Big Sur coast. Red squares mark some of the sites damaged by 2016–17 winter storms, including Mud Creek and Paul’s Slide areas.
Images
Coastal and Marine Hazards and Resources Program images.
Big Sur coast. Red squares mark some of the sites damaged by 2016–17 winter storms, including Mud Creek and Paul’s Slide areas.
Fieldtrip participants at the former San Clemente Dam site
Fieldtrip participants at the former San Clemente Dam siteFieldtrip participants at the former San Clemente Dam site.
Fieldtrip participants at the former San Clemente Dam site
Fieldtrip participants at the former San Clemente Dam siteFieldtrip participants at the former San Clemente Dam site.
Wave-driven flooding and overwash on Roi-Namur Atoll, Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll, Marshall IslandsPhoto shows results of wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands.
Wave-driven flooding and overwash on Roi-Namur Atoll, Marshall Islands
Wave-driven flooding and overwash on Roi-Namur Atoll, Marshall IslandsPhoto shows results of wave-driven flooding and overwash on Roi-Namur Atoll, Republic of the Marshall Islands.
Diagram: different ocean features that contribute to coastal flooding
Diagram: different ocean features that contribute to coastal floodingDiagram of different ocean features that contribute to coastal flooding.
Diagram: different ocean features that contribute to coastal flooding
Diagram: different ocean features that contribute to coastal floodingDiagram of different ocean features that contribute to coastal flooding.
Map shows hill-shaded bathymetric, backscatter, and photographic data
Map shows hill-shaded bathymetric, backscatter, and photographic dataHill-shaded bathymetric, backscatter, and photographic data collected by NOAA and the USGS. Backscatter data give indications of seafloor character. In general, low-backscatter intensity (blue) corresponds to finer-grained material, whereas high-backscatter intensity (orange) corresponds to coarser substrate.
Map shows hill-shaded bathymetric, backscatter, and photographic data
Map shows hill-shaded bathymetric, backscatter, and photographic dataHill-shaded bathymetric, backscatter, and photographic data collected by NOAA and the USGS. Backscatter data give indications of seafloor character. In general, low-backscatter intensity (blue) corresponds to finer-grained material, whereas high-backscatter intensity (orange) corresponds to coarser substrate.
The USGS conducted surveys on the inner continental shelf of the Delma
The USGS conducted surveys on the inner continental shelf of the DelmaThe USGS conducted surveys on the inner continental shelf of the Delmarva Peninsula (shown in green) to complement related datasets previously collected in the area by partners NOAA and BOEM. The inset map shows location of the study area.
The USGS conducted surveys on the inner continental shelf of the Delma
The USGS conducted surveys on the inner continental shelf of the DelmaThe USGS conducted surveys on the inner continental shelf of the Delmarva Peninsula (shown in green) to complement related datasets previously collected in the area by partners NOAA and BOEM. The inset map shows location of the study area.
The 3DR Solo with GoPro Hero4 camera and gimbal. Coming to a survey area near you soon.
The 3DR Solo with GoPro Hero4 camera and gimbal. Coming to a survey area near you soon.
Installing large boulders to armor the shore against further erosion
Installing large boulders to armor the shore against further erosionInstalling large boulders as riprap to armor the shore against further erosion at Goleta Beach in Southern California. The tide is very low (negative).
Installing large boulders to armor the shore against further erosion
Installing large boulders to armor the shore against further erosionInstalling large boulders as riprap to armor the shore against further erosion at Goleta Beach in Southern California. The tide is very low (negative).
An example of the CoSMoS-COAST shoreline data for La Jolla Shores
An example of the CoSMoS-COAST shoreline data for La Jolla ShoresAn example of the shoreline data for La Jolla Shores, used in the CoSMoS-COAST model. The many squiggly colored lines indicate the changing shoreline location through time [basemaps from Google Earth].
An example of the CoSMoS-COAST shoreline data for La Jolla Shores
An example of the CoSMoS-COAST shoreline data for La Jolla ShoresAn example of the shoreline data for La Jolla Shores, used in the CoSMoS-COAST model. The many squiggly colored lines indicate the changing shoreline location through time [basemaps from Google Earth].
Shawn Harrison during a post-storm survey of beaches in Santa Cruz, CA
Shawn Harrison during a post-storm survey of beaches in Santa Cruz, CAShawn Harrison uses a GPS-equipped backpack to measure sand elevations during a post-storm survey of beaches in Santa Cruz, California.
Shawn Harrison during a post-storm survey of beaches in Santa Cruz, CA
Shawn Harrison during a post-storm survey of beaches in Santa Cruz, CAShawn Harrison uses a GPS-equipped backpack to measure sand elevations during a post-storm survey of beaches in Santa Cruz, California.
USGS scientist measures water, sediment movement in coastal salt marsh
USGS scientist measures water, sediment movement in coastal salt marshUSGS scientist Zafer Defne measures water and sediment movement at Forsythe National Wildlife Refuge, New Jersey. Defne is co-author with Neil Ganju of a 2017 study on how to estimate coastal salt marshes’ potential longevity, based on their sediment budgets and the ratio of open water to vegetation.
USGS scientist measures water, sediment movement in coastal salt marsh
USGS scientist measures water, sediment movement in coastal salt marshUSGS scientist Zafer Defne measures water and sediment movement at Forsythe National Wildlife Refuge, New Jersey. Defne is co-author with Neil Ganju of a 2017 study on how to estimate coastal salt marshes’ potential longevity, based on their sediment budgets and the ratio of open water to vegetation.
A look into the USGS Pacific Coastal and Marine Science Center’s Marine Minerals Laboratory Suite.
A look into the USGS Pacific Coastal and Marine Science Center’s Marine Minerals Laboratory Suite.
USGS Oceanographer, Neil Ganju, at the 2017 Woods Hole Science Stroll
USGS Oceanographer, Neil Ganju, at the 2017 Woods Hole Science StrollWoods Hole Coastal and Marine Science Center Oceanographer, Neil Ganju, sharing science at the 2017 Woods Hole Science Stroll outreach event
USGS Oceanographer, Neil Ganju, at the 2017 Woods Hole Science Stroll
USGS Oceanographer, Neil Ganju, at the 2017 Woods Hole Science StrollWoods Hole Coastal and Marine Science Center Oceanographer, Neil Ganju, sharing science at the 2017 Woods Hole Science Stroll outreach event
Gerry Hatcher (left) and Shawn Harrison work on their video-camera station atop a hotel in Santa Cruz, California.
Gerry Hatcher (left) and Shawn Harrison work on their video-camera station atop a hotel in Santa Cruz, California.
Map of Edwin B Forsythe National Wildlife Refuge, N.J., marsh shoreline change rates.
Map of Edwin B Forsythe National Wildlife Refuge, N.J., marsh shoreline change rates.
Basemap of the United States with an overview image of elevation models
Basemap of the United States with an overview image of elevation models
Authigenic carbonate supplies the foundation for deep-sea corals, including colonies of bubblegum corals (Paragorgia) seen here.
Authigenic carbonate supplies the foundation for deep-sea corals, including colonies of bubblegum corals (Paragorgia) seen here.
Backscatter, bathymetry, and hill shaded relief maps
Backscatter, bathymetry, and hill shaded relief maps(A) Maximum Likelihood Classification (MLC) with two inputs, slope, and ISO-classified backscatter for the whole survey area. (B) MLC with five inputs, slope, ISO-classified backscatter, bathymetry, hillshaded-relief, and curvature.
Backscatter, bathymetry, and hill shaded relief maps
Backscatter, bathymetry, and hill shaded relief maps(A) Maximum Likelihood Classification (MLC) with two inputs, slope, and ISO-classified backscatter for the whole survey area. (B) MLC with five inputs, slope, ISO-classified backscatter, bathymetry, hillshaded-relief, and curvature.
Time series of the coral reef at Grecian Rocks (Key Largo, FL) illustrating an example of the dramatic decline in live coral on Florida Keys reefs in recent decades. From Shinn and Kuffner (2017).
Time series of the coral reef at Grecian Rocks (Key Largo, FL) illustrating an example of the dramatic decline in live coral on Florida Keys reefs in recent decades. From Shinn and Kuffner (2017).
Views of Cowells Beach in Santa Cruz, California, from a video
Views of Cowells Beach in Santa Cruz, California, from a videoViews of Cowells Beach in Santa Cruz, California, from a 10-minute video shot on May 6, 2017. Snapshot (first frame in video) on left; time-averaged image on right.
Views of Cowells Beach in Santa Cruz, California, from a video
Views of Cowells Beach in Santa Cruz, California, from a videoViews of Cowells Beach in Santa Cruz, California, from a 10-minute video shot on May 6, 2017. Snapshot (first frame in video) on left; time-averaged image on right.
Scientist with the system he designed to record precise photo data
Scientist with the system he designed to record precise photo dataGerry Hatcher with the system he designed to record the precise time and geographic location of each air photo Van Wagenen shoots.
Scientist with the system he designed to record precise photo data
Scientist with the system he designed to record precise photo dataGerry Hatcher with the system he designed to record the precise time and geographic location of each air photo Van Wagenen shoots.