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Coastal and Marine Hazards and Resources Program images.

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Image: Deep-Sea, Cold Water Coral
Deep-Sea, Cold Water Coral
Deep-Sea, Cold Water Coral
Deep-Sea, Cold Water Coral

Close-up image of the cold-water coral Lophelia pertusa, with polyps extended. The coral polyps eat by grabbing tiny suspended particulates (visible against the dark water background). The bright orange claws of a squat lobster (Eumunida picta) can be seen peeking out from behind the coral branches.

Close-up image of the cold-water coral Lophelia pertusa, with polyps extended. The coral polyps eat by grabbing tiny suspended particulates (visible against the dark water background). The bright orange claws of a squat lobster (Eumunida picta) can be seen peeking out from behind the coral branches.

Aerial images of the wilderness breach
Aerial images of the wilderness breach
Aerial images of the wilderness breach
Aerial images of the wilderness breach

Aerial images of the wilderness breach: a) Aerial photograph taken several days after Hurricane Sandy (photo credit: NOAA); b) Aerial mosaic of the breach in June 2015 showing the location of erosion on the ocean side of the breach and deposition that results in the seasonal formation of a spit.

Aerial images of the wilderness breach: a) Aerial photograph taken several days after Hurricane Sandy (photo credit: NOAA); b) Aerial mosaic of the breach in June 2015 showing the location of erosion on the ocean side of the breach and deposition that results in the seasonal formation of a spit.

Beach houses behind a sand dune at Cape Hatteras, North Carolina
Dunes, Beach Towns and Resilience
Dunes, Beach Towns and Resilience
Dunes, Beach Towns and Resilience

Sand dunes in Avon on Cape Hatteras, NC are the only separation between many beach house communities and the Atlantic Ocean. 

 

Sand dunes in Avon on Cape Hatteras, NC are the only separation between many beach house communities and the Atlantic Ocean. 

 

Underwater view of coral in some shades of pink where it is alive, shades of brown and green where it's dying.
Healthy vs. unhealthy corals
Healthy vs. unhealthy corals
Healthy vs. unhealthy corals

Underwater photograph off Molokaʻi Hawaiʻi, showing some of the impacts of land-based pollution, such as terrestrial sediment, on coral reefs: burial by sediment, algal overgrowth, and coral bleaching.

Underwater photograph off Molokaʻi Hawaiʻi, showing some of the impacts of land-based pollution, such as terrestrial sediment, on coral reefs: burial by sediment, algal overgrowth, and coral bleaching.

Gas hydrate at the seafloor on the U.S. Atlantic margin.
Gas hydrate at the seafloor on the U.S. Atlantic margin.
Gas hydrate at the seafloor on the U.S. Atlantic margin.
Gas hydrate at the seafloor on the U.S. Atlantic margin.

Gas hydrate at the seafloor on the U.S. Atlantic margin. The icy deposit formed as gas bubbles emitted from the seafloor transformed into methane hydrate beneath the overhanging rock.

Gas hydrate at the seafloor on the U.S. Atlantic margin. The icy deposit formed as gas bubbles emitted from the seafloor transformed into methane hydrate beneath the overhanging rock.

Aerial imagery sequence of Indian Point, Louisiana, showing shoreline erosion since 1950
Aerial imagery sequence of Indian Point, Louisiana, 1950–2012
Aerial imagery sequence of Indian Point, Louisiana, 1950–2012
Aerial imagery sequence of Indian Point, Louisiana, 1950–2012

Aerial imagery sequence of Indian Point, Louisiana, showing the contraction of the peninsula marsh in response to shoreline erosion since 1950.

Aerial imagery sequence of Indian Point, Louisiana, showing the contraction of the peninsula marsh in response to shoreline erosion since 1950.

USGS hydrologist and a Shinnecock Nation member work together gathering oyster and bed sediment samples
Gathering oyster and bed sediment samples along Long Island, NY
Gathering oyster and bed sediment samples along Long Island, NY
Gathering oyster and bed sediment samples along Long Island, NY

USGS hydrologist Kaitlyn Colella and a Shinnecock Nation member work together gathering oyster and bed sediment samples along Long Island, New York, coast.

Image showing a study area from Boston Harbor to the mouth of Cape Cod
Image showing a study area from Boston Harbor to the mouth of Cape Cod
Image showing a study area from Boston Harbor to the mouth of Cape Cod
Image showing a study area from Boston Harbor to the mouth of Cape Cod

Image showing a study area from Boston Harbor to the mouth of Cape Cod Bay including some images of geophysical and sample data available in the associated report.

Image showing a study area from Boston Harbor to the mouth of Cape Cod Bay including some images of geophysical and sample data available in the associated report.

map of acoustic backscatter intensity of the seafloor in Buzzards Bay, MA
Acoustic Backscatter Intensity
Acoustic Backscatter Intensity
Acoustic Backscatter Intensity

Acoustic backscatter intensity data are an indication of the relative hardness or softness of the sea floor, which is closely related to sediment texture and cohesion. The map shows acoustic backscatter intensity of the sea floor in the Buzzards Bay, Massachusetts.

Acoustic backscatter intensity data are an indication of the relative hardness or softness of the sea floor, which is closely related to sediment texture and cohesion. The map shows acoustic backscatter intensity of the sea floor in the Buzzards Bay, Massachusetts.

Photo of Sunset Beach, Florida, during tropical storm Colin in June 2016
Photo of Sunset Beach, Florida, during tropical storm Colin, June 2016
Photo of Sunset Beach, Florida, during tropical storm Colin, June 2016
Photo of Sunset Beach, Florida, during tropical storm Colin, June 2016

Photo of Sunset Beach, Florida, during tropical storm Colin in June 2016. The storm resulted in large waves and elevated water levels that caused erosion in this area, as can be seen in the scarp forming at the vegetation line. CMHRP researchers surveyed the elevation of the beach before and after the storm to quantify the storm's impacts.

Photo of Sunset Beach, Florida, during tropical storm Colin in June 2016. The storm resulted in large waves and elevated water levels that caused erosion in this area, as can be seen in the scarp forming at the vegetation line. CMHRP researchers surveyed the elevation of the beach before and after the storm to quantify the storm's impacts.

SEABOSS deployment from Ocean Survey Vessel Bold
SEABOSS deployment
SEABOSS deployment
SEABOSS deployment

 Left to right: Mike Bastoni (volunteer) and Lisa Engler (Massachusetts Bays Program) deploying the USGS-desgined SEABed Observation and Sampling System (SEABOSS) from Ocean Survey Vessel Bold, with Marinna Martini (USGS) running the winch

 Left to right: Mike Bastoni (volunteer) and Lisa Engler (Massachusetts Bays Program) deploying the USGS-desgined SEABed Observation and Sampling System (SEABOSS) from Ocean Survey Vessel Bold, with Marinna Martini (USGS) running the winch

Oblique-angle illustration showing the seafloor offshore of Half Moon Bay, California, with bumps of bedrock protruding.
Seafloor Offshore of Half Moon Bay
Seafloor Offshore of Half Moon Bay
Seafloor Offshore of Half Moon Bay

Perspective view of seafloor offshore of Half Moon Bay, showing scarp (arrows) along the eastern strand of the San Gregorio fault zone. Rocks are notably upwarped and folded adjacent to the fault.

Perspective view of seafloor offshore of Half Moon Bay, showing scarp (arrows) along the eastern strand of the San Gregorio fault zone. Rocks are notably upwarped and folded adjacent to the fault.

 Westco discrete nutrient analyzer
Westco discrete nutrient analyzer
Westco discrete nutrient analyzer
Westco discrete nutrient analyzer

 Westco discrete nutrient analyzer measures low-levels of nutrients in water samples

Hurricane Sandy created a breach in the Otis Pike High Dunes Wilderness Area at Fire Island National Seashore in NY
Hurricane Sandy created a breach in a barrier island
Hurricane Sandy created a breach in a barrier island
Hurricane Sandy created a breach in a barrier island

Extreme storms can drastically increase water levels and wave energy causing a breach, or complete erosion of the island itself. Hurricane Sandy created a breach in the Otis Pike High Dunes Wilderness Area at Fire Island National Seashore in NY.

Extreme storms can drastically increase water levels and wave energy causing a breach, or complete erosion of the island itself. Hurricane Sandy created a breach in the Otis Pike High Dunes Wilderness Area at Fire Island National Seashore in NY.

An aerial image of a barrier island showing sediment that has been eroded from dunes and beach and redeposited into the estuary.
Hurricane Sandy leveled dunes and moved sediment into the estuary
Hurricane Sandy leveled dunes and moved sediment into the estuary
Hurricane Sandy leveled dunes and moved sediment into the estuary

Hurricane Sandy leveled dunes and moved eroded sediment from the dunes and beach across the island and into the estuary (Great South Bay) at Fire Island, NY.

Hurricane Sandy leveled dunes and moved eroded sediment from the dunes and beach across the island and into the estuary (Great South Bay) at Fire Island, NY.

View looks up to the sky through a metal frame with tubes and instruments, and a woman wearing a hard hat is working on it.
Retrieving samples from a CTD
Retrieving samples from a CTD
Retrieving samples from a CTD

USGS scientist Nancy Prouty collects samples from a CTD. A CTD is package of electronic instruments that measure conductivity, temperature, and depth of water.

USGS scientist Nancy Prouty collects samples from a CTD. A CTD is package of electronic instruments that measure conductivity, temperature, and depth of water.

Image: Multichannel Seismic Streamer Repair on the Helo Deck
Multichannel Seismic Streamer Repair on the Helo Deck
Multichannel Seismic Streamer Repair on the Helo Deck
Multichannel Seismic Streamer Repair on the Helo Deck

The streamer is flaked out on the deck with a make shift workbench for tools.  The technical staff (Geological Survey of Canada) are sharing a lighter moment during trouble shooting and repair aboard CCGS Louis S. St-Laurent.

The streamer is flaked out on the deck with a make shift workbench for tools.  The technical staff (Geological Survey of Canada) are sharing a lighter moment during trouble shooting and repair aboard CCGS Louis S. St-Laurent.

Seafloor image showing depth with lots of text of explanation.
Shaded-relief bathymetry
Shaded-relief bathymetry
Shaded-relief bathymetry

Smaller version of Shaded-Relief Bathymetry (Sheet 2) from USGS Scientific Investigations Map 3225, California State Waters Map Series—Hueneme Canyon and Vicinity, California, as an example of the different kinds of maps (“sheets”) produced within a coastal map “block”.

Smaller version of Shaded-Relief Bathymetry (Sheet 2) from USGS Scientific Investigations Map 3225, California State Waters Map Series—Hueneme Canyon and Vicinity, California, as an example of the different kinds of maps (“sheets”) produced within a coastal map “block”.

Seafloor image showing depth with lots of text of explanation.
Shaded-relief bathymetry
Shaded-relief bathymetry
Shaded-relief bathymetry

Smaller version of Colored Shaded-Relief Bathymetry (Sheet 1) from USGS Scientific Investigations Map 3225, California State Waters Map Series—Hueneme Canyon and Vicinity, California, as an example of the different kinds of maps (“sheets”) produced within a coastal map “block”.

Smaller version of Colored Shaded-Relief Bathymetry (Sheet 1) from USGS Scientific Investigations Map 3225, California State Waters Map Series—Hueneme Canyon and Vicinity, California, as an example of the different kinds of maps (“sheets”) produced within a coastal map “block”.

Seafloor map shows the varied intensity of the sonar pulse returned to the ship depending on the substrate it encounters.
Acoustic backscatter
Acoustic backscatter
Acoustic backscatter

Smaller version of Acoustic Backscatter (Sheet 3) from USGS Scientific Investigations Map 3225, California State Waters Map Series—Hueneme Canyon and Vicinity, California, as an example of the different kinds of maps (“sheets”) produced within a coastal map “block”.

Smaller version of Acoustic Backscatter (Sheet 3) from USGS Scientific Investigations Map 3225, California State Waters Map Series—Hueneme Canyon and Vicinity, California, as an example of the different kinds of maps (“sheets”) produced within a coastal map “block”.

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