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).
Images
Images related to natural hazards.
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).
Sea-level rise effects vary in geomorphology and ecology
Sea-level rise effects vary in geomorphology and ecologyThe 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)
Sea-level rise effects vary in geomorphology and ecology
Sea-level rise effects vary in geomorphology and ecologyThe 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; 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. 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.
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.
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.
Map of daily-averaged ocean surface current data integrated from multiple IOOS Partner forecast models
Map of daily-averaged ocean surface current data integrated from multiple IOOS Partner forecast models
USGS vessel used to collect single-beam bathymetry
USGS vessel used to collect single-beam bathymetryThis 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.
USGS vessel used to collect single-beam bathymetry
USGS vessel used to collect single-beam bathymetryThis 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.
Vector Shorelines and Associated Shoreline Change Data for the Southeast Atlantic Coast
Vector Shorelines and Associated Shoreline Change Data for the Southeast Atlantic Coast
Bathymetry and backscatter intensity of the sea floor of the Hudson Shelf Valley location map
Bathymetry and backscatter intensity of the sea floor of the Hudson Shelf Valley location map
Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Bear Inlet, North Carolina. View looking northwest along the North Carolina shore. High waves and storm surge from Hurricane Joaquin eroded the beaches, moving sand inland (green arrow) and reshaping the flood-tidal shoals.
Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Bear Inlet, North Carolina. View looking northwest along the North Carolina shore. High waves and storm surge from Hurricane Joaquin eroded the beaches, moving sand inland (green arrow) and reshaping the flood-tidal shoals.
Aerial images of the wilderness breach: a) Aerial photograph taken several days after Hurricane Sandy (photo credit: NOAA); b) Aerial mosaic of the breach in June 2015 showing the location of erosion on the ocean side of the breach and deposition that results in the seasonal formation of a spit (photo credit: Stonybrook University).
Aerial images of the wilderness breach: a) Aerial photograph taken several days after Hurricane Sandy (photo credit: NOAA); b) Aerial mosaic of the breach in June 2015 showing the location of erosion on the ocean side of the breach and deposition that results in the seasonal formation of a spit (photo credit: Stonybrook University).
North Atlantic Landscape Conservation Cooperative region
North Atlantic Landscape Conservation Cooperative regionCoastal area within the North Atlantic Landscape Conservation Cooperative region for which predictions have been generated.
North Atlantic Landscape Conservation Cooperative region
North Atlantic Landscape Conservation Cooperative regionCoastal area within the North Atlantic Landscape Conservation Cooperative region for which predictions have been generated.
Minipod style tripod for near bottom current and wave measurements
Minipod style tripod for near bottom current and wave measurementsMinipod style tripod for near bottom current and wave measurements ready for deployment.
Minipod style tripod for near bottom current and wave measurements
Minipod style tripod for near bottom current and wave measurementsMinipod style tripod for near bottom current and wave measurements ready for deployment.
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.
Seafloor trace of the Queen Charlotte-Fairweather fault
Seafloor trace of the Queen Charlotte-Fairweather faultSeafloor 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
Seafloor trace of the Queen Charlotte-Fairweather faultSeafloor 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 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.
Tsunami evacuation route sign at an intersection in Nehalem, Oregon.
Tsunami evacuation route sign at an intersection in Nehalem, Oregon.
USGS scientist and GeoGirls viewing Mount St. Helens
USGS scientist and GeoGirls viewing Mount St. HelensUSGS scientists Kate Allstadt and Cynthia Gardner tell the story of the May 18, 1980 eruption of Mount St. Helens and how the catastrophic landslide, lateral blast, and lahar changed the landscape.
USGS scientist and GeoGirls viewing Mount St. Helens
USGS scientist and GeoGirls viewing Mount St. HelensUSGS scientists Kate Allstadt and Cynthia Gardner tell the story of the May 18, 1980 eruption of Mount St. Helens and how the catastrophic landslide, lateral blast, and lahar changed the landscape.
Headscarp of Red Bluffs Landslide Overlooking Crescent Lake Landslide
Headscarp of Red Bluffs Landslide Overlooking Crescent Lake LandslideView out over the Crescent Lake landslide from the headscarp (left foreground) of the Red Bluffs landslide, looking toward Stevenson, Washington and the Columbia River.
Headscarp of Red Bluffs Landslide Overlooking Crescent Lake Landslide
Headscarp of Red Bluffs Landslide Overlooking Crescent Lake LandslideView out over the Crescent Lake landslide from the headscarp (left foreground) of the Red Bluffs landslide, looking toward Stevenson, Washington and the Columbia River.