a thick black cable.
Researchers pull in a cable containing underwater microphones
Researchers pull in a cable containing underwater microphones
Researchers pull in a cable containing underwater microphones

Rob Thieler (left), Laura Brothers, and David Foster pull in a cable containing underwater microphones after completing a seismic survey in 2014.

Image of an instrumented bottom lander deployed south of Martha's Vineyard, MA
Bottom lander deployed south of Martha's Vineyard, MA
Bottom lander deployed south of Martha's Vineyard, MA
Bottom lander deployed south of Martha's Vineyard, MA

 An 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.

 An 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.

Timeline of past drilling activities
Gas Hydrates Drilling Activities
Gas Hydrates Drilling Activities
Gas Hydrates Drilling Activities

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

Schematic showing the general setting of seeps on the US Atlantic margin and related processes, such as gas hydrate degradation,
U.S. Atlantic Margin Seeps
U.S. Atlantic Margin Seeps
U.S. Atlantic Margin Seeps

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
Sample preparation and processing area
Sample preparation and processing area
Sample preparation and processing area

Sample preparation and processing area in the K.O. Emery Geotechnical Wing at the Woods Hole Coastal and Marine Science Center, Woods Hole, MA

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