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Images related to natural hazards.

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Image showing example of seafloor images and deployment of the SEABOSS sampler.
SEABOSS Collage
SEABOSS Collage
SEABOSS Collage

SEABed Observation and Sampling System (SEABOSS) (center image) and the MiniSEABOSS (right) designed for rapid, inexpensive, and effective collection of seabed imagery (photographs and video) as well sediment samples from the coastal/inner-continental shelf regions.

SEABed Observation and Sampling System (SEABOSS) (center image) and the MiniSEABOSS (right) designed for rapid, inexpensive, and effective collection of seabed imagery (photographs and video) as well sediment samples from the coastal/inner-continental shelf regions.

 Three-dimensional model of Chimney Bluffs, New York along Lake Ontario
Three-dimensional model of Chimney Bluffs, New York along Lake Ontari
Three-dimensional model of Chimney Bluffs, New York along Lake Ontari
Three-dimensional model of Chimney Bluffs, New York along Lake Ontari

Three-dimensional model of Chimney Bluffs, New York along Lake Ontario created from low-altitude digital images collected from an unmanned aerial system (UAS).

city skyline at night with tall buildings and bridge in left foreground lit up
The Bay Bridge and the Oakland city skyline
The Bay Bridge and the Oakland city skyline
The Bay Bridge and the Oakland city skyline

The nighttime Oakland city skyline as seen from San Francisco with the Bay Bridge in the foreground

Map of distribution sediment textures from Nantucket and Marthas Vineyard, Massachusetts
Sediment textures distribution from Nantucket and Marthas Vineyard, MA
Sediment textures distribution from Nantucket and Marthas Vineyard, MA
Sediment textures distribution from Nantucket and Marthas Vineyard, MA

The distribution of sediment textures within the study area. The bottom-type classification is from Barnhardt and others (1998) and is based on 16 sediment classes. The classification is based on four sediment units that include gravel (G), mud (M), rock (R), and sand (S). If the texture is greater than 90 percent, it is labeled with a single letter.

The distribution of sediment textures within the study area. The bottom-type classification is from Barnhardt and others (1998) and is based on 16 sediment classes. The classification is based on four sediment units that include gravel (G), mud (M), rock (R), and sand (S). If the texture is greater than 90 percent, it is labeled with a single letter.

Geologic sections illustrating general distributions and thickness of seismic stratigraphic units Marthas Vineyard, Nantucket
Nantucket and Marthas Vineyard geologic illustrations
Nantucket and Marthas Vineyard geologic illustrations
Nantucket and Marthas Vineyard geologic illustrations

Geologic sections (C-C', D-D', and E-E') illustrating the general distributions and thicknesses of seismic stratigraphic units and major unconformities in the Martha’s Vineyard and Nantucket study areas.

Geologic sections (C-C', D-D', and E-E') illustrating the general distributions and thicknesses of seismic stratigraphic units and major unconformities in the Martha’s Vineyard and Nantucket study areas.

 Department of Interior UAS pilots
UAS pilots at Kilauea
UAS pilots at Kilauea
UAS pilots at Kilauea

Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb

Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb

house next to landslide with snowcovered ground
Landslide near Potter Hill, Anchorage, Alaska
Landslide near Potter Hill, Anchorage, Alaska
Landslide near Potter Hill, Anchorage, Alaska

Landslide near Potter Hill, Anchorage, Alaska, after 2018 Anchorage earthquake.

Map showing the locations of all U.S. volcanoes
Map of volcano threat category designated by color
Map of volcano threat category designated by color
Map of volcano threat category designated by color

Map showing the locations of all U.S. volcanoes with their threat category designated by color. Very high threat is red, high is orange, moderate is yellow, low is green, and very low is blue. 

Map showing the locations of all U.S. volcanoes with their threat category designated by color. Very high threat is red, high is orange, moderate is yellow, low is green, and very low is blue. 

Brown landscape with volcano in the background
Mount Shasta, a steep-sided Cascade Range stratovolcano in Northern Ca
Mount Shasta, a steep-sided Cascade Range stratovolcano in Northern Ca
Mount Shasta, a steep-sided Cascade Range stratovolcano in Northern Ca

Mount Shasta, a steep-sided Cascade Range stratovolcano in Northern California, looms above Little Glass Mountain, a thick obsidian flow erupted from the Medicine Lake shield volcano about 1,000 years ago. These are just two of the young volcanic areas monitored by the USGS California Volcano Observatory. USGS photo.

Mount Shasta, a steep-sided Cascade Range stratovolcano in Northern California, looms above Little Glass Mountain, a thick obsidian flow erupted from the Medicine Lake shield volcano about 1,000 years ago. These are just two of the young volcanic areas monitored by the USGS California Volcano Observatory. USGS photo.

USGS personnel recovering ocean bottom seismometers
Ocean Bottom Seismometer Recovery
Ocean Bottom Seismometer Recovery
Ocean Bottom Seismometer Recovery

A WHCMSC and WHOI team recovered six intermediate period ocean bottom seismographs from the continental slope offshore New England in Georges Bank. The instruments had been deployed for about ten months to record background, ambient seismic noise.

A WHCMSC and WHOI team recovered six intermediate period ocean bottom seismographs from the continental slope offshore New England in Georges Bank. The instruments had been deployed for about ten months to record background, ambient seismic noise.

HayWired scenario landslide probabillity map
HayWired scenario landslide probabillity map
HayWired scenario landslide probabillity map

Map showing probablity of landslides based on the HayWired scenario.

Shake map for HayWired scenario
Shake map for HayWired scenario
Shake map for HayWired scenario

Map showing ground shaking that would result from the HayWired earthquake scenario.

Map showing ground shaking that would result from the HayWired earthquake scenario.

HayWired scenario earthquake map
HayWired scenario earthquake map
Perspective view of coastal bathymetry looking onshore, St. Thomas, US Virgin Islands
Perspective lidar view of coastal bathymetry at St. Thomas, USVI
Perspective lidar view of coastal bathymetry at St. Thomas, USVI
Perspective lidar view of coastal bathymetry at St. Thomas, USVI

Perspective view of coastal bathymetry looking onshore, St. Thomas, US Virgin Islands, mapped using lidar and depicted with false-color, showing detailed submerged features, including coral reefs.

image related to volcanoes. See description
A view into the center of Pu‘u ‘Ō‘ō. Collapses on th
A view into the center of Pu‘u ‘Ō‘ō. Collapses on th
A view into the center of Pu‘u ‘Ō‘ō. Collapses on th

A view into the center of Pu‘u ‘Ō‘ō. Collapses on the crater walls have enlarged sections of the crater and filled the bottom of the crater with rockfall debris. The deepest portion of the crater is about 286 m (938 ft) below the crater floor that existed prior to the collapse on April 30, 2018. Steam rises from the loose rock on the crater floor. USGS image by F.

A view into the center of Pu‘u ‘Ō‘ō. Collapses on the crater walls have enlarged sections of the crater and filled the bottom of the crater with rockfall debris. The deepest portion of the crater is about 286 m (938 ft) below the crater floor that existed prior to the collapse on April 30, 2018. Steam rises from the loose rock on the crater floor. USGS image by F.

image related to volcanoes. See description
Equipment check at Pu‘u ‘Ō‘ō
Equipment check at Pu‘u ‘Ō‘ō
Equipment check at Pu‘u ‘Ō‘ō

On May 7, 2019, field crews visited a telemetry hub on the rim of Pu‘u ‘Ō‘ō to assess damage after a small collapse on May 1. During the overflight, photos and observations were made of the Pu‘u ‘Ō‘ō crater. The crater walls expose a clear sequence of lava flows and cinder that built the cone in the early 1980s. USGS image by F. Younger.

On May 7, 2019, field crews visited a telemetry hub on the rim of Pu‘u ‘Ō‘ō to assess damage after a small collapse on May 1. During the overflight, photos and observations were made of the Pu‘u ‘Ō‘ō crater. The crater walls expose a clear sequence of lava flows and cinder that built the cone in the early 1980s. USGS image by F. Younger.

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