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Coastal and Marine Hazards and Resources Program images.

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A scientist stands on a dune with scientific equipment with the ocean in the background.
Ground-Penetrating Radar acquisition at Fire Island, NY
Ground-Penetrating Radar acquisition at Fire Island, NY
Ground-Penetrating Radar acquisition at Fire Island, NY

Ground-Penetrating Radar instruments are towed across land. Data from this instrument show underlying sediment layers within the dune and barrier island, which may reveal patterns of growth and erosion.

Ground-Penetrating Radar instruments are towed across land. Data from this instrument show underlying sediment layers within the dune and barrier island, which may reveal patterns of growth and erosion.

A colony of the soft coral known as the "bent sea rod" stands bleached on a reef off of Islamorada, Florida.
Bent Sea Rod Bleaching
Bent Sea Rod Bleaching
Bent Sea Rod Bleaching

A colony of the soft coral known as the "bent sea rod" stands bleached on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

A colony of the soft coral known as the "bent sea rod" stands bleached on a reef off of Islamorada, Florida. Hard and soft corals are presently bleaching- losing their symbiotic algae – all over the coral reefs of the Florida Keys due to unusually warm ocean temperatures this summer.

Scientists on a beach use sediment coring equipment (a tall aluminum barrel and motor to vibrate the barrel into the ground)
Collecting a sediment vibracore on the beach in Fire Island, NY
Collecting a sediment vibracore on the beach in Fire Island, NY
Collecting a sediment vibracore on the beach in Fire Island, NY

We collect terrestrial (barrier island) and marine (nearshore and estuarine) sediment cores to ground-truth geophysical observations. These cores are used to understand the history of barrier island formation and erosion.

a sandy coastline with heavily eroded dunes with two houses on stilts nearby
Erosion at Fire Island, New York
Erosion at Fire Island, New York
Erosion at Fire Island, New York

The impacts of extreme storms can be striking. Here, winter nor’easters eroded sediments from an artificial dune at Fire Island, New York and moved them onto the beach and shoreface. Such erosion created a steep vertical face, or scarp. Erosion and overwash are expected to increase on Fire Island with rising sea levels. 

The impacts of extreme storms can be striking. Here, winter nor’easters eroded sediments from an artificial dune at Fire Island, New York and moved them onto the beach and shoreface. Such erosion created a steep vertical face, or scarp. Erosion and overwash are expected to increase on Fire Island with rising sea levels. 

Winter nor’easters eroded sediments from an artificial dune and moved them seaward to the beach and shoreface
Winter nor’easters eroded sediments from an artificial dune
Winter nor’easters eroded sediments from an artificial dune
Winter nor’easters eroded sediments from an artificial dune

Though often less intense than hurricanes, extratropical storms (e.g., nor’easters) occur more frequently and their impacts can be striking. Here, several years after Hurricane Sandy, winter nor’easters eroded sediments from an artificial dune at Fire Island, NY and moved them onto the beach and shoreface. Such erosion created a steep vertical face, or scarp.

Though often less intense than hurricanes, extratropical storms (e.g., nor’easters) occur more frequently and their impacts can be striking. Here, several years after Hurricane Sandy, winter nor’easters eroded sediments from an artificial dune at Fire Island, NY and moved them onto the beach and shoreface. Such erosion created a steep vertical face, or scarp.

 The mapping team in front of the old Coast Guard Station at Cape Cod National Seashore. Left to right: Michael Klinker, Connor
Mapping Cape Cod National Seashore using unmanned aerial systems
Mapping Cape Cod National Seashore using unmanned aerial systems
Mapping Cape Cod National Seashore using unmanned aerial systems

The USGS conducted UAS flights to map the Nauset Marsh and Coast Guard Beach areas of Cape Cod National Seashore on Tuesday, March 1, 2016. These are the first authorized UAS flights in the northeast region of the national park system, and were performed under a research permit according to FAA and DOI regulations. 

The USGS conducted UAS flights to map the Nauset Marsh and Coast Guard Beach areas of Cape Cod National Seashore on Tuesday, March 1, 2016. These are the first authorized UAS flights in the northeast region of the national park system, and were performed under a research permit according to FAA and DOI regulations. 

USGS scientist Jackson Currie navigates a personal water craft through waves, collecting bathymetric data in Monterey, CA
Collecting Bathymetric Data
Collecting Bathymetric Data
Collecting Bathymetric Data

Physical scientist Jackson Currie steers a personal water craft (PWC) equipped with GPS and echo sounder through the waves of the nearshore area of Zmudowski State Beach in Moss Landing, California.

Physical scientist Jackson Currie steers a personal water craft (PWC) equipped with GPS and echo sounder through the waves of the nearshore area of Zmudowski State Beach in Moss Landing, California.

Image: Large Breaking Wave on Beach
Large Breaking Wave on Beach
Large Breaking Wave on Beach
Large Breaking Wave on Beach

Photograph showing the impact of a large wave at the south shore of Laysan Island, with endangered Laysan teal in the foreground.

Location: Laysan Islands (Northwestern Hawaiian Islands).

Photograph showing the impact of a large wave at the south shore of Laysan Island, with endangered Laysan teal in the foreground.

Location: Laysan Islands (Northwestern Hawaiian Islands).

Image: Methane Seeps along Offshore New England
Methane Seeps along Offshore New England
Methane Seeps along Offshore New England
Methane Seeps along Offshore New England

Seafloor image at a deepwater (~1400 m water depth) seep site on the New England margin. Seafloor conditions here are well inside the pressure-temperature stability field for methane hydrate. Gas being emitted below the rock overhang has formed gas hydrate (the white ice-like material). Distinct bubbles are visible in the foreground. The red laser scale is 10 cm.

Seafloor image at a deepwater (~1400 m water depth) seep site on the New England margin. Seafloor conditions here are well inside the pressure-temperature stability field for methane hydrate. Gas being emitted below the rock overhang has formed gas hydrate (the white ice-like material). Distinct bubbles are visible in the foreground. The red laser scale is 10 cm.

Image: Deployment of Trawl Aboard R/V Kiyi
Deployment of Trawl Aboard R/V Kiyi
Deployment of Trawl Aboard R/V Kiyi
Deployment of Trawl Aboard R/V Kiyi

Two researchers deploying a fishing trawl into Lake Superior while aboard the USGS GLSC's R/V Kiyi

Photo shows white, bleached coral surrounded by brown coral, with fish swimming
Photograph of shallow-water coral bleaching at Sombrero de Pelo reef
Photograph of shallow-water coral bleaching at Sombrero de Pelo reef
Photograph of shallow-water coral bleaching at Sombrero de Pelo reef

Photograph of shallow-water coral bleaching at Sombrero de Pelo reef in Pacific Panama during the 2015-2016 El Nino event. Because of the influence of internal waves, corals growing at deeper locations at this site did not bleach.

Photograph of shallow-water coral bleaching at Sombrero de Pelo reef in Pacific Panama during the 2015-2016 El Nino event. Because of the influence of internal waves, corals growing at deeper locations at this site did not bleach.

Sea surface temperature map of the world during 2016's El Niño. Dark areas show where temperatures are higher than normal.
SST anomalies during El Niño 2016
SST anomalies during El Niño 2016
SST anomalies during El Niño 2016

Pacific Ocean temperature differences during this winter’s record-setting El Niño. Dark red areas are much warmer than average.

Pacific Ocean temperature differences during this winter’s record-setting El Niño. Dark red areas are much warmer than average.

Image shows relief and orthophotomosaic maps of Coast Guard Beach, Cape Cod National Seashore.
Preliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore
Preliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore
Preliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore

Preliminary map products derived from the UAS imagery collected near Coast Guard Beach, Cape Cod National Seashore on 1 March 2016. Left: shaded relief color contoured digital elevation map on a 0.1-meter grid. Right: orthophotomosaic (0.05-meter resolution) overlaid on the shaded relief map.

Map of the world shows sea surface temperature anomalies on March 1, 2016 due to El Niño.
SST temperature anomalies on March 1, 2016
SST temperature anomalies on March 1, 2016
SST temperature anomalies on March 1, 2016

Sea surface temperature differences on March 1, 2016. Dark red indicates much warmer water.

Kim Yates and Nate Smiley measure acidity, nutrient levels, and other characteristics of water sampled near the coral reef
Kim Yates and Nate Smiley of the USGS
Kim Yates and Nate Smiley of the USGS
Kim Yates and Nate Smiley of the USGS

Kim Yates (left) and Nate Smiley of the USGS St. Petersburg Coastal and Marine Science Center measure acidity, nutrient levels, and other characteristics of water sampled near the coral reef off Kahekili Beach Park, Maui, Hawai‘i, in March 2016.

Kim Yates (left) and Nate Smiley of the USGS St. Petersburg Coastal and Marine Science Center measure acidity, nutrient levels, and other characteristics of water sampled near the coral reef off Kahekili Beach Park, Maui, Hawai‘i, in March 2016.

Photograph taken from above the stern of the ship, with crew readying the streamer cable for a seismic survey.
Multichannel seismic streamer
Multichannel seismic streamer
Multichannel seismic streamer

A ship will tow this green cable, which contains underwater microphones that record sound reflected off layers beneath the seafloor. USGS scientists will use the data to pinpoint the location of faults.

A ship will tow this green cable, which contains underwater microphones that record sound reflected off layers beneath the seafloor. USGS scientists will use the data to pinpoint the location of faults.

A man stands looking at a set of maps on a table, while another man in the background in the dark sits at a laptop.
Using seafloor maps to plan further mapping
Using seafloor maps to plan further mapping
Using seafloor maps to plan further mapping

USGS geologist Jamie Conrad uses a map of the seafloor off Southern California to plan high-resolution mapping southwest of Santa Catalina Island. Small inset shows seafloor data collected by the ship that reveals hills, gullies, and basins.

USGS geologist Jamie Conrad uses a map of the seafloor off Southern California to plan high-resolution mapping southwest of Santa Catalina Island. Small inset shows seafloor data collected by the ship that reveals hills, gullies, and basins.

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