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Clams half buried in very fine, gray sediment.
Calyptogena spp. in Alaska
Calyptogena spp. in Alaska
Calyptogena spp. in Alaska

These clams (Calyptogena spp.) were discovered in about 1000 meter-deep waters off the southern tip of Alaska near a 250-meter-high cone rising from the seafloor and 10 kilometers from the Queen Charlotte-Fairweather fault.

These clams (Calyptogena spp.) were discovered in about 1000 meter-deep waters off the southern tip of Alaska near a 250-meter-high cone rising from the seafloor and 10 kilometers from the Queen Charlotte-Fairweather fault.

Computer-generated illustration of colored, high-resolution seafloor map clearly shows a fault and where the seafloor is offset.
Seafloor trace of the Queen Charlotte-Fairweather fault
Seafloor trace of the Queen Charlotte-Fairweather fault
Seafloor trace of the Queen Charlotte-Fairweather fault

Seafloor trace of the Queen Charlotte-Fairweather fault (from top left to bottom right) offsets the edge of the Yakobi Sea Valley off southeast Alaska. This 700-mile-long fault has generated large earthquakes in the past. Future shocks—and tsunamis—could threaten coastal communities in the U.S. and Canada. (Color-coded depths, in meters, were mapped in 2015.)

Seafloor trace of the Queen Charlotte-Fairweather fault (from top left to bottom right) offsets the edge of the Yakobi Sea Valley off southeast Alaska. This 700-mile-long fault has generated large earthquakes in the past. Future shocks—and tsunamis—could threaten coastal communities in the U.S. and Canada. (Color-coded depths, in meters, were mapped in 2015.)

Sandy Brosnahan transporting a weather buoy into the Woods Hole Coastal and Marine Science Center’s operational facility in prep
Special Delivery
Special Delivery
Special Delivery

Sandy Brosnahan transporting a weather buoy into the Woods Hole Coastal and Marine Science Center’s operational facility in preparation for deployment. This buoy was one of 6 deployed to measure wind speed, direction, pressure, and temperature off the coast of Fire Island, NY.

Sandy Brosnahan transporting a weather buoy into the Woods Hole Coastal and Marine Science Center’s operational facility in preparation for deployment. This buoy was one of 6 deployed to measure wind speed, direction, pressure, and temperature off the coast of Fire Island, NY.

Image: Tsunami Evacuation Sign
Tsunami Evacuation Sign
Tsunami Evacuation Sign
Tsunami Evacuation Sign

Tsunami evacuation route sign at an intersection in Nehalem, Oregon.

Scientist sets up solar-powered research station amid Fire Island dunes
Setting up a science base in a barrier island wilderness
Setting up a science base in a barrier island wilderness
Setting up a science base in a barrier island wilderness

USGS scientist BJ Reynolds sets up a solar-powered, satellite-uplinked GPS base station in the Fire Island Wilderness Area to support detailed elevation surveys.

Photo of a coastal cliff with an apartment building right at the edge of the cliff.
Cliff erosion
Cliff erosion
Cliff erosion

Cliff erosion is a common storm-induced hazard along the West Coast. Two condemned apartment buildings along Esplanade Avenue in Pacifica, California are shown here before their demolition in 2016 and 2017.

Cliff erosion is a common storm-induced hazard along the West Coast. Two condemned apartment buildings along Esplanade Avenue in Pacifica, California are shown here before their demolition in 2016 and 2017.

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Topsail, North Carolina. 
Aerial photographs of Topsail, North Carolina
Aerial photographs of Topsail, North Carolina
Aerial photographs of Topsail, North Carolina

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Topsail, North Carolina. View looking northwest along the North Carolina shore. Elevated storm-induced water levels overtopped the low dunes here causing the dune to overwash. Sand was transported landward, burying the marsh (green arrow).

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Topsail, North Carolina. View looking northwest along the North Carolina shore. Elevated storm-induced water levels overtopped the low dunes here causing the dune to overwash. Sand was transported landward, burying the marsh (green arrow).

marsh, rocky coast, barrier beach, coastal bluff
Sea-level rise effects vary in geomorphology and ecology
Sea-level rise effects vary in geomorphology and ecology
Sea-level rise effects vary in geomorphology and ecology

The effects of sea-level rise will vary by differences in the geomorphology and ecology of the landscape.  Images show marsh (top left) rocky coast (top right), barrier beach (bottom left), and coastal bluff (bottom right)

The effects of sea-level rise will vary by differences in the geomorphology and ecology of the landscape.  Images show marsh (top left) rocky coast (top right), barrier beach (bottom left), and coastal bluff (bottom right)

Map showing extent and coverage of coastal response type predictions
Coastal Response Predictions
Coastal Response Predictions
Coastal Response Predictions

Map showing extent and coverage of coastal response type predictions; insets display different prediction types and geospatial variability through time. Predictions of coastal response likelihood for the four prediction time steps at Blackwater National Wildlife Refuge, VA.

Map showing extent and coverage of coastal response type predictions; insets display different prediction types and geospatial variability through time. Predictions of coastal response likelihood for the four prediction time steps at Blackwater National Wildlife Refuge, VA.

Newberry Volcano's Youngest Lava Flows...
Newberry Volcano's Youngest Lava Flows
Newberry Volcano's Youngest Lava Flows
Newberry Volcano's Youngest Lava Flows

Newberry Volcano's youngest lava flows. Source: Robinson, J.E., Donnelly-Nolan, J.M., and Jensen, R.A., 2015, Newberry Volcano’s Youngest Lava Flows: U.S. Geological Survey Scientific Investigations Map 3329, 1 sheet, https://dx.doi.org/10.3133/sim3329.

Newberry Volcano's youngest lava flows. Source: Robinson, J.E., Donnelly-Nolan, J.M., and Jensen, R.A., 2015, Newberry Volcano’s Youngest Lava Flows: U.S. Geological Survey Scientific Investigations Map 3329, 1 sheet, https://dx.doi.org/10.3133/sim3329.

Map illustration showing bathymetry, or depth, and a fault offshore of the Alaskan coastline.
Queen Charlotte-Fairweather fault
Queen Charlotte-Fairweather fault
Queen Charlotte-Fairweather fault

Enlarged details of Survey Area 1 showing new multibeam bathymetry data (rainbow colors) acquired on R/V Solstice near Cross Sound and Glacier Bay National Park, southeastern Alaska. Arrows highlight the surface expression, or trace, of the Queen Charlotte-Fairweather fault.

Enlarged details of Survey Area 1 showing new multibeam bathymetry data (rainbow colors) acquired on R/V Solstice near Cross Sound and Glacier Bay National Park, southeastern Alaska. Arrows highlight the surface expression, or trace, of the Queen Charlotte-Fairweather fault.

Computer application screen showing seafloor features, depth on left, a volcano-like cone sticking up in middle with plume.
Sidescan sonar record off so. Alaska
Sidescan sonar record off so. Alaska
Sidescan sonar record off so. Alaska

Profile of newly discovered volcano-like cone in sonar record collected off southern Alaska. The cone’s summit is at about 1,000 meters water depth. Note fluid plume (blue) rising more than 700 meters upward from the summit.

Profile of newly discovered volcano-like cone in sonar record collected off southern Alaska. The cone’s summit is at about 1,000 meters water depth. Note fluid plume (blue) rising more than 700 meters upward from the summit.

USGS scientists operating a small research vessel in water near a grassy shoreline.
USGS vessel used to collect single-beam bathymetry
USGS vessel used to collect single-beam bathymetry
USGS vessel used to collect single-beam bathymetry

This USGS vessel acquires single-beam bathymetry in shallow nearshore environments. We acquire repeat bathymetry surveys over multiple years and compute changes in bathymetry, thus allowing us to identify hotspots of erosion and deposition on short timescales.

This USGS vessel acquires single-beam bathymetry in shallow nearshore environments. We acquire repeat bathymetry surveys over multiple years and compute changes in bathymetry, thus allowing us to identify hotspots of erosion and deposition on short timescales.

Image: USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation

USGS scientists Paul Rydlund, Eric Looper and Jason Carron dock the boat and coordinate with emergency managers.

The sun angle was ideal this morning to show the complex texture on...
The sun angle was ideal this morning to show the complex texture on...
The sun angle was ideal this morning to show the complex texture on...
The sun angle was ideal this morning to show the complex texture on...

The sun angle was ideal this morning to show the complex texture on the surface of the lava lake in Halema‘uma‘u Crater at Kīlauea's summit. Spattering was active in the southeast portion of the lake. For scale, the lake is about 230 meters or 755 feet across.

The sun angle was ideal this morning to show the complex texture on the surface of the lava lake in Halema‘uma‘u Crater at Kīlauea's summit. Spattering was active in the southeast portion of the lake. For scale, the lake is about 230 meters or 755 feet across.

Image: USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation

USGS scientists Chris Rowden, Larry Buschmann and Bob Holmes were on the Mississippi River at St. Louis taking streamflow measurements on New Years Eve. This information is critical to the National Weather Service, the U.S. Army Corps of Engineers and emergency managers in making flood predictions and response.

USGS scientists Chris Rowden, Larry Buschmann and Bob Holmes were on the Mississippi River at St. Louis taking streamflow measurements on New Years Eve. This information is critical to the National Weather Service, the U.S. Army Corps of Engineers and emergency managers in making flood predictions and response.

Image: USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation

USGS crews had two research vessels out measuring streamflow on the Mississippi River at St. Louis on New Years Eve. USGS scientists Eric Looper and Jason Carron are one of many USGS field crews out in the floodwaters over the holiday.

USGS crews had two research vessels out measuring streamflow on the Mississippi River at St. Louis on New Years Eve. USGS scientists Eric Looper and Jason Carron are one of many USGS field crews out in the floodwaters over the holiday.

Image: USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation

USGS crews had two research vessels out measuring streamflow on the Mississippi River at St. Louis on New Years Eve. USGS scientists Eric Looper and Jason Carron are one of many USGS field crews out in the floodwaters over the holiday.

USGS crews had two research vessels out measuring streamflow on the Mississippi River at St. Louis on New Years Eve. USGS scientists Eric Looper and Jason Carron are one of many USGS field crews out in the floodwaters over the holiday.

Image: USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation
USGS Measures Historic Flooding Across the Nation

USGS scientists Chris Rowden and Larry Buschmann dock the boat and coordinate with emergency managers.

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