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Coastal and Marine Hazards and Resources Program images.

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Oblique aerial view of a coastline with eroding bluff, part of the bluff has been anchored with large, black sand-filled bags.
Long Range Radar Site on Barter Island
Long Range Radar Site on Barter Island
Long Range Radar Site on Barter Island

An oblique aerial photograph shows the currently active Long Range Radar Site on Barter Island, formerly a DEW Line (Distant Early Warning) station that was deactivated in 1990. The Cold War-era landfill in the foreground of the photograph was at immediate risk from coastal erosion in 2006 and has since been relocated farther inland.

An oblique aerial photograph shows the currently active Long Range Radar Site on Barter Island, formerly a DEW Line (Distant Early Warning) station that was deactivated in 1990. The Cold War-era landfill in the foreground of the photograph was at immediate risk from coastal erosion in 2006 and has since been relocated farther inland.

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

This oblique aerial photograph is of Flaxman Island off the Alaska coast and shows a tapped thermokarst lakes, caribou tracks and ice-rich bluffs that are eroding.

This oblique aerial photograph is of Flaxman Island off the Alaska coast and shows a tapped thermokarst lakes, caribou tracks and ice-rich bluffs that are eroding.

Image: Eroding Shoreline Along Alaska's Coast
Eroding Shoreline Along Alaska's Coast
Eroding Shoreline Along Alaska's Coast
Eroding Shoreline Along Alaska's Coast

This photograph shows ice-wedge polygons and an eroding shoreline at Cape Halkett on the Beaufort 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 ice-wedge polygons and an eroding shoreline at Cape Halkett on the Beaufort 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.

Thermokarst lakes in Alaska
Thermokarst lakes in Alaska
Thermokarst lakes in Alaska
Thermokarst lakes in Alaska

This photograph shows the Arctic Coastal Plain of northern 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 the Arctic Coastal Plain of northern 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: Caribou Tracks Along Alaska's Coast
Caribou Tracks Along Alaska's Coast
Caribou Tracks Along Alaska's Coast
Caribou Tracks Along Alaska's Coast

This photograph shows caribou tracks on ice-wedge polygons near Garry Creek in 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 caribou tracks on ice-wedge polygons near Garry Creek in 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: Polar Bear Along Alaska's Coast
Polar Bear Along Alaska's Coast
Polar Bear Along Alaska's Coast
Polar Bear Along Alaska's Coast

A polar bear stands on a low-lying barrier shoal near the Huluhula River on the Beaufort 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.

A polar bear stands on a low-lying barrier shoal near the Huluhula River on the Beaufort 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.

Photo from the sky looking back at a narrow, sandy island spit in a shallow part of the ocean.
Barrier islands near the western terminus of Icy Reef
Barrier islands near the western terminus of Icy Reef
Barrier islands near the western terminus of Icy Reef

Photograph of barrier islands near the western terminus of Icy Reef located on the Beaufort Sea coast of Alaska, looking south. Egaksrak Lagoon separates the islands from the low-lying mainland coast of the Arctic National Wildlife Refuge and the Brooks Range in the background.

Photograph of barrier islands near the western terminus of Icy Reef located on the Beaufort Sea coast of Alaska, looking south. Egaksrak Lagoon separates the islands from the low-lying mainland coast of the Arctic National Wildlife Refuge and the Brooks Range in the background.

Shoreline is crumbling into the water, and the land itself is interlocking polygons with brackish water in the centers.
Cape Halkett, Beaufort Sea, Alaska
Cape Halkett, Beaufort Sea, Alaska
Cape Halkett, Beaufort Sea, Alaska

This photograph shows ice-wedge polygons and an eroding shoreline at Cape Halkett on the Beaufort 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 ice-wedge polygons and an eroding shoreline at Cape Halkett on the Beaufort 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.

Satellite view of a oval-shaped island with deep water inside and outside the oval,
Coral atoll Tureia
Coral atoll Tureia
Coral atoll Tureia

Coral atolls are normally long, thin bars of white sand that rise just a few meters above sea level. The island or island group surrounds a hollow center where a volcanic peak once was. The atoll shown in this photo-like satellite image is the island of Tureia, in French Polynesia, in the South Pacific Ocean.

Coral atolls are normally long, thin bars of white sand that rise just a few meters above sea level. The island or island group surrounds a hollow center where a volcanic peak once was. The atoll shown in this photo-like satellite image is the island of Tureia, in French Polynesia, in the South Pacific Ocean.

Satellite view of island showing features like green mountains, brownish red soils, and bright, shallow, ocean waters.
Maui
Maui
Maui

Landsat image of Maui, Hawaiʻi, with the small island of Kahoʻolawe to its south.

Landsat image of Maui, Hawaiʻi, with the small island of Kahoʻolawe to its south.

Andrew Schwartz and Dan Hanes hold a current profiler for a study of surf-zone hydrodynamics at Ocean Beach, San Francisco.
Studying Surf-Zone Hydrodynamics
Studying Surf-Zone Hydrodynamics
Studying Surf-Zone Hydrodynamics

USGS scientists Andrew Schwartz and Dan Hanes maneuver a current profiler for a study of surf-zone hydrodynamics at Ocean Beach, on the west side of San Francisco, California. Beach erosion has been a continuing problem in this area.

USGS scientists Andrew Schwartz and Dan Hanes maneuver a current profiler for a study of surf-zone hydrodynamics at Ocean Beach, on the west side of San Francisco, California. Beach erosion has been a continuing problem in this area.

Illustration of a bay in the ocean with the water drained away, showing underwater features of a landslide in the bay.
Resurrection Bay, Alaska
Resurrection Bay, Alaska
Resurrection Bay, Alaska

Sonar-generated image showing underwater topography and the potential for landslides near the head of Resurrection Bay, Alaska. The terrain looks three times as steep as it occurs naturally. The arrow points to underwater landslide debris from the collapse of a fan-delta following the great Alaskan earthquake of 1964.

Sonar-generated image showing underwater topography and the potential for landslides near the head of Resurrection Bay, Alaska. The terrain looks three times as steep as it occurs naturally. The arrow points to underwater landslide debris from the collapse of a fan-delta following the great Alaskan earthquake of 1964.

Poster laid out with photos, images, and text.
Should Englebright Dam Be Removed?
Should Englebright Dam Be Removed?
Should Englebright Dam Be Removed?

Large-scale poster describing USGS work.

The USGS, in cooperation with the Upper Yuba River Studies Program and the California Bay–Delta Authority (CALFED), studied Englebright Lake. Englebright Dam was built in 1941 to trap sediment washed downstream by hydraulic gold mining.

Large-scale poster describing USGS work.

The USGS, in cooperation with the Upper Yuba River Studies Program and the California Bay–Delta Authority (CALFED), studied Englebright Lake. Englebright Dam was built in 1941 to trap sediment washed downstream by hydraulic gold mining.

Poster composed of photographs and text.
Flying Eyeball Measures Grand Canyon Sand
Flying Eyeball Measures Grand Canyon Sand
Flying Eyeball Measures Grand Canyon Sand

Large-scale poster describing USGS work.

USGS scientists needed a better way to measure river sand in the Grand Canyon. Traditionally, scientists used a bucket to get about 75 sand samples on each trip, which were analyzed weeks later in a lab.

Large-scale poster describing USGS work.

USGS scientists needed a better way to measure river sand in the Grand Canyon. Traditionally, scientists used a bucket to get about 75 sand samples on each trip, which were analyzed weeks later in a lab.

Dauphin Island, Alabama, map views
Dauphin Island, Alabama, map views
Dauphin Island, Alabama, map views
Dauphin Island, Alabama, map views

Dauphin Island, Alabama. Map views of post-storm difference grids for Hurricanes Ivan (A) and Katrina (B), and vertical photography of the same location (C). The lidar images show elevation gains (green) and losses (red).

Dauphin Island, Alabama. Map views of post-storm difference grids for Hurricanes Ivan (A) and Katrina (B), and vertical photography of the same location (C). The lidar images show elevation gains (green) and losses (red).

Dauphin Island, Alabama
Dauphin Island, Alabama
Dauphin Island, Alabama
Dauphin Island, Alabama

Dauphin Island, Alabama. Three-dimensional views of island topography (A-C), post-Katrina oblique aerial photograph (D), and differences in topography from Hurricanes Ivan (E) and Katrina (F). The view is along the island, looking from east to west, with the Gulf of Mexico to the left and Mississippi Sound to the right.

Dauphin Island, Alabama. Three-dimensional views of island topography (A-C), post-Katrina oblique aerial photograph (D), and differences in topography from Hurricanes Ivan (E) and Katrina (F). The view is along the island, looking from east to west, with the Gulf of Mexico to the left and Mississippi Sound to the right.

Photo sets of Waveland, Mississippi, pre- and post-Katrina
Photo sets of Waveland, Mississippi, pre- and post-Katrina
Photo sets of Waveland, Mississippi, pre- and post-Katrina
Photo sets of Waveland, Mississippi, pre- and post-Katrina

The top image was taken off the coast of Bay St. Louis, Mississippi, in July 1998 by researchers at the University of New Orleans. In this image, notice the large multi-story houses, some of which are built on stilts to protect the homes from flooding. The bottom image shows the same location on August 31, 2005, two days after landfall of Hurricane Katrina.

The top image was taken off the coast of Bay St. Louis, Mississippi, in July 1998 by researchers at the University of New Orleans. In this image, notice the large multi-story houses, some of which are built on stilts to protect the homes from flooding. The bottom image shows the same location on August 31, 2005, two days after landfall of Hurricane Katrina.

Computer model shows undersea features as well as land in 3-D and wave patterns in the ocean near an island
Tsunami wave field in Bay of Bengal
Tsunami wave field in Bay of Bengal
Tsunami wave field in Bay of Bengal

Tsunami wave field in the Bay of Bengal one hour after the M=9.1 Sumatra-Andaman earthquake on December 26, 2004. View looks to the northwest.

Tsunami wave field in the Bay of Bengal one hour after the M=9.1 Sumatra-Andaman earthquake on December 26, 2004. View looks to the northwest.

3-D angular view of a bay inlet with a bridge spanning the inlet, the floor of the bay is shown as if the water is drained out.
Sand waves at mouth of San Francisco Bay
Sand waves at mouth of San Francisco Bay
Sand waves at mouth of San Francisco Bay

A field of giant sand waves, among the largest in the world, at the mouth of San Francisco Bay in California.

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