Colored, shaded-relief bathymetry of Trinidad Submarine Canyon northwest of Humboldt Bay in northern California. Area is in the vicinity of a potential offshore renewable energy development. See larger map for location.
Images
Coastal and Marine Hazards and Resources Program images.
Colored, shaded-relief bathymetry of Trinidad Submarine Canyon northwest of Humboldt Bay in northern California. Area is in the vicinity of a potential offshore renewable energy development. See larger map for location.
Colored shaded-relief bathymetry including submarine channels and pockmarks offshore Morro Bay, California. Map generated from AUV-based multibeam bathymetry data collected by MBARI both prior to and as a part of EXPRESS.
Colored shaded-relief bathymetry including submarine channels and pockmarks offshore Morro Bay, California. Map generated from AUV-based multibeam bathymetry data collected by MBARI both prior to and as a part of EXPRESS.
Rebecca Sanders-DeMott performing maintenance on an eddy flux tower
Rebecca Sanders-DeMott performing maintenance on an eddy flux towerInstruments continue to collect vital data during workplace closures. Here staff perform maintenance on an eddy flux tower located within a phragmites wetland at the Cape Cod National Seashore. The instruments on this tower measure methane and CO2 fluxes related to plant and soil processes day in and day out for the entire year.
Rebecca Sanders-DeMott performing maintenance on an eddy flux tower
Rebecca Sanders-DeMott performing maintenance on an eddy flux towerInstruments continue to collect vital data during workplace closures. Here staff perform maintenance on an eddy flux tower located within a phragmites wetland at the Cape Cod National Seashore. The instruments on this tower measure methane and CO2 fluxes related to plant and soil processes day in and day out for the entire year.
Image showing the distribution of usSEABED data output files US9_EXT (blue triangles) and US9_PRS (pink circles) around the continental United States, Hawai'i, and Puerto Rico.
Image showing the distribution of usSEABED data output files US9_EXT (blue triangles) and US9_PRS (pink circles) around the continental United States, Hawai'i, and Puerto Rico.
Map of gas hydrate locations, known and inferred. Browse graphic for ScienceBase data release, Preliminary global database of known and inferred gas hydrate locations.
Map of gas hydrate locations, known and inferred. Browse graphic for ScienceBase data release, Preliminary global database of known and inferred gas hydrate locations.
Marine technician Dan Powers, from the Pacific Coastal and Marine Science Center's Marine Facility (PCMSC MarFac), wears all the required personal protective equipment: bib waders, personal floatation device, and mask.
Marine technician Dan Powers, from the Pacific Coastal and Marine Science Center's Marine Facility (PCMSC MarFac), wears all the required personal protective equipment: bib waders, personal floatation device, and mask.
Meagan Gonneea at the Herring River Estuary, Wellfleet, MA
Meagan Gonneea at the Herring River Estuary, Wellfleet, MAWhen wetland plants in the northeast emerged this spring, USGS scientists were working from home and unable to start many planned research activities. However, many instruments were already deployed and continued to collect information critical to USGS research.
Meagan Gonneea at the Herring River Estuary, Wellfleet, MA
Meagan Gonneea at the Herring River Estuary, Wellfleet, MAWhen wetland plants in the northeast emerged this spring, USGS scientists were working from home and unable to start many planned research activities. However, many instruments were already deployed and continued to collect information critical to USGS research.
Section of a sediment core collected from the deepest basin of Lake Enriquillo in the Dominican Republic. USGS scientists are analyzing cores from the lake to reconstruct past changes in rainfall.
Section of a sediment core collected from the deepest basin of Lake Enriquillo in the Dominican Republic. USGS scientists are analyzing cores from the lake to reconstruct past changes in rainfall.
Fire Island, New York is sparsely populated and regularly nourished, but has few modifications that impede natural sediment exchanges. Shoreface geomorphology reflects past periods of seaward progradation and alongshore extension resulting in a relatively sediment-rich shoreface. USGS scientists collect geologic and morphologic data from this island’s shoreface.
Fire Island, New York is sparsely populated and regularly nourished, but has few modifications that impede natural sediment exchanges. Shoreface geomorphology reflects past periods of seaward progradation and alongshore extension resulting in a relatively sediment-rich shoreface. USGS scientists collect geologic and morphologic data from this island’s shoreface.
Modeled beach profile evolution at Parramore Island, Virginia
Modeled beach profile evolution at Parramore Island, VirginiaAnimation displays modeled beach profile elevation as it has evolved at Parramore Island, Virginia. These data are based on geomorphic investigation and measure distance (in kilometers) of cross-shore accretion. QS is the flux of sand to the beach, and QD is the flux of sand from the beach to the active dune.
Modeled beach profile evolution at Parramore Island, Virginia
Modeled beach profile evolution at Parramore Island, VirginiaAnimation displays modeled beach profile elevation as it has evolved at Parramore Island, Virginia. These data are based on geomorphic investigation and measure distance (in kilometers) of cross-shore accretion. QS is the flux of sand to the beach, and QD is the flux of sand from the beach to the active dune.
Cedar Island, Virginia is an uninhabited barrier that has migrated landward approximately 15-30 meters per year since 1984 due to its low sediment supply. The shoreface slope is gradual but almost entirely devoid of island sediment - both responses to its recent, rapid retreat. USGS scientists collect geologic and morphologic data from this island’s shoreface.
Cedar Island, Virginia is an uninhabited barrier that has migrated landward approximately 15-30 meters per year since 1984 due to its low sediment supply. The shoreface slope is gradual but almost entirely devoid of island sediment - both responses to its recent, rapid retreat. USGS scientists collect geologic and morphologic data from this island’s shoreface.
Rockaway Beach, New York is heavily developed, has seawalls and groins and is regularly nourished. It hasn’t changed much over 20 years. The shoreface is steep and sediment cover doesn’t extend far from shore—likely the result of being fixed in place for decades. USGS scientists collect geologic and morphologic data from this island’s shoreface.
Rockaway Beach, New York is heavily developed, has seawalls and groins and is regularly nourished. It hasn’t changed much over 20 years. The shoreface is steep and sediment cover doesn’t extend far from shore—likely the result of being fixed in place for decades. USGS scientists collect geologic and morphologic data from this island’s shoreface.
Modeled beach profile evolution at Fishing Point, Virginia
Modeled beach profile evolution at Fishing Point, VirginiaAnimation displays modeled beach profile elevation as it has evolved at Fishing Point, Virginia. These data are based on historical charts and images and measure distance (in kilometers) of cross-shore accretion. QS is the flux of sand to the beach, and QD is the flux of sand from the beach to the active dune.
Modeled beach profile evolution at Fishing Point, Virginia
Modeled beach profile evolution at Fishing Point, VirginiaAnimation displays modeled beach profile elevation as it has evolved at Fishing Point, Virginia. These data are based on historical charts and images and measure distance (in kilometers) of cross-shore accretion. QS is the flux of sand to the beach, and QD is the flux of sand from the beach to the active dune.
Overview of Taan Fiord. Inset showing location of Taan Fiord, Alaska in Wrangell St. Elias National Park and Preserve. Taan Fiord is about 100 km from the nearest town, Yakutat, AK. Landsat 8 image of Taan Fiord acquired in 2016. Vegetation loss is clear near the water line.
Overview of Taan Fiord. Inset showing location of Taan Fiord, Alaska in Wrangell St. Elias National Park and Preserve. Taan Fiord is about 100 km from the nearest town, Yakutat, AK. Landsat 8 image of Taan Fiord acquired in 2016. Vegetation loss is clear near the water line.
A USGS scientist navigates a personal watercraft (PWC) slowly through Elkhorn Slough. The PWC is equipped with an echosounder and GPS, to record accurate depth and location. This mapping effort is part of recurring surveys in the Monterey Bay area.
A USGS scientist navigates a personal watercraft (PWC) slowly through Elkhorn Slough. The PWC is equipped with an echosounder and GPS, to record accurate depth and location. This mapping effort is part of recurring surveys in the Monterey Bay area.
Collecting nearshore bathymetry data off Rio del Mar
Collecting nearshore bathymetry data off Rio del MarA USGS scientist navigates a personal watercraft equipped with sonar and GPS to collect depth information (bathymetry) of the nearshore. This mapping effort is part of recurring surveys in the Monterey Bay area.
Collecting nearshore bathymetry data off Rio del Mar
Collecting nearshore bathymetry data off Rio del MarA USGS scientist navigates a personal watercraft equipped with sonar and GPS to collect depth information (bathymetry) of the nearshore. This mapping effort is part of recurring surveys in the Monterey Bay area.
A USGS scientist walks along Santa Cruz Main Beach at the edge of the San Lorenzo River in Santa Cruz, California, wearing a backpack with GPS equipment. She is collecting elevation data that will be used to create a topographic map of the beach. This mapping effort is part of recurring surveys in the Monterey Bay area.
A USGS scientist walks along Santa Cruz Main Beach at the edge of the San Lorenzo River in Santa Cruz, California, wearing a backpack with GPS equipment. She is collecting elevation data that will be used to create a topographic map of the beach. This mapping effort is part of recurring surveys in the Monterey Bay area.
From left to right – Uri ten Brink, Eric Moore, Wayne Baldwin, Alex Nichols, Jason Chaytor, and Captain Orlando Espinoza. Less than two months after the largest earthquake in the seismic sequence, the USGS Woods Hole Coastal and Marine Science Center organized a rapid response seismic survey.
From left to right – Uri ten Brink, Eric Moore, Wayne Baldwin, Alex Nichols, Jason Chaytor, and Captain Orlando Espinoza. Less than two months after the largest earthquake in the seismic sequence, the USGS Woods Hole Coastal and Marine Science Center organized a rapid response seismic survey.
Permanently flooded shore in Guayanilla, Puerto Rico.
Permanently flooded shore in Guayanilla, Puerto Rico.
R/V Sultana. Less than two months after the largest earthquake in the seismic sequence, the USGS Woods Hole Coastal and Marine Science Center organized a rapid response seismic survey.
R/V Sultana. Less than two months after the largest earthquake in the seismic sequence, the USGS Woods Hole Coastal and Marine Science Center organized a rapid response seismic survey.
Collapsed arch in Guayanilla, Puerto Rico.
Collapsed arch in Guayanilla, Puerto Rico.