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First map shows aerial view of beach area, next with 50-centimeter sea-level rise, last with added annual storm.
Flood Map, Stinson Beach
Flood Map, Stinson Beach
Flood Map, Stinson Beach

Flood maps from Our Coast, Our Future showing Stinson Beach today (slide 1); with a 50-centimeter sea-level rise (slide 2); and when an annual storm strikes in addition to 50-centimeter sea-level rise (slide 3). Green patches are low-lying areas prone to flooding.

Flood maps from Our Coast, Our Future showing Stinson Beach today (slide 1); with a 50-centimeter sea-level rise (slide 2); and when an annual storm strikes in addition to 50-centimeter sea-level rise (slide 3). Green patches are low-lying areas prone to flooding.

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

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Rodanthe, North Carolina. View looking west along the North Carolina shore. High waves and storm surge from Hurricane Joaquin eroded the beach, exposing the pilings of the homes to wave attack (green and orange arrows).

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Rodanthe, North Carolina. View looking west along the North Carolina shore. High waves and storm surge from Hurricane Joaquin eroded the beach, exposing the pilings of the homes to wave attack (green and orange arrows).

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

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Salvo, North Carolina. View looking west along the North Carolina shore. Waves and surge from Hurricane Joaquin eroded the beach, causing significant shoreline retreat and a narrower beach, leaving deposits of darker sand at the base of the dune (green arrow).

Near vertical (top, middle) and low angle oblique (bottom) aerial photographs of Salvo, North Carolina. View looking west along the North Carolina shore. Waves and surge from Hurricane Joaquin eroded the beach, causing significant shoreline retreat and a narrower beach, leaving deposits of darker sand at the base of the dune (green arrow).

. Problem statement, objectives, and alternative actions defined by DOI collaborators using structured decision making framework
Decision Making Framework
Decision Making Framework
Decision Making Framework

Problem statement, objectives, and alternative actions defined by Department of Interior  collaborators using structured decision making framework

Problem statement, objectives, and alternative actions defined by Department of Interior  collaborators using structured decision making framework

Yellowstone subsurface cross-section schematic oriented SW-NE, depi...
Yellowstone subsurface cross-section schematic oriented SW-NE, depi...
Yellowstone subsurface cross-section schematic oriented SW-NE, depi...
Yellowstone subsurface cross-section schematic oriented SW-NE, depi...

Yellowstone subsurface cross-section schematic oriented SW-NE, depicts rise of magma beneath mantle plus heating and movement of mantle and crustal material. Credit Univ Utah. Click to enlarge.

Kīlauea Volcano's East Rift Zone eruption turns 33!...
Kīlauea's ERZ eruption turns 33!
Kīlauea's ERZ eruption turns 33!
Kīlauea's ERZ eruption turns 33!

The November 25, 2015, breakout that began as a rupture from the tube supplying the June 27th lava flow advanced slowly to the northeast of Pu‘u ‘Ō‘ō (background) and reached the forest in mid-December, but still poses no immediate threat to Puna communities. USGS image.

The November 25, 2015, breakout that began as a rupture from the tube supplying the June 27th lava flow advanced slowly to the northeast of Pu‘u ‘Ō‘ō (background) and reached the forest in mid-December, but still poses no immediate threat to Puna communities. USGS image.

Illustration of the NIMBBLE (New instrument for making bottom boundary layer evaluations)
Illustration of the NIMBBLE (New instrument for making bottom boun
Illustration of the NIMBBLE (New instrument for making bottom boun
Illustration of the NIMBBLE (New instrument for making bottom boun

Illustration of the NIMBBLE (New instrument for making bottom boundary layer evaluations). The NIMBBLE is a low-profile platform with two acoustic Doppler velocimeters and an upward-looking acoustic Doppler profilers.

USGS staff and ship's crew prepare to deploy a deep-water multibeam sonar.
Deploying multibeam sonar
Deploying multibeam sonar
Deploying multibeam sonar

USGS staff and the ship's crew of the R/V Sharp prepare to deploy a deep-water multibeam echosounder during a mapping program in the mid-Atlantic in 2015.

USGS staff and the ship's crew of the R/V Sharp prepare to deploy a deep-water multibeam echosounder during a mapping program in the mid-Atlantic in 2015.

Science crew aboard R/V Marcus G. Langseth.
Science crew aboard R/V Marcus G. Langseth.
Science crew aboard R/V Marcus G. Langseth.
Science crew aboard R/V Marcus G. Langseth.

Science crew aboard R/V Marcus G. Langseth. Ray Sliter (Pacific Coastal and Marine Science Center) and Deb Hutchison (Woods Hole Coastal and Marine Science Center) shown at far left.

Photo showing complex geomorphology of the Grand Bay marsh landscape
Photo showing complex geomorphology of the Grand Bay marsh landscape
Photo showing complex geomorphology of the Grand Bay marsh landscape
Photo showing complex geomorphology of the Grand Bay marsh landscape

Photo showing the complex geomorphology of the marsh landscape of the Grand Bay National Wildlife Refuge/Grand Bay National Estuarine Research Reserve in coastal Alabama and Mississippi. (1) Geology—a tidal creek that at lower sea level than present served as a distributary channel of a river-delta system. (2) Hydrodynamics—wave erosion of the marsh edge.

Photo showing the complex geomorphology of the marsh landscape of the Grand Bay National Wildlife Refuge/Grand Bay National Estuarine Research Reserve in coastal Alabama and Mississippi. (1) Geology—a tidal creek that at lower sea level than present served as a distributary channel of a river-delta system. (2) Hydrodynamics—wave erosion of the marsh edge.

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.

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