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Coastal and Marine Hazards and Resources Program images.

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Map of a bay with islands near a city has an overlay to show the extent of flooding given a huge storm event.
Mission Bay San Diego flooding scenario
Mission Bay San Diego flooding scenario
Mission Bay San Diego flooding scenario

Estimated coastal inundation (blue shading) at Mission Bay in San Diego, California, using the Coastal Storm Modeling System (CoSMoS) developed for ARkStorm. (From USGS Open-File Report 2010-1312.) 

Estimated coastal inundation (blue shading) at Mission Bay in San Diego, California, using the Coastal Storm Modeling System (CoSMoS) developed for ARkStorm. (From USGS Open-File Report 2010-1312.) 

An illustrated city street with buildings, cars, and a person all in standing water during a rain storm.
ARkStorm scenario
ARkStorm scenario
ARkStorm scenario

The ARkStorm scenario led by the USGS and hundreds of scientists and experts from many disciplines details impacts of a scientifically plausible storm similar to the Great California Storm of 1862 in the modern day.

The ARkStorm scenario led by the USGS and hundreds of scientists and experts from many disciplines details impacts of a scientifically plausible storm similar to the Great California Storm of 1862 in the modern day.

Comparison of observed near-bed velocities and modeled near-bed velocities using several bottom-roughness formulations.
Comparison of observed near-bed velocities and modeled near-bed veloci
Comparison of observed near-bed velocities and modeled near-bed veloci
Comparison of observed near-bed velocities and modeled near-bed veloci

Comparison of observed near-bed velocities and modeled near-bed velocities using several bottom-roughness formulations. Velocity vectors are overlaid on map of backscatter from the sea floor showing regions with coarse sand (light color) and fine sand (dark colors). White lines are bathymetry contours.

Comparison of observed near-bed velocities and modeled near-bed velocities using several bottom-roughness formulations. Velocity vectors are overlaid on map of backscatter from the sea floor showing regions with coarse sand (light color) and fine sand (dark colors). White lines are bathymetry contours.

Hydrate Molecule
Hydrate Molecule
Hydrate Molecule
Hydrate Molecule

Water molecules (1 red oxygen and 2 white hydrogens) form a pentagonal dodecahedron around a methane molecule (1 gray carbon and 4 green hydrogens). This represents 2 of the 8 parts of the typical Structure I gas hydrate molecule.

Water molecules (1 red oxygen and 2 white hydrogens) form a pentagonal dodecahedron around a methane molecule (1 gray carbon and 4 green hydrogens). This represents 2 of the 8 parts of the typical Structure I gas hydrate molecule.

Topography and bathymetry map of the Northeastern Caribbean.
Topography and bathymetry map of the Northeastern Caribbean.
Topography and bathymetry map of the Northeastern Caribbean.
Topography and bathymetry map of the Northeastern Caribbean.

Map of the Northeastern Caribbean: topography is in shades of green and bathymetry in shades of blue. Fault traces are shown as lines with the following descriptions: barbed=thrust fault; solid=strike-slip fault with arrows showing relative direction of motion; black and white=normal fault. Faults outlined in red have a potential to generate a large earthquake.

Map of the Northeastern Caribbean: topography is in shades of green and bathymetry in shades of blue. Fault traces are shown as lines with the following descriptions: barbed=thrust fault; solid=strike-slip fault with arrows showing relative direction of motion; black and white=normal fault. Faults outlined in red have a potential to generate a large earthquake.

Simulation model for geomorphic change
Simulation Model
Simulation Model
Simulation Model

Simulation results for geomorphic change in Suisun Bay, CA (Ganju and Schoellhamer, 2010)

 Instrumented Pressure Testing Chamber (IPTC)
Instrumented Pressure Testing Chamber (IPTC)
Instrumented Pressure Testing Chamber (IPTC)
Instrumented Pressure Testing Chamber (IPTC)

The Instrumented Pressure Testing Chamber (IPTC). A device for measuring the physical properties of naturally-occurring, hydrate-bearing sediment at nearly in situ pressure conditions

The Instrumented Pressure Testing Chamber (IPTC). A device for measuring the physical properties of naturally-occurring, hydrate-bearing sediment at nearly in situ pressure conditions

Topographic and bathymetric map of the island of Hispaniola.
Topographic and bathymetric map of the island of Hispaniola.
Topographic and bathymetric map of the island of Hispaniola.
Topographic and bathymetric map of the island of Hispaniola.

Map of the island of Hispaniola that include the countries of Haiti and the Dominican Republic. Fault traces are shown as lines with the following descriptions: barbed=thrust fault; solid=strike-slip fault with arrows showing relative direction of motion; black and white=normal fault.

Map of the island of Hispaniola that include the countries of Haiti and the Dominican Republic. Fault traces are shown as lines with the following descriptions: barbed=thrust fault; solid=strike-slip fault with arrows showing relative direction of motion; black and white=normal fault.

"Sea Level Rise, Subsidence, and Wetland Loss" video screenshot
"Sea Level Rise, Subsidence, and Wetland Loss" video screenshot
"Sea Level Rise, Subsidence, and Wetland Loss" video screenshot
"Sea Level Rise, Subsidence, and Wetland Loss" video screenshot

Sea Level Rise, Subsidence, and Wetland Loss. This video describes causes of wetland loss in the Mississippi River Delta. Rapid land subsidence due to sediment compaction and dewatering increases the rate of submergence in this deltaic system.

Sea Level Rise, Subsidence, and Wetland Loss. This video describes causes of wetland loss in the Mississippi River Delta. Rapid land subsidence due to sediment compaction and dewatering increases the rate of submergence in this deltaic system.

Methane seeping on the Virginia margin just shallower than the limit for gas hydrate stability.
Methane seeping
Methane seeping
Methane seeping

Methane seeping on the Virginia margin just shallower than the limit for gas hydrate stability. 

Methane seeping on the Virginia margin just shallower than the limit for gas hydrate stability. 

R/V Rafael
R/V Rafael
R/V Rafael
R/V Rafael

The R/V Rafael performs nearshore geophysical surveys, and includes high resolution sub-bottom profiling, sidescan sonar, and multibeam echosounding in its arsenal of survey capabilities.

The R/V Rafael performs nearshore geophysical surveys, and includes high resolution sub-bottom profiling, sidescan sonar, and multibeam echosounding in its arsenal of survey capabilities.

Many walruses on a beach, with a photographer laying on the sand.
Photographer on the beach with a tagged walrus
Photographer on the beach with a tagged walrus
Photographer on the beach with a tagged walrus

Tony Fischbach (USGS) on the beach with a tagged walrus near Point Lay, Alaska, on September 1, 2010. Walruses gathered on Alaskan shores of the Chukchi Sea by the tens of thousands in late August and September 2010 after the last of the sea ice dissipated.

Tony Fischbach (USGS) on the beach with a tagged walrus near Point Lay, Alaska, on September 1, 2010. Walruses gathered on Alaskan shores of the Chukchi Sea by the tens of thousands in late August and September 2010 after the last of the sea ice dissipated.

Photo of bleaching colony of massive starlet coral, Siderastrea siderea, Florida Keys.
Bleaching colony of massive starlet coral, Siderastrea siderea
Bleaching colony of massive starlet coral, Siderastrea siderea
Bleaching colony of massive starlet coral, Siderastrea siderea

Bleaching colony of massive starlet coral, Siderastrea siderea, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Bleaching colony of massive starlet coral, Siderastrea siderea, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Photo of bleaching colony of elliptical star coral, Dichocoenia stokesii, Florida Keys.
Bleaching colony of elliptical star coral, Dichocoenia stokesii
Bleaching colony of elliptical star coral, Dichocoenia stokesii
Bleaching colony of elliptical star coral, Dichocoenia stokesii

Bleaching colony of elliptical star coral, Dichocoenia stokesii, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Bleaching colony of elliptical star coral, Dichocoenia stokesii, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Photo of bleaching colony of symmetrical brain coral, Diploria strigosa
Bleaching colony of symmetrical brain coral, Diploria strigosa
Bleaching colony of symmetrical brain coral, Diploria strigosa
Bleaching colony of symmetrical brain coral, Diploria strigosa

Bleaching colony of symmetrical brain coral, Diploria strigosa, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Bleaching colony of symmetrical brain coral, Diploria strigosa, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Photo of bleaching colony of lobed star coral, Montastraea annularis
Bleaching colony of lobed star coral, Montastraea annularis
Bleaching colony of lobed star coral, Montastraea annularis
Bleaching colony of lobed star coral, Montastraea annularis

Bleaching colony of lobed star coral, Montastraea annularis, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Bleaching colony of lobed star coral, Montastraea annularis, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

bleaching colony of star coral
Bleaching colonies of mountainous star coral, Montastraea faveolata
Bleaching colonies of mountainous star coral, Montastraea faveolata
Bleaching colonies of mountainous star coral, Montastraea faveolata

Bleaching colonies of mountainous star coral, Montastraea faveolata, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

Bleaching colonies of mountainous star coral, Montastraea faveolata, Florida Keys. When corals are stressed, the symbiosis between the coral animal and its photosynthetic algal symbionts (zooxanthellae) breaks down and the zooxanthellae are expelled from the coral tissue.

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