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Coastal and Marine Hazards and Resources Program images.

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Image: Grizzly Bears Along Alaska's Coast
Grizzly Bears Along Alaska's Coast
Grizzly Bears Along Alaska's Coast
Grizzly Bears Along Alaska's Coast

This photograph shows two grizzly bears frolic on the tundra near the Avak River on the Chukchi Sea coast of Alaska. Coastal erosion along the Arctic coast is chronic, widespread and potentially accelerating, posing threats to infrastructure important for defense and energy purposes, natural shoreline habitats and nearby Native communities.

This photograph shows two grizzly bears frolic on the tundra near the Avak River on the Chukchi Sea coast of Alaska. Coastal erosion along the Arctic coast is chronic, widespread and potentially accelerating, posing threats to infrastructure important for defense and energy purposes, natural shoreline habitats and nearby Native communities.

Image: Scientists Explore Alaska's Coast
Scientists Explore Alaska's Coast
Scientists Explore Alaska's Coast
Scientists Explore Alaska's Coast

This photograph shows snow and ice melt along the rolling hills and coastal bluffs near Cape Sabine on the western Chukchi Sea coast of Alaska.

This photograph shows snow and ice melt along the rolling hills and coastal bluffs near Cape Sabine on the western Chukchi Sea coast of Alaska.

A small boat in a calm area of water with a spit of land in the distance, and snow-capped mountain peak in the far background.
PCMSC research vessel Parke Snavely on Nisqually Reach
PCMSC research vessel Parke Snavely on Nisqually Reach
PCMSC research vessel Parke Snavely on Nisqually Reach

USGS Pacific Coastal and Marine Science Center’s research vessel R/V Parke Snavely motors on the Nisqually Reach of Puget Sound.

View along the railroad tracks on Cape Canaveral
View along the railroad tracks on Cape Canaveral
View along the railroad tracks on Cape Canaveral
View along the railroad tracks on Cape Canaveral

Low dunes on Cape Canaveral often overwash during storm events, transporting sand landward. Critical infrastructure may be buried or flooded. In addition, significant landward transport of sand may lead to extensive shoreline erosion. 

Low dunes on Cape Canaveral often overwash during storm events, transporting sand landward. Critical infrastructure may be buried or flooded. In addition, significant landward transport of sand may lead to extensive shoreline erosion. 

A bottomfish with small, bright spots lazily swims over a rocky seafloor among a few small pieces of kelp.
Kelp Greenling in Half Moon Bay
Kelp Greenling in Half Moon Bay
Kelp Greenling in Half Moon Bay

Kelp greenling fish, about 8 inches long, swims above a seafloor of mixed gravel, cobble, and rock near Half Moon Bay, California.

Marinna Martini prepares to deploy tripods along the outer perimeter of Diamond Shoals, NC
Tripod deployment along the outer perimeter of Diamond Shoals, NC
Tripod deployment along the outer perimeter of Diamond Shoals, NC
Tripod deployment along the outer perimeter of Diamond Shoals, NC

Marinna Martini, Woods Hole, Coastal and Marine Science Center,  prepares to deploy tripods at three sites along the outer perimeter of Diamond Shoals, North Carolina.

Shaded relief and combined bathymetry map of Puerto Rico
Shaded relief and combined bathymetry map of Puerto Rico
Shaded relief and combined bathymetry map of Puerto Rico
Shaded relief and combined bathymetry map of Puerto Rico

(Top image) Shaded relief of the new multibeam bathymetry along the Puerto Rico Trench illuminated from the northwest. Thin contours indicate bathymetry at 500-m intervals. (Bottom image) Combined bathymetry map of the multibeam bathymetry data, single-beam bathymetry compilation around Puerto Rico, Lidar data near shore, and topography of Puerto Rico.

(Top image) Shaded relief of the new multibeam bathymetry along the Puerto Rico Trench illuminated from the northwest. Thin contours indicate bathymetry at 500-m intervals. (Bottom image) Combined bathymetry map of the multibeam bathymetry data, single-beam bathymetry compilation around Puerto Rico, Lidar data near shore, and topography of Puerto Rico.

Photograph of USGS scientists standing in front of a helicopter
Remote places
Remote places
Remote places

Woods Hole Coastal and Marine Science Center's Ellyn Montgomery (right) on the helipad of the Canadian Coast Guard Vessel Louis St. Laurent returning from an ice reconnaissance flight as part of a joint study mapping the foot of the continental slope in the Arctic Ocean in 2008

Woods Hole Coastal and Marine Science Center's Ellyn Montgomery (right) on the helipad of the Canadian Coast Guard Vessel Louis St. Laurent returning from an ice reconnaissance flight as part of a joint study mapping the foot of the continental slope in the Arctic Ocean in 2008

Map indicating locations of personnel involved in the Gas Hydrates Project
Gas Hydrates Project personnel location map.
Gas Hydrates Project personnel location map.
Gas Hydrates Project personnel location map.

The USGS Gas Hydrates Project integrates across USGS mission areas, programs, and regions. The stars indicate the locations of personnel involved in the Gas Hydrates Project. Within the US, much of the research focuses on the Gulf of America and Alaska, which represent marine and permafrost-associated settings for gas hydrates, respectively.

The USGS Gas Hydrates Project integrates across USGS mission areas, programs, and regions. The stars indicate the locations of personnel involved in the Gas Hydrates Project. Within the US, much of the research focuses on the Gulf of America and Alaska, which represent marine and permafrost-associated settings for gas hydrates, respectively.

Static stress change models
Static stress change models
Static stress change models
Static stress change models

Static stress change models for known or hypothesized faults in the Hispaniola and Puerto Rico subduction segments due to (a) slip on a patch of the Puerto Rico subduction zone, and (b) slip on a patch of the Hispaniola subduction zone. An open arrow denotes slip direction and the patches are marked by dashed rectangles.

Static stress change models for known or hypothesized faults in the Hispaniola and Puerto Rico subduction segments due to (a) slip on a patch of the Puerto Rico subduction zone, and (b) slip on a patch of the Hispaniola subduction zone. An open arrow denotes slip direction and the patches are marked by dashed rectangles.

A very close-up photo of sand grains from the Grand Canyon River, with a centimeter scale drawn on top.
Grand Canyon sand
Grand Canyon sand
Grand Canyon sand

Grand Canyon sand was photographed with a hand-held point-and-shoot camera in a waterproof housing.

Grand Canyon sand was photographed with a hand-held point-and-shoot camera in a waterproof housing.

A person wearing scuba gear positions an underwater instrument package on the seafloor.
Installing oceanographic monitoring instrumentation on the seafloor
Installing oceanographic monitoring instrumentation on the seafloor
Installing oceanographic monitoring instrumentation on the seafloor

USGS research geologist Curt Storlazzi installs an instrument package on the seafloor of Maunalua Bay, Oʻahu. The platform, called a MiniPROBE, hosts six upward-looking acoustic Doppler current profilers (ADCP), seven conductivity and temperature (CT) sensors, and eight self-logging optical backscatter sensors (SLOBS).

USGS research geologist Curt Storlazzi installs an instrument package on the seafloor of Maunalua Bay, Oʻahu. The platform, called a MiniPROBE, hosts six upward-looking acoustic Doppler current profilers (ADCP), seven conductivity and temperature (CT) sensors, and eight self-logging optical backscatter sensors (SLOBS).

Scientists operate scientific sediment coring equipment with a tall metal barrel and tripod on a sandy beach near the water.
USGS staff collecting vibracore on Ft. DeSoto Beach, Florida
USGS staff collecting vibracore on Ft. DeSoto Beach, Florida
USGS staff collecting vibracore on Ft. DeSoto Beach, Florida

USGS staff collecting a sediment core on Ft. Desoto Beach, Florida using vibracoring equipment. This type of sediment coring uses the vibration of an electric motor to sink an aluminum core barrel into the ground. When the core barrel enters the ground the sediment in the ground fills up the barrel and the crew uses the tripod to pull the core out of the ground.

USGS staff collecting a sediment core on Ft. Desoto Beach, Florida using vibracoring equipment. This type of sediment coring uses the vibration of an electric motor to sink an aluminum core barrel into the ground. When the core barrel enters the ground the sediment in the ground fills up the barrel and the crew uses the tripod to pull the core out of the ground.

Photograph of  Instrumented Pressure Testing Chamber body
Instrumented Pressure Testing Chamber
Instrumented Pressure Testing Chamber
Instrumented Pressure Testing Chamber

A pressurized, stable, hydrate-bearing sediment core can be fed through the IPTC body, shown here being used in Singapore to support the Indian National Gas Hydrates Program (NGHP1)

A pressurized, stable, hydrate-bearing sediment core can be fed through the IPTC body, shown here being used in Singapore to support the Indian National Gas Hydrates Program (NGHP1)

People stand on the stern of a boat while launching equipment into the water.
Deploying the poking eyeball
Deploying the poking eyeball
Deploying the poking eyeball

USGS scientists from the Pacific Coastal and Marine Science Center (PCMSC) in Santa Cruz, California deploy an instrument called the poking eyeball. The system, developed by PCMSC, was designed to take repetitive microscopic images of the seabed from a tripod on the seafloor.

USGS scientists from the Pacific Coastal and Marine Science Center (PCMSC) in Santa Cruz, California deploy an instrument called the poking eyeball. The system, developed by PCMSC, was designed to take repetitive microscopic images of the seabed from a tripod on the seafloor.

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