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Coastal and Marine Hazards and Resources Program images.

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Gentle river waters near grassy cliff in foreground, with a beach, and an amusement park in background, other buildings afar.
Santa Cruz Main Beach view from east
Santa Cruz Main Beach view from east
Santa Cruz Main Beach view from east

Panoramic view from the cliffs above the San Lorenzo River and east of the Santa Cruz Beach Boardwalk and Main Beach. Santa Cruz municipal pier and other buildings are visible in the background.

Panoramic view from the cliffs above the San Lorenzo River and east of the Santa Cruz Beach Boardwalk and Main Beach. Santa Cruz municipal pier and other buildings are visible in the background.

A man guides a data collection instrument, that is strapped to two large pontoons, out into water from the stern of a boat.
Chirp sub-bottom profiler deployment
Chirp sub-bottom profiler deployment
Chirp sub-bottom profiler deployment

USGS scientist Jackson Currie deploys a chirp sub-bottom profiler (in the center) from research vessel Parke Snavely. The chirp is attached to pontoons to keep the equipment from running aground in the shallow waters of San Pablo Bay, California.

USGS scientist Jackson Currie deploys a chirp sub-bottom profiler (in the center) from research vessel Parke Snavely. The chirp is attached to pontoons to keep the equipment from running aground in the shallow waters of San Pablo Bay, California.

A scientist pushes a push core into the sandy ground. A photograph and x-ray of the core are shown to the right.
Hand push core from barrier island, core photo, and X-ray
Hand push core from barrier island, core photo, and X-ray
Hand push core from barrier island, core photo, and X-ray

Cores can contain sediment units deposited in different environmental settings. Core photos and X-rays illuminate how sediment units can have contrasting color and density.  

Two people maneuver an apparatus suspended from a cable on the stern of a boat.
BOB Sled recovery on R/V Snavely
BOB Sled recovery on R/V Snavely
BOB Sled recovery on R/V Snavely

Scientists recover the Benthic OBservation camera Sled, or “BOB Sled,” onto the research vessel Parke Snavely

Image: Fire Coral Bleaching
Fire Coral Bleaching
Fire Coral Bleaching
Fire Coral Bleaching

Colonies of “blade fire coral” that have lost their symbiotic algae, or “bleached,” on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

Colonies of “blade fire coral” that have lost their symbiotic algae, or “bleached,” on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

Image: Bent Sea Rod Bleaching
Bent Sea Rod Bleaching
Bent Sea Rod Bleaching
Bent Sea Rod Bleaching

A colony of the soft coral known as the "bent sea rod" stands bleached on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

A colony of the soft coral known as the "bent sea rod" stands bleached on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

Image: Brain Coral Bleaching
Brain Coral Bleaching
Brain Coral Bleaching
Brain Coral Bleaching

No, that is not a mound of snow sitting on a coral reef – it is a colony of bleached "brain coral" on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

No, that is not a mound of snow sitting on a coral reef – it is a colony of bleached "brain coral" on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

View along a snowy, grassy coastal bluff that is slumping into the ocean, waves are right at the bottom of cliff.
Eroding coastal bluff on Barter Island
Eroding coastal bluff on Barter Island
Eroding coastal bluff on Barter Island

Photograph from a mounted time-lapse camera looking eastward along Barter Island’s north shore document how the coastal bluffs and beach changed during a single summer. The photograph shows a late-summer extreme storm with waves crashing into the bluff (September 3, 2014).

Photograph from a mounted time-lapse camera looking eastward along Barter Island’s north shore document how the coastal bluffs and beach changed during a single summer. The photograph shows a late-summer extreme storm with waves crashing into the bluff (September 3, 2014).

Timeline of past drilling activities
Gas Hydrates Drilling Activities
Gas Hydrates Drilling Activities
Gas Hydrates Drilling Activities

Timeline of past drilling activities conducted by countries, private sector firms, government agencies, and academe that have helped to refine global gas hydrate estimates and possible future drilling and production testing

Timeline of past drilling activities conducted by countries, private sector firms, government agencies, and academe that have helped to refine global gas hydrate estimates and possible future drilling and production testing

Schematic showing the general setting of seeps on the US Atlantic margin and related processes, such as gas hydrate degradation,
U.S. Atlantic Margin Seeps
U.S. Atlantic Margin Seeps
U.S. Atlantic Margin Seeps

Schematic showing the general setting of seeps on the US Atlantic margin and related processes, such as gas hydrate degradation, groundwater seepage, leakage through fractured rocks, or emissions from the seafloor overlying salt diapirs. Pockmarks shown in white, and the nominal updip limit of gas hydrate stability is represented by the dashed black line.

Schematic showing the general setting of seeps on the US Atlantic margin and related processes, such as gas hydrate degradation, groundwater seepage, leakage through fractured rocks, or emissions from the seafloor overlying salt diapirs. Pockmarks shown in white, and the nominal updip limit of gas hydrate stability is represented by the dashed black line.

Sample preparation and processing area
Sample preparation and processing area
Sample preparation and processing area
Sample preparation and processing area

Sample preparation and processing area in the K.O. Emery Geotechnical Wing at the Woods Hole Coastal and Marine Science Center, Woods Hole, MA

Arctica islandica shells
Arctica islandica shells
Arctica islandica shells
Arctica islandica shells

Three Arctica islandica shells that have been washed and set out to dry.                                     

Three Arctica islandica shells that have been washed and set out to dry.                                     

View along a grassy coastal bluff that is slumping into the ocean.
Eroding coastal bluff on Barter Island
Eroding coastal bluff on Barter Island
Eroding coastal bluff on Barter Island

Photograph from a mounted time-lapse camera looking eastward along Barter Island’s north shore document how the coastal bluffs and beach changed during a single summer. The photograph shows a summer storm from the west eroding the beach (July 25, 2014).

Photograph from a mounted time-lapse camera looking eastward along Barter Island’s north shore document how the coastal bluffs and beach changed during a single summer. The photograph shows a summer storm from the west eroding the beach (July 25, 2014).

Jen Suttles collects water samples from a salt marsh tidal creek (East Falmouth, MA) for laboratory analysis
Collecting samples from a salt marsh
Collecting samples from a salt marsh
Collecting samples from a salt marsh

Jen Suttles collects water samples from a salt marsh tidal creek (East Falmouth, MA) for laboratory analysis of total organic carbon.  These samples will be compared to data recorded by instrumentation deployed in an adjacent tidal creek as part of research efforts to quantify carbon dynamics in coastal ecosystems

Jen Suttles collects water samples from a salt marsh tidal creek (East Falmouth, MA) for laboratory analysis of total organic carbon.  These samples will be compared to data recorded by instrumentation deployed in an adjacent tidal creek as part of research efforts to quantify carbon dynamics in coastal ecosystems

The Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay National Estuarine Research Reserve
Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay, MA
Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay, MA
Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay, MA

The Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay National Estuarine Research Reserve serves as an important platform for research in coastal salt marshes. Infrastrucutre in this marsh allows researchers to access sites while maintaining habitat and platform health.

The Salt Marsh Observatory at Sage Lot Pond in the Waquoit Bay National Estuarine Research Reserve serves as an important platform for research in coastal salt marshes. Infrastrucutre in this marsh allows researchers to access sites while maintaining habitat and platform health.

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