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Coastal and Marine Hazards and Resources Program images.

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View looks out across a verdant marsh with a sinuous water channel running through it, a large body of water in background.
China Camp State Park marsh
China Camp State Park marsh
China Camp State Park marsh

Estuarine salt marsh at China Camp State Park looking towards San Pablo Bay, northern San Francisco, California.

Estuarine salt marsh at China Camp State Park looking towards San Pablo Bay, northern San Francisco, California.

Image: Deep Sea Crab on Mussels a Mile Below Atlantic Ocean
Deep Sea Crab on Mussels a Mile Below Atlantic Ocean
Deep Sea Crab on Mussels a Mile Below Atlantic Ocean
Deep Sea Crab on Mussels a Mile Below Atlantic Ocean

A lithodid crab seen on a bed of deep sea mussels living near a gas seep 1,600 meters below the surface of the Atlantic Ocean. Images courtesy Deepwater Canyons 2013 - Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

A lithodid crab seen on a bed of deep sea mussels living near a gas seep 1,600 meters below the surface of the Atlantic Ocean. Images courtesy Deepwater Canyons 2013 - Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

Image: ROC Sampling Deep Sea Urchin
ROC Sampling Deep Sea Urchin
ROC Sampling Deep Sea Urchin
ROC Sampling Deep Sea Urchin

Images of the remotely operated vehicle Jason2 sampling a sea urchin in a deep sea mussel community found near a gas seep on the U.S. outer continental shelf. Images courtesy Deepwater Canyons 2013 - Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

Images of the remotely operated vehicle Jason2 sampling a sea urchin in a deep sea mussel community found near a gas seep on the U.S. outer continental shelf. Images courtesy Deepwater Canyons 2013 - Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

Photo of bubbles rising through the water from the seafloor.
Methane bubbles rise from the seafloor
Methane bubbles rise from the seafloor
Methane bubbles rise from the seafloor

Methane gas bubbles rise from the seafloor—this type of activity, originally noticed by NOAA Ship Okeanos Explorer in 2012 on a multibeam sonar survey, is what led scientists to the area. Image courtesy of Deepwater Canyons 2013 – Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

Methane gas bubbles rise from the seafloor—this type of activity, originally noticed by NOAA Ship Okeanos Explorer in 2012 on a multibeam sonar survey, is what led scientists to the area. Image courtesy of Deepwater Canyons 2013 – Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS.

Adrian Mann is using a piezometer to extract submarine groundwater to analyze for geochemical parameters in Indian River Bay, DE
Groundwater collection using a piezometer
Groundwater collection using a piezometer
Groundwater collection using a piezometer

Adrian Mann is using a piezometer to extract submarine groundwater to analyze for geochemical parameters in Indian River Bay, DE.

Survey vessel in Barnegat Bay, NJ during a beautiful sunset
Survey vessel in Barnegat Bay, NJ during a beautiful sunset
Survey vessel in Barnegat Bay, NJ during a beautiful sunset
Survey vessel in Barnegat Bay, NJ during a beautiful sunset

Assessing how storms move sediment during storms provides coastal scientists and managers the information they need to keep coastal communities safe and prosperous. And, lucky for us, provides many opportunities to see great coastal sunsets!

Assessing how storms move sediment during storms provides coastal scientists and managers the information they need to keep coastal communities safe and prosperous. And, lucky for us, provides many opportunities to see great coastal sunsets!

Water running through a dam on a river.
San Clemente Dam in 2013
San Clemente Dam in 2013
San Clemente Dam in 2013

The San Clemente Dam, built in the 1920s on the Carmel River in Monterey County, California, was removed during 2014 and 2015.

The San Clemente Dam, built in the 1920s on the Carmel River in Monterey County, California, was removed during 2014 and 2015.

A view from a boat shows a house that was moved into estuary waters during Hurricane Sandy.
Hurricane Sandy moved a house from barrier island to estuary
Hurricane Sandy moved a house from barrier island to estuary
Hurricane Sandy moved a house from barrier island to estuary

Hurricane Sandy moved a house from barrier island to estuary, in this case into Barnegat Bay, NJ. Waves from extreme storms do the same with barrier island sediment.

Debris from Hurricane Sandy is piled up behind an artificial dune, built to protect the island from the winter storm season
Debris from Hurricane Sandy is piled up behind an artificial dune
Debris from Hurricane Sandy is piled up behind an artificial dune
Debris from Hurricane Sandy is piled up behind an artificial dune

Debris from Hurricane Sandy (Seaside Heights, NJ) is piled up behind an artificial dune in order to protect island infrastructure from the subsequent winter storm season. Like storms, humans change coasts too.

Surveying A Barrier Island Evolution Research (BIER) program study site in the Chandeleur Islands
Surveying program study site in the Chandeleur Islands
Surveying program study site in the Chandeleur Islands
Surveying program study site in the Chandeleur Islands

Surveying A Barrier Island Evolution Research (BIER) program study site in the Chandeleur Islands in 2013. The survey data is used to map the pre-storm conditions.
 

A scuba diver underwater with scientific equipment
Legna Torres-Garcia
Legna Torres-Garcia
Legna Torres-Garcia

USGS Graduate Research Assistant Legna Torres-Garcia installs a temperature logger on a coral reef in Dry Tortugas National Park. She and her team deployed a vertical array with temperature loggers every 1m from the seabed to near-surface with the goal to capture any changes in temperature through time and across depth.

USGS Graduate Research Assistant Legna Torres-Garcia installs a temperature logger on a coral reef in Dry Tortugas National Park. She and her team deployed a vertical array with temperature loggers every 1m from the seabed to near-surface with the goal to capture any changes in temperature through time and across depth.

Drone footage taken of the Woods Hole Oceanographic facility
Drone footage of Woods Hole Oceanographic facility
Drone footage of Woods Hole Oceanographic facility
Drone footage of Woods Hole Oceanographic facility

Drone footage taken of the Woods Hole Oceanographic facility on the Quissett campus in Woods Hole Ma.  This is an example of a tidally restricted marsh system cutoff from tidal flows by the bike path.

Drone footage taken of the Woods Hole Oceanographic facility on the Quissett campus in Woods Hole Ma.  This is an example of a tidally restricted marsh system cutoff from tidal flows by the bike path.

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.

Image: Deep-Sea Coral: Lophelia pertusa
Deep-Sea Coral: Lophelia pertusa
Deep-Sea Coral: Lophelia pertusa
Deep-Sea Coral: Lophelia pertusa

Live Lophelia pertusa is white because the calcium carbonate skeleton shows through the nonpigmented coral tissue. Dead coral is soon covered in a brown biofilm. The red-orange squat lobster (Eumunida picta) in the center of the photo is prepared to catch its dinner.

Live Lophelia pertusa is white because the calcium carbonate skeleton shows through the nonpigmented coral tissue. Dead coral is soon covered in a brown biofilm. The red-orange squat lobster (Eumunida picta) in the center of the photo is prepared to catch its dinner.

Grid of photomicrographs and sketches of foraminifera.
Trochammina hadai Uchio
Trochammina hadai Uchio
Trochammina hadai Uchio

Figure 2 from the 2012 publication, "Arrival and Expansion of the Invasive Foraminifera Trochammina hadai Uchio in Padilla Bay, Washington," by McGann, et al. Trochammina hadai Uchio: A, dorsal view; B, edge view; C, ventral view.

Figure 2 from the 2012 publication, "Arrival and Expansion of the Invasive Foraminifera Trochammina hadai Uchio in Padilla Bay, Washington," by McGann, et al. Trochammina hadai Uchio: A, dorsal view; B, edge view; C, ventral view.

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.

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.

A man bends over instruments and pipes near the water on a dock.
Servicing continuous monitoring instruments
Servicing continuous monitoring instruments
Servicing continuous monitoring instruments

USGS hydrologic technician Kurt Weidich services continuous monitoring instruments at the Dumbarton Bridge in south San Francisco Bay.

USGS hydrologic technician Kurt Weidich services continuous monitoring instruments at the Dumbarton Bridge in south San Francisco Bay.

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