Screenshot of CoastSeg interface, from the study CoastSeg: an accessible and extendable hub for satellite-derived-shoreline (SDS) detection and mapping.
Images
Coastal and Marine Hazards and Resources Program images.
Screenshot of CoastSeg interface, from the study CoastSeg: an accessible and extendable hub for satellite-derived-shoreline (SDS) detection and mapping.
Satellite-derived shorelines for a barrier island east of Moses Point Fishing Village, Norton Sound, Alaska
Satellite-derived shorelines for a barrier island east of Moses Point Fishing Village, Norton Sound, AlaskaSatellite-derived shorelines for a barrier island east of Moses Point Fishing Village, Norton Sound, Alaska, from the study CoastSeg: an accessible and extendable hub for satellite-derived-shoreline (SDS) detection and mapping.
Satellite-derived shorelines for a barrier island east of Moses Point Fishing Village, Norton Sound, Alaska
Satellite-derived shorelines for a barrier island east of Moses Point Fishing Village, Norton Sound, AlaskaSatellite-derived shorelines for a barrier island east of Moses Point Fishing Village, Norton Sound, Alaska, from the study CoastSeg: an accessible and extendable hub for satellite-derived-shoreline (SDS) detection and mapping.
Satellite images of barrier island near Moses Point Fishing Village, taken in 1986 and 2023
Satellite images of barrier island near Moses Point Fishing Village, taken in 1986 and 2023Satellite images of barrier island near Moses Point Fishing Village, Norton Sound, Alaska, taken in 1986 and 2023.
Satellite images of barrier island near Moses Point Fishing Village, taken in 1986 and 2023
Satellite images of barrier island near Moses Point Fishing Village, taken in 1986 and 2023Satellite images of barrier island near Moses Point Fishing Village, Norton Sound, Alaska, taken in 1986 and 2023.
USGS Coastal Change Hazards Portal shows Hurricane Beryl's expected impacts
USGS Coastal Change Hazards Portal shows Hurricane Beryl's expected impactsPotential coastal change impacts are predicted during a direct landfall of Hurricane Beryl on the Texas coast at 4:00 am, Sunday, July 7, 2024.
USGS Coastal Change Hazards Portal shows Hurricane Beryl's expected impacts
USGS Coastal Change Hazards Portal shows Hurricane Beryl's expected impactsPotential coastal change impacts are predicted during a direct landfall of Hurricane Beryl on the Texas coast at 4:00 am, Sunday, July 7, 2024.
USGS Marine Operations Manager Chuck Worley conducting fieldwork to study the geologic framework of Nantucket Sound.
USGS Marine Operations Manager Chuck Worley conducting fieldwork to study the geologic framework of Nantucket Sound.
U.S. Coastal Wetland Synthesis Applications Webpage Image
U.S. Coastal Wetland Synthesis Applications Webpage ImageThe USGS is assessing the physical condition of coastal wetlands and their response to external forces, using field observations and remote-sensing data. The U.S.
U.S. Coastal Wetland Synthesis Applications Webpage Image
U.S. Coastal Wetland Synthesis Applications Webpage ImageThe USGS is assessing the physical condition of coastal wetlands and their response to external forces, using field observations and remote-sensing data. The U.S.
Distinguished Service Award for Research Geologist Curt Storlazzi, presented on May 8, 2024.
Distinguished Service Award for Research Geologist Curt Storlazzi, presented on May 8, 2024.
Distinguished Service Award for USGS Research Geophysicist Carolyn Ruppel, presented on May 8, 2024.
Distinguished Service Award for USGS Research Geophysicist Carolyn Ruppel, presented on May 8, 2024.
Honorees pose with their awards at the 77th DOI Honor Awards Convocation
Honorees pose with their awards at the 77th DOI Honor Awards ConvocationHonorees pose with their awards at the 77th DOI Honor Awards Convocation on May 8, 2024.
Honorees pose with their awards at the 77th DOI Honor Awards Convocation
Honorees pose with their awards at the 77th DOI Honor Awards ConvocationHonorees pose with their awards at the 77th DOI Honor Awards Convocation on May 8, 2024.
The United States has ECS in seven offshore areas: the Arctic, Atlantic (east coast), Bering Sea, Pacific (west coast), Mariana Islands, and two areas in the Gulf of America. The U.S. ECS area is approximately one million square kilometers – an area about twice the size of California.
The United States has ECS in seven offshore areas: the Arctic, Atlantic (east coast), Bering Sea, Pacific (west coast), Mariana Islands, and two areas in the Gulf of America. The U.S. ECS area is approximately one million square kilometers – an area about twice the size of California.
Overview map of the Mississippi River delta showing subaerial birdfoot morphology formed by distributaries.
Overview map of the Mississippi River delta showing subaerial birdfoot morphology formed by distributaries.
In transit to survey the shallows of Wallops Island, Virginia
In transit to survey the shallows of Wallops Island, VirginiaSabrina Levinson, a USGS intern on the Coastal Sediment Availability and Flux Project (St. Petersburg Coastal and Marine Science Center), pilots a survey waverunner to the shallows of Wallops Island, Virginia.
In transit to survey the shallows of Wallops Island, Virginia
In transit to survey the shallows of Wallops Island, VirginiaSabrina Levinson, a USGS intern on the Coastal Sediment Availability and Flux Project (St. Petersburg Coastal and Marine Science Center), pilots a survey waverunner to the shallows of Wallops Island, Virginia.
From June through December, WHCMSC scientists are collecting shoreline and volumetric data at a beach in Sandwich, Massachusetts following a 2023 U.S. Army Corps of Engineers beach nourishment. The data will be useful for various purposes. Chris Sherwood is interested in comparing how the different measuring techniques work on different types of vegetation.
From June through December, WHCMSC scientists are collecting shoreline and volumetric data at a beach in Sandwich, Massachusetts following a 2023 U.S. Army Corps of Engineers beach nourishment. The data will be useful for various purposes. Chris Sherwood is interested in comparing how the different measuring techniques work on different types of vegetation.
Map of study area showing the Sur Pockmark Field offshore of central California
Map of study area showing the Sur Pockmark Field offshore of central CaliforniaLocation Map showing the Sur Pockmark Field outlined in green, individual pockmarks are shown as small red dots. This study focuses on the largest section of the pockmark field, from the Lucia Chica Channel down to the San Simeon Channel. AUV surveys are outlined in white and the offshore wind commercial leases are outlined in gray.
Map of study area showing the Sur Pockmark Field offshore of central California
Map of study area showing the Sur Pockmark Field offshore of central CaliforniaLocation Map showing the Sur Pockmark Field outlined in green, individual pockmarks are shown as small red dots. This study focuses on the largest section of the pockmark field, from the Lucia Chica Channel down to the San Simeon Channel. AUV surveys are outlined in white and the offshore wind commercial leases are outlined in gray.
Diagram showing patterns of erosion and deposition that produce seafloor pockmarks
Diagram showing patterns of erosion and deposition that produce seafloor pockmarksA diagram illustrating how the patterns of erosion and deposition associated with three sediment gravity flows could produce the stacked pockmarks and lateral migration observed in AUV-collected Chirp profiles. Long, uneventful episodes of hemipelagic drape (a, d, g, j) are intermittently interrupted by sediment gravity flows that either: 1b.
Diagram showing patterns of erosion and deposition that produce seafloor pockmarks
Diagram showing patterns of erosion and deposition that produce seafloor pockmarksA diagram illustrating how the patterns of erosion and deposition associated with three sediment gravity flows could produce the stacked pockmarks and lateral migration observed in AUV-collected Chirp profiles. Long, uneventful episodes of hemipelagic drape (a, d, g, j) are intermittently interrupted by sediment gravity flows that either: 1b.
Ernest F. Hollings ACE Basin National Wildlife Refuge
Ernest F. Hollings ACE Basin National Wildlife RefugeErnest F. Hollings ACE Basin National Wildlife Refuge in South Carolina shown in the pop-out of the U.S. Coastal Wetlands Synthesis Applications geonarrative.
Ernest F. Hollings ACE Basin National Wildlife Refuge
Ernest F. Hollings ACE Basin National Wildlife RefugeErnest F. Hollings ACE Basin National Wildlife Refuge in South Carolina shown in the pop-out of the U.S. Coastal Wetlands Synthesis Applications geonarrative.
Detail of sediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.
Detail of sediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.Sediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.
Detail of sediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.
Detail of sediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.Sediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.
Ernest F. Hollings ACE Basin National Wildlife Refuge
Ernest F. Hollings ACE Basin National Wildlife RefugeErnest F. Hollings ACE Basin National Wildlife Refuge in South Carolina shown in the pop-out of the U.S. Coastal Wetlands Synthesis Applications geonarrative.
Ernest F. Hollings ACE Basin National Wildlife Refuge
Ernest F. Hollings ACE Basin National Wildlife RefugeErnest F. Hollings ACE Basin National Wildlife Refuge in South Carolina shown in the pop-out of the U.S. Coastal Wetlands Synthesis Applications geonarrative.
Researchers who conducted prior paleotsunami research at Salmon River estuary, Oregon
Researchers who conducted prior paleotsunami research at Salmon River estuary, OregonResearchers Brian Atwater and Wendy Grant Walter conducting prior paleotsunami research at Salmon River estuary, Oregon.
Researchers who conducted prior paleotsunami research at Salmon River estuary, Oregon
Researchers who conducted prior paleotsunami research at Salmon River estuary, OregonResearchers Brian Atwater and Wendy Grant Walter conducting prior paleotsunami research at Salmon River estuary, Oregon.
Sediment core with tsunami deposit from the Salmon River estuary, Oregon
Sediment core with tsunami deposit from the Salmon River estuary, OregonSediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.
Sediment core with tsunami deposit from the Salmon River estuary, Oregon
Sediment core with tsunami deposit from the Salmon River estuary, OregonSediment core with tidal silt, tsunami sand, and marsh peat collected from the Salmon River estuary, Oregon.
USGS scientists SeanPaul La Selle and Jason Padgett collecting sediment cores at the Salmon River estuary, Oregon
USGS scientists SeanPaul La Selle and Jason Padgett collecting sediment cores at the Salmon River estuary, OregonUSGS scientists SeanPaul La Selle and Jason Padgett collecting sediment cores at the Salmon River estuary, Oregon.
USGS scientists SeanPaul La Selle and Jason Padgett collecting sediment cores at the Salmon River estuary, Oregon
USGS scientists SeanPaul La Selle and Jason Padgett collecting sediment cores at the Salmon River estuary, OregonUSGS scientists SeanPaul La Selle and Jason Padgett collecting sediment cores at the Salmon River estuary, Oregon.