Wave-driven flooding and overwash on Roi-Namur Atoll
Wave-driven flooding and overwash on Roi-Namur AtollWave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
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Coastal and Marine Hazards and Resources Program images.
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands
Schematic geologic cross section of Southern Oʻahu showing groundwater–seawater interaction in the vicinity of Honolulu, HI (modified from Frans et al., 2012).
Schematic geologic cross section of Southern Oʻahu showing groundwater–seawater interaction in the vicinity of Honolulu, HI (modified from Frans et al., 2012).
Every inch of the deck of the R/V Connecticut is covered by instrumented platforms awaiting deployment on the seafloor south of Fire Island NY in winter 2014.
Every inch of the deck of the R/V Connecticut is covered by instrumented platforms awaiting deployment on the seafloor south of Fire Island NY in winter 2014.
Every inch of the deck of the R/V Connecticut is covered by instrumented platforms awaiting deployment on the seafloor south of Fire Island NY in winter 2014.
Every inch of the deck of the R/V Connecticut is covered by instrumented platforms awaiting deployment on the seafloor south of Fire Island NY in winter 2014.
Snowy owl visitor to CCGS Louis S. St-Laurent in the Arctic Ocean
Snowy owl visitor to CCGS Louis S. St-Laurent in the Arctic Ocean
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.
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.
U.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.
U.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 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 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.
USGS 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.
USGS 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.
Assemblage 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, 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.
Some 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.
Some 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 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 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.