Images

Engineering technician Tim Elfers of the USGS Pacific Coastal and Marine Science Center navigates a personal watercraft (PWC) through waves offshore of central California. The PWC is equipped with sonar and GPS in order to map the nearshore seafloor.

Personal watercraft were utilized to collect bathymetry in the surf zone and shore face (top left), setup on the beach (top right), instrument configuration (bottom left) and Pelican case hardware configuration (bottom right).

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.

USGS scientist Lisa Robbins next to the research vessel (R/V) Atlantis, which is owned by the U.S. Navy and operated by the Woods Hole Oceanographic Institution.

Picture shows United States Geological Survey scientist Beth Middleton and a lake in China. 

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.

Map showing the tracklines and grab sample sites of the 2014 and 2015 geophysical surveys offshore of the Delmarva Peninsula.

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).

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; 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.

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.

Map of daily-averaged ocean surface current data integrated from multiple IOOS Partner forecast models

A vibracore taken from a marshy area in Anahola Valley, Kaua‛i reveals a sandier mud layer.

The challenging and complex study environment of Molokaʻi’s (Hawaiʻi) fringing reef. Learn more about USGS studies on this island: “Coral Reef Project: Molokaʻi”

Geology and geomorphology offshore of Fort Ross, California, showing location of the San Andreas Fault and slope failures in the fault zone.

Left: USGS research hydrologist Mark Reid (left) and USGS research geologist Kevin Schmidt collect GPS data along the Big Sur coast on September 19, 2007. Photo credit: Maiana Hanshaw, USGS (now with swisstopo).

Pamela Swarzenski from the USGS Pacific Coastal and Marine Science Center sampling gas released by gas hydrate breakdown during a quantitative degassing aboard the drilling vessel Chikyu during the Indian Government’s National Gas Hydrates Program (NGHP-02) drilling expedition offshore from eastern India.

Junbong Jang of the USGS Woods Hole Coastal and Marine Science Center measures index properties on sediment collected during the Indian Government’s National Gas Hydrates Program (NGHP-02) drilling expedition offshore from eastern India in the summer of 2015.

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.

USGS research geologist Cheryl Hapke (center) explains to National Park Service manager Mike Bilecki (right) how instruments mounted on personal watercraft will measure depths in shallow water. USGS engineering technician BJ Reynolds is beside the watercraft.