Hundreds of catsharks, or chainlink dogfish, rest on one of the "Billy Mitchell" Fleet shipwrecks. The shipwreck has also been occupied by colonies of anemones, starfish, and hydroids.
Images
Coastal and Marine Hazards and Resources Program images.
Hundreds of catsharks, or chainlink dogfish, rest on one of the "Billy Mitchell" Fleet shipwrecks. The shipwreck has also been occupied by colonies of anemones, starfish, and hydroids.
Scientists prepare to extract push core sediment sample
Scientists prepare to extract push core sediment sampleU.S. Geological Survey scientists (left to right) Jennifer McClain-Counts, Jill Bourque, and Amanda Demopoulos prepare to extract a sediment sample from one of the push cores deployed by the Jason II remotely operated vehicle.
Scientists prepare to extract push core sediment sample
Scientists prepare to extract push core sediment sampleU.S. Geological Survey scientists (left to right) Jennifer McClain-Counts, Jill Bourque, and Amanda Demopoulos prepare to extract a sediment sample from one of the push cores deployed by the Jason II remotely operated vehicle.
Juvenile sand lance (Ammodytes hexapterus) (top) and surf smelt (Hypomesus pretiosus) (bottom) collected on Bainbridge Island, Washington. Scale is in inches.
Juvenile sand lance (Ammodytes hexapterus) (top) and surf smelt (Hypomesus pretiosus) (bottom) collected on Bainbridge Island, Washington. Scale is in inches.
Deep-sea coral communities can be very diverse. Here a squat lobster rests among a bubblegum coral, a red tree coral, and a sponge. A brisingid seastar arm is also visible.
Deep-sea coral communities can be very diverse. Here a squat lobster rests among a bubblegum coral, a red tree coral, and a sponge. A brisingid seastar arm is also visible.
Sites visited during Northeast US Canyons Expedition
Sites visited during Northeast US Canyons ExpeditionSites visited by the National Oceanic and Atmospheric Administration (NOAA) remotely operated vehicle (ROV) Deep Discoverer (D2) during the two legs of the Northeast U.S. Canyons Expedition 2013.
Sites visited during Northeast US Canyons Expedition
Sites visited during Northeast US Canyons ExpeditionSites visited by the National Oceanic and Atmospheric Administration (NOAA) remotely operated vehicle (ROV) Deep Discoverer (D2) during the two legs of the Northeast U.S. Canyons Expedition 2013.
Shaded relief image of Vineyard Sound, MA Shoals
Shaded relief image of Vineyard Sound, MA Shoals
USGS technicians prepare a sediment trap to sample the sea floor off Cape Hatteras.
USGS technicians prepare a sediment trap to sample the sea floor off Cape Hatteras.
Sampling seep gas through the ice in Lake Qalluuraq, Barrow Alaska
Sampling seep gas through the ice in Lake Qalluuraq, Barrow AlaskaUSGS research chemist John Pohlman samples seep gas through ice in Lake Qalluuraq, located in continuous permafrost approximately 97 kilometers (60 miles) south of Barrow, Alaska.
Sampling seep gas through the ice in Lake Qalluuraq, Barrow Alaska
Sampling seep gas through the ice in Lake Qalluuraq, Barrow AlaskaUSGS research chemist John Pohlman samples seep gas through ice in Lake Qalluuraq, located in continuous permafrost approximately 97 kilometers (60 miles) south of Barrow, Alaska.
Eric Moore, Wayne Baldwin, and Tommy O’Brien are deploying multichannel seismic streamer onboard R/V Pelican during a 2013 seismic cruise in the Gulf of Mexico as part of the gas hydrates program.
Eric Moore, Wayne Baldwin, and Tommy O’Brien are deploying multichannel seismic streamer onboard R/V Pelican during a 2013 seismic cruise in the Gulf of Mexico as part of the gas hydrates program.
SAFRR tsunami scenario for Oakland and Newport Beach
SAFRR tsunami scenario for Oakland and Newport BeachSome areas that would be inundated (in red) during the SAFRR tsunami scenario. Top, in Oakland and Alameda, in the eastern San Francisco Bay area, large parts of the Oakland Airport would be flooded.
SAFRR tsunami scenario for Oakland and Newport Beach
SAFRR tsunami scenario for Oakland and Newport BeachSome areas that would be inundated (in red) during the SAFRR tsunami scenario. Top, in Oakland and Alameda, in the eastern San Francisco Bay area, large parts of the Oakland Airport would be flooded.
Maximum current speeds for the Port of Los Angeles (POLA) and the Port of Long Beach (POLB) generated during the SAFRR tsunami scenario. The ports are protected by a breakwater, but during the tsunami there would be dangerously fast currents around the port entrances in the wall, locally referred to as “Angels Gate” (at POLA) and “Queens Gate” (at POLB).
Maximum current speeds for the Port of Los Angeles (POLA) and the Port of Long Beach (POLB) generated during the SAFRR tsunami scenario. The ports are protected by a breakwater, but during the tsunami there would be dangerously fast currents around the port entrances in the wall, locally referred to as “Angels Gate” (at POLA) and “Queens Gate” (at POLB).
A bright orange Brisingid starfish is seen in the center of the image. The background is a thicket of live (white) and dead (brown) Lophelia coral. Several squat lobsters (Eumunida picta) can be seen in the coral, as well as a blue encrusting sponge and an urchin (foreground, lower left).
A bright orange Brisingid starfish is seen in the center of the image. The background is a thicket of live (white) and dead (brown) Lophelia coral. Several squat lobsters (Eumunida picta) can be seen in the coral, as well as a blue encrusting sponge and an urchin (foreground, lower left).
Photo of the seafloor in Block Island Sound, Rhode Island
Photo of the seafloor in Block Island Sound, Rhode IslandPhoto of the seafloor in Block Island Sound showing a rock crab and several shrimp on a boulder that is covered with bryozoans. The photo was collected in support of research and management activities (e.g., wind farms and fisheries) along the Rhode Island inner continental shelf.
Photo of the seafloor in Block Island Sound, Rhode Island
Photo of the seafloor in Block Island Sound, Rhode IslandPhoto of the seafloor in Block Island Sound showing a rock crab and several shrimp on a boulder that is covered with bryozoans. The photo was collected in support of research and management activities (e.g., wind farms and fisheries) along the Rhode Island inner continental shelf.
Assemblage of invertebrates living on a steep submarine canyon wall
Assemblage of invertebrates living on a steep submarine canyon wallAssemblage of invertebrates living on a steep submarine canyon wall, seen during the Deepwater Canyons 2013 - Pathways to the Abyss.
Assemblage of invertebrates living on a steep submarine canyon wall
Assemblage of invertebrates living on a steep submarine canyon wallAssemblage of invertebrates living on a steep submarine canyon wall, seen during the Deepwater Canyons 2013 - Pathways to the Abyss.
A sonar on a bottom platform while steaming to the deployment site in the Columbia River in 2013. The 3 platforms acquired data on currents and sediment transport at the river mouth over several months.
A sonar on a bottom platform while steaming to the deployment site in the Columbia River in 2013. The 3 platforms acquired data on currents and sediment transport at the river mouth over several months.
Sandy Brosnahan transporting a weather buoy into the Woods Hole Coastal and Marine Science Center’s operational facility to continue the process of getting it ready to deploy. This buoy was one of 6, deployed by John Warner and others, to measure wind speed, direction, pressure, and temperature off the coast of Fire Island, NY. Paired with each weather b
Sandy Brosnahan transporting a weather buoy into the Woods Hole Coastal and Marine Science Center’s operational facility to continue the process of getting it ready to deploy. This buoy was one of 6, deployed by John Warner and others, to measure wind speed, direction, pressure, and temperature off the coast of Fire Island, NY. Paired with each weather b
Photo for upcoming seminar titled, “Sediment delivery across the bay-marsh interface of an estuarine salt marsh,” by Jessie Lacy.
Photo for upcoming seminar titled, “Sediment delivery across the bay-marsh interface of an estuarine salt marsh,” by Jessie Lacy.
Scientist diver on Sombrero Reef, Florida Keys, FL
Scientist diver on Sombrero Reef, Florida Keys, FLA USGS diver carrying a scale bar and clipboard swims above Sombrero Reef, Florida Keys using SCUBA.
Scientist diver on Sombrero Reef, Florida Keys, FL
Scientist diver on Sombrero Reef, Florida Keys, FLA USGS diver carrying a scale bar and clipboard swims above Sombrero Reef, Florida Keys using SCUBA.
Image of ripples in sand, next to a rocky surface on the seafloor 2.5 km (1.5 miles) offshore San Mateo County, California at a depth of 24.6 meters (81 feet). The two red dots in the image (from lasers mounted on the camera and used as reference points) are 15 cm (6 inches) apart.
Image of ripples in sand, next to a rocky surface on the seafloor 2.5 km (1.5 miles) offshore San Mateo County, California at a depth of 24.6 meters (81 feet). The two red dots in the image (from lasers mounted on the camera and used as reference points) are 15 cm (6 inches) apart.
USGS diver taking a core of a 100-year-old coral in USVI
USGS diver taking a core of a 100-year-old coral in USVIUSGS diver taking a core of a 100-year-old coral to allow reconstruction of past ocean temperatures in St. Thomas, U.S. Virgin Islands.
USGS diver taking a core of a 100-year-old coral in USVI
USGS diver taking a core of a 100-year-old coral in USVIUSGS diver taking a core of a 100-year-old coral to allow reconstruction of past ocean temperatures in St. Thomas, U.S. Virgin Islands.
PCMSC research vessel Karluk