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Illustration showing islands and the channels in the ocean in between them with path lines of instruments with little flags.
Ocean current-following surface drifters
Ocean current-following surface drifters
Ocean current-following surface drifters

Map showing the paths that ocean current-following surface drifters deployed in coral larval slicks off west Maui traveled in 24 hours following their release during a coral spawning event. Such data suggests that the coral reefs off west-central Maui may provide coral larvae to the reefs off northeastern Lānaʻi.

Map showing the paths that ocean current-following surface drifters deployed in coral larval slicks off west Maui traveled in 24 hours following their release during a coral spawning event. Such data suggests that the coral reefs off west-central Maui may provide coral larvae to the reefs off northeastern Lānaʻi.

Underwater photograph near a coral reef with small orbs of coral larvae in the water column.
Coral Larvae
Coral Larvae
Coral Larvae

Underwater photograph of larvae being released into the water column from reef-building coral spawning off Maui the night of June 30, 2003. The white larvae are about 0.5 to 1.5 mm across.

Underwater photograph of larvae being released into the water column from reef-building coral spawning off Maui the night of June 30, 2003. The white larvae are about 0.5 to 1.5 mm across.

A series of 4 cartoon to illustrate how we go from an active volcanic island, to fringing and barrier reef, to atoll.
Atoll development
Atoll development
Atoll development

Coral atolls develop from reefs fringing volcanic islands. As first hypothesized by Charles Darwin, and confirmed by ocean drilling done by British scientists a century ago, reefs fringing volcanic islands build vertically to sea level, forming steep-walled barrier reefs.

Coral atolls develop from reefs fringing volcanic islands. As first hypothesized by Charles Darwin, and confirmed by ocean drilling done by British scientists a century ago, reefs fringing volcanic islands build vertically to sea level, forming steep-walled barrier reefs.

Photo shows hands holding ice that is covered in mud.
Gas hydrate
Gas hydrate
Gas hydrate

Gas hydrate recovered in shallow layers just below the seafloor during piston coring in the Mississippi Canyon in the northern Gulf of Mexico in 2002.

Gas hydrate recovered in shallow layers just below the seafloor during piston coring in the Mississippi Canyon in the northern Gulf of Mexico in 2002.

Illustration looking at the land from out over the ocean, as if the water were drained away, to show seafloor features.
Los Angeles Margin and Basin
Los Angeles Margin and Basin
Los Angeles Margin and Basin

Overall perspective view of the Los Angeles Margin and Basin looking northeast. The distance across the bottom of the image is about 100 kilometers with a vertical exaggeration of 6 times. The margin is bisected by a series of large underwater canyons, channels, and gullies.

Overall perspective view of the Los Angeles Margin and Basin looking northeast. The distance across the bottom of the image is about 100 kilometers with a vertical exaggeration of 6 times. The margin is bisected by a series of large underwater canyons, channels, and gullies.

View from the sky looking at a very high coastal cliff with gentle waves.
Coastal cliffs near Fort Funston in 2002
Coastal cliffs near Fort Funston in 2002
Coastal cliffs near Fort Funston in 2002

Photograph of a coastal cliff where a large landslide occurred between 2002 and 2010. This photo, taken in 2002, shows the cliff before the landslide.

Photograph of a coastal cliff where a large landslide occurred between 2002 and 2010. This photo, taken in 2002, shows the cliff before the landslide.

This poster shows an illustration of a lake bed looking from a side-angle, with text that talks about how the map was made.
Mapping Crater Lake, Oregon
Mapping Crater Lake, Oregon
Mapping Crater Lake, Oregon

Large-scale poster describing USGS work.

The USGS mapped Crater Lake, Oregon using sonar, in cooperation with the National Park Service, the University of New Hampshire, and C&C Technologies.

Large-scale poster describing USGS work.

The USGS mapped Crater Lake, Oregon using sonar, in cooperation with the National Park Service, the University of New Hampshire, and C&C Technologies.

Colorful image showing the geomorphology of the Puerto Rico Trench and surrounding terrain
Morphology and color-shaded bathymetry of the Puerto Rico Trench
Morphology and color-shaded bathymetry of the Puerto Rico Trench
Morphology and color-shaded bathymetry of the Puerto Rico Trench

Morphology and color-shaded bathymetry of the northeastern Caribbean region. Digital data courtesy of Troy Holcombe and Lisa Taylor, National Geophysical Data Center, Boulder, Colorado.

Morphology and color-shaded bathymetry of the northeastern Caribbean region. Digital data courtesy of Troy Holcombe and Lisa Taylor, National Geophysical Data Center, Boulder, Colorado.

Flat ocean floor made up of nodules packed in tightly.
Bed of manganese nodules
Bed of manganese nodules
Bed of manganese nodules

A bed of manganese nodules from deep offshore of the Cook Islands. Each color bar in the staff represents 10 centimeters.

A bed of manganese nodules from deep offshore of the Cook Islands. Each color bar in the staff represents 10 centimeters.

Flat underwater surface with many rocks tucked in close to each other; bright stripes of tape on rod that is touching bottom.
Cook Islands manganese nodules
Cook Islands manganese nodules
Cook Islands manganese nodules

A bed of manganese nodules from deep offshore of the Cook Islands; photo sourced from Hein et al., 2015, taken during a Japanese research cruise in the year 2000. Nodules range from about 2 to 10 centimeters across.

A bed of manganese nodules from deep offshore of the Cook Islands; photo sourced from Hein et al., 2015, taken during a Japanese research cruise in the year 2000. Nodules range from about 2 to 10 centimeters across.

Aerial view of an island with clouds floating above it, with distinctive land features like mountains and agriculture.
Landsat satellite image of Kauaʻi
Landsat satellite image of Kauaʻi
Landsat satellite image of Kauaʻi

This image was acquired on December 26, 2000, by the Enhanced Thematic Mapper plus instrument aboard NASA’s Landsat 7 satellite.

This image was acquired on December 26, 2000, by the Enhanced Thematic Mapper plus instrument aboard NASA’s Landsat 7 satellite.

Cartoon depicting an earthquake along a subduction zone with big starburst symbol, shows how ocean water is displaced upward.
Earthquake starts tsunami
Earthquake starts tsunami
Earthquake starts tsunami

An earthquake along a subduction zone happens when the leading edge of the overriding plate breaks free and springs seaward, raising the sea floor and the water above it. This uplift starts a tsunami. Meanwhile, the bulge behind the leading edge collapses, thinning the plate and lowering coastal areas.

An earthquake along a subduction zone happens when the leading edge of the overriding plate breaks free and springs seaward, raising the sea floor and the water above it. This uplift starts a tsunami. Meanwhile, the bulge behind the leading edge collapses, thinning the plate and lowering coastal areas.

Poster with illustrations of the underwater part of a bay, with text about the work done in the area.
Mapping Shipping Hazards in San Francisco Bay, 1997-1998
Mapping Shipping Hazards in San Francisco Bay, 1997-1998
Mapping Shipping Hazards in San Francisco Bay, 1997-1998

Large-scale poster describing USGS work.

The USGS mapped western San Francisco Bay using sonar, in cooperation with the National Oceanic and Atmospheric Administration (NOAA) and C&C Technologies. Some parts of the Bay floor are so shallow that a large tanker or container ship could run aground at low tide and create a massive oil spill.

Large-scale poster describing USGS work.

The USGS mapped western San Francisco Bay using sonar, in cooperation with the National Oceanic and Atmospheric Administration (NOAA) and C&C Technologies. Some parts of the Bay floor are so shallow that a large tanker or container ship could run aground at low tide and create a massive oil spill.

Aerial view of Assateague Island
Aerial view of Assateague Island
Aerial view of Assateague Island
Aerial view of Assateague Island

Aerial view of Assateague Island, looking north. Ocean City, Maryland, is visible in the far distance at top. Sinepuxent Bay lies between the island’s western shore and the Delmarva Peninsula to the upper left. Photograph taken in 1998 

Aerial view of Assateague Island, looking north. Ocean City, Maryland, is visible in the far distance at top. Sinepuxent Bay lies between the island’s western shore and the Delmarva Peninsula to the upper left. Photograph taken in 1998 

A large inflatable raft with two pontoons carries three people and equipment along a waterway with steep rocky edge.
Sonar in the Grand Canyon, 1992
Sonar in the Grand Canyon, 1992
Sonar in the Grand Canyon, 1992

George Tate (right, in light baseball cap) drives a raft on the Colorado River in Grand Canyon, 1992. The crane near the bow was used to deploy a small tripod holding a rotating sidescan sonar, which sat on the riverbed recording the motion of underwater sand dunes.

George Tate (right, in light baseball cap) drives a raft on the Colorado River in Grand Canyon, 1992. The crane near the bow was used to deploy a small tripod holding a rotating sidescan sonar, which sat on the riverbed recording the motion of underwater sand dunes.

An older, faded image of a brick building with blue-trimmed windows
Studebaker Building circa 1989
Studebaker Building circa 1989
Studebaker Building circa 1989

This historic brick Studebaker Building, originally built in 1925, was chosen as the location for the USGS St. Petersburg Coastal and Marine Science Center in the late 1980s.

This historic brick Studebaker Building, originally built in 1925, was chosen as the location for the USGS St. Petersburg Coastal and Marine Science Center in the late 1980s.

Photo shows the major collapse of a building following an earthquake, the building has fallen onto and crushed a car completely.
Loma Prieta earthquake, Marina District
Loma Prieta earthquake, Marina District
Loma Prieta earthquake, Marina District

An automobile lies crushed under the third story of this apartment building in the Marina District. The ground levels are no longer visible because of structural failure and sinking due to liquefaction.

An automobile lies crushed under the third story of this apartment building in the Marina District. The ground levels are no longer visible because of structural failure and sinking due to liquefaction.

Poster laid out with photos, images, and text.
Giant Hawaiian Underwater Landslides
Giant Hawaiian Underwater Landslides
Giant Hawaiian Underwater Landslides

Large-scale poster describing USGS work.

The USGS, in cooperation with the UK Institute of Oceanographic Sciences (IOS) and others, took images of the seafloor 200 miles around the Hawaiian Islands using GLORIA. GLORIA is a long-range sonar that gives a bird’s-eye view of the seafloor.

Large-scale poster describing USGS work.

The USGS, in cooperation with the UK Institute of Oceanographic Sciences (IOS) and others, took images of the seafloor 200 miles around the Hawaiian Islands using GLORIA. GLORIA is a long-range sonar that gives a bird’s-eye view of the seafloor.

A man and woman stand together having a discussion in 1979.
USGS Deputy Director Joe Cragwall with Susan Russell-Robinson
USGS Deputy Director Joe Cragwall with Susan Russell-Robinson
USGS Deputy Director Joe Cragwall with Susan Russell-Robinson

Susan Russell-Robinson with USGS Deputy Director Joe Cragwall at a National Archives exhibit marking the 100th anniversary of the USGS in 1979.

Susan Russell-Robinson with USGS Deputy Director Joe Cragwall at a National Archives exhibit marking the 100th anniversary of the USGS in 1979.

A grinning man looks up from an inflatable boat with a motor, he is wearing sunglasses and a lifejacket, holding a big hook.
Readying the grappling hook
Readying the grappling hook
Readying the grappling hook

George Tate playfully brandishes a grappling hook in a boat in Cook Inlet, Alaska, 1978. The driver (not shown) and George are about to motor away from the research vessel Sea Sounder to drag for the large tripod dubbed the Geoprobe. The apparatus had not deployed its recovery float and line, so the scientists had to try to hook it up off the seafloor.

George Tate playfully brandishes a grappling hook in a boat in Cook Inlet, Alaska, 1978. The driver (not shown) and George are about to motor away from the research vessel Sea Sounder to drag for the large tripod dubbed the Geoprobe. The apparatus had not deployed its recovery float and line, so the scientists had to try to hook it up off the seafloor.

Image cropped from USGS Hydrologic Atlas 457 showing flooded areas in blue on a contoured elevation map base
Floods in the Aguadilla-Aguada area, northwestern Puerto Rico
Floods in the Aguadilla-Aguada area, northwestern Puerto Rico
Floods in the Aguadilla-Aguada area, northwestern Puerto Rico

Map shows floods in the Aguadilla-Aguada area, northwestern Puerto Rico. The image is from USGS Hydrologic Atlas 457, created in 1972.