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Pacific Coastal and Marine Science Center images.

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Series of diagrams with arrows from left to right, how data visualization tool goes from a global to regional to local scale.
How projections in CoSMoS work
How projections in CoSMoS work
How projections in CoSMoS work

CoSMoS’s approach to projecting flood hazards: global winds, waves, tides, and anomalous water levels are scaled down to the local scale for  projecting nearshore wave heights, flooding, and shoreline change, including beach erosion and cliff failures.

Learn more at usgs.gov/cosmos

CoSMoS’s approach to projecting flood hazards: global winds, waves, tides, and anomalous water levels are scaled down to the local scale for  projecting nearshore wave heights, flooding, and shoreline change, including beach erosion and cliff failures.

Learn more at usgs.gov/cosmos

Map shows a coastal city with an airport and how, during a large storm, ocean water would flood around city features.
CoSMoS projection for San Diego
CoSMoS projection for San Diego
CoSMoS projection for San Diego

Example of CoSMoS projected flooding extents for a 1.5 meter sea level rise in combination with possible 100 year return period coastal storms.

Example of CoSMoS projected flooding extents for a 1.5 meter sea level rise in combination with possible 100 year return period coastal storms.

Underwater photograph looking across a reef of jagged corals, and looking up at the surface of the water with visible ripples.
Underwater photo of coral reef, Tutuila Island
Underwater photo of coral reef, Tutuila Island
Underwater photo of coral reef, Tutuila Island

Underwater photograph showing corals in Tāfeu Cove, National Park of American Samoa, north shore of Tutuila Island, American Samoa.

“Variance” images derived from videos of Madeira Beach (left) and Cowells Beach (right)
“Variance” images derived from videos of beaches studied
“Variance” images derived from videos of beaches studied
“Variance” images derived from videos of beaches studied

“Variance” images derived from the same videos used in the studies. Left, Madeira Beach; right, Cowells Beach. In a variance image, the more variation in light intensity at a given pixel, the brighter the value assigned to that pixel. Bright areas indicate many changes in light intensity, caused by a lot of movement.

“Variance” images derived from the same videos used in the studies. Left, Madeira Beach; right, Cowells Beach. In a variance image, the more variation in light intensity at a given pixel, the brighter the value assigned to that pixel. Bright areas indicate many changes in light intensity, caused by a lot of movement.

3 close-up views of the toe of the Mud Creek landslide created from air photos after the landslide
3 close-up views of the toe of the Mud Creek landslide
3 close-up views of the toe of the Mud Creek landslide
3 close-up views of the toe of the Mud Creek landslide

Close-up views of the toe of the Mud Creek landslide created from air photos taken May 27 (top), June 13 (middle), and June 26 (bottom). Caltrans built roads on top of the slide for assessment and monitoring activities.

Close-up views of the toe of the Mud Creek landslide created from air photos taken May 27 (top), June 13 (middle), and June 26 (bottom). Caltrans built roads on top of the slide for assessment and monitoring activities.

Topographic-change image produced by comparing 3D map derived from May 27 air photos with that derived from June 13 air photos
Topographic-change image produced by comparing subsequent 3D maps
Topographic-change image produced by comparing subsequent 3D maps
Topographic-change image produced by comparing subsequent 3D maps

Topographic-change image produced by comparing 3D map derived from May 27 air photos with that derived from June 13 air photos. Note that material has eroded from the seaward edge of the toe (yellow and orange tones), and material has built up on beaches to either side of the slide (blue tones).

Topographic-change image produced by comparing 3D map derived from May 27 air photos with that derived from June 13 air photos. Note that material has eroded from the seaward edge of the toe (yellow and orange tones), and material has built up on beaches to either side of the slide (blue tones).

Brown lines across the image describe the fault, with labeled features, depth, and width
Multichannel seismic-reflection profile from Queen Charlotte-Fault
Multichannel seismic-reflection profile from Queen Charlotte-Fault
Multichannel seismic-reflection profile from Queen Charlotte-Fault

Multichannel seismic-reflection profile across the Queen Charlotte-Fairweather fault, acquired aboard the R/V Norseman in August 2016. Dashed red line in enlarged section at lower right is the Queen Charlotte-Fairweather fault. m, meter; km, kilometer; ms, millisecond.

Multichannel seismic-reflection profile across the Queen Charlotte-Fairweather fault, acquired aboard the R/V Norseman in August 2016. Dashed red line in enlarged section at lower right is the Queen Charlotte-Fairweather fault. m, meter; km, kilometer; ms, millisecond.

Photo of a laboratory with various equipment and tables to work on.
PCMSC Marine Minerals Laboratory
PCMSC Marine Minerals Laboratory
PCMSC Marine Minerals Laboratory

A look into the USGS Pacific Coastal and Marine Science Center’s Marine Minerals Laboratory Suite.

Underwater photo of a vast area of dead corals on the seafloor at Buck Island, U.S. Virgin Islands
Some elkhorn corals in the U.S. Virgin Islands have died
Some elkhorn corals in the U.S. Virgin Islands have died
Some elkhorn corals in the U.S. Virgin Islands have died

Elkhorn corals (Acropora palmata) on the seafloor along the northeastern coast of Buck Island, U.S. Virgin Islands, have died and collapsed into rubble. As coral reef structure degrades, habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves, and erosion.

Elkhorn corals (Acropora palmata) on the seafloor along the northeastern coast of Buck Island, U.S. Virgin Islands, have died and collapsed into rubble. As coral reef structure degrades, habitat for marine life is lost and nearby coastlines become more susceptible to storms, waves, and erosion.

A view of healthy elkhorn corals on the seafloor in the U.S. Virgin Islands
Healthy elkhorn coral on the seafloor in the U.S. Virgin Islands
Healthy elkhorn coral on the seafloor in the U.S. Virgin Islands
Healthy elkhorn coral on the seafloor in the U.S. Virgin Islands

Healthy elkhorn coral (Acropora palmata) on the seafloor along the southeastern coast of Buck Island, U.S. Virgin Islands. Elkhorn coral is one of many important reef-building species that create 3D structure on the seafloor. Coral reef structure provides habitat for marine life and helps break up waves as they approach the coastline.

Healthy elkhorn coral (Acropora palmata) on the seafloor along the southeastern coast of Buck Island, U.S. Virgin Islands. Elkhorn coral is one of many important reef-building species that create 3D structure on the seafloor. Coral reef structure provides habitat for marine life and helps break up waves as they approach the coastline.

3 different views created using multibeam bathymetry data show the fault in bright colors
Perspective views of multibeam bathymetry data acquired by the USGS
Perspective views of multibeam bathymetry data acquired by the USGS
Perspective views of multibeam bathymetry data acquired by the USGS

Perspective views of multibeam bathymetry data acquired by the USGS aboard the R/V Medeia. Shallower depths in red. Arrows point to the distinct line in the seafloor associated with the Queen Charlotte-Fairweather fault.

Two maps; the left hand one shows brown land, blue water, and red arrows. The right hand one shows colored survey tracklines
Maps with key features and shaded relief of the study area
Maps with key features and shaded relief of the study area
Maps with key features and shaded relief of the study area

Left: Key features in and around the Gulf of Alaska. A black rectangle outlines our 2016 study area along the Queen Charlotte-Fairweather fault. Red arrows indicate relative tectonic plate motions. Right: A shaded relief map of the 2016 study area. Rainbow colors show seafloor depths acquired by the USGS in 2015 and 2016. Red indicates shallower depths.

Left: Key features in and around the Gulf of Alaska. A black rectangle outlines our 2016 study area along the Queen Charlotte-Fairweather fault. Red arrows indicate relative tectonic plate motions. Right: A shaded relief map of the 2016 study area. Rainbow colors show seafloor depths acquired by the USGS in 2015 and 2016. Red indicates shallower depths.

A very calm river in the woods with a gravel beach and lots of lush trees around.
Carmel River by Sleepy Hollow reach
Carmel River by Sleepy Hollow reach
Carmel River by Sleepy Hollow reach

Photograph of Carmel River near the Sleepy Hollow reach. San Clemente Dam was built on Carmel River in 1921 to supply water locally. After being declared seismically unfit, plans to remove the dam began. It was completely removed in 2015.

Photograph of Carmel River near the Sleepy Hollow reach. San Clemente Dam was built on Carmel River in 1921 to supply water locally. After being declared seismically unfit, plans to remove the dam began. It was completely removed in 2015.

The pilot and plane used to take air photos for the USGS

Pilot Bob Van Wagenen and the Cessna 182R he flies when taking air photos for the USGS Remote Sensing Coastal Change Project.

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