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Coastal and Marine Hazards and Resources Program images.

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Aerial imagery of a peninsula are marked to show different data about each island's coast.
Florida Coral Reefs and Coastal Hazard Risk Reduction
Florida Coral Reefs and Coastal Hazard Risk Reduction
Aerial imagery of islands are marked to show different data about each island's coast.
Puerto Rico Coral Reefs and Coastal Hazard Risk Reduction
Puerto Rico Coral Reefs and Coastal Hazard Risk Reduction
Cliff feature outputs from the algorithm are shown as colored dots and lines on a 3-dimensional rendering of a coastal cliff.
Cliff Feature Delineation Tool Outputs in Malibu, California
Cliff Feature Delineation Tool Outputs in Malibu, California
Cliff Feature Delineation Tool Outputs in Malibu, California

Digital three-dimensional rendering of the coastal cliffs around Point Dume in Malibu, California. Cliff feature outputs from the Cliff Feature Delineation Tool are shown to conceptually display the cliff delineation process, including cross-shore transects (green), the cliff top line (red), the cliff toe line (blue), and subsidiary cliff features (orange).

Digital three-dimensional rendering of the coastal cliffs around Point Dume in Malibu, California. Cliff feature outputs from the Cliff Feature Delineation Tool are shown to conceptually display the cliff delineation process, including cross-shore transects (green), the cliff top line (red), the cliff toe line (blue), and subsidiary cliff features (orange).

A series of panels, looking down at a river delta, show how the delta changed, growing larger as more sediment flowed downriver.
Evolution of shoreline around Elwha River mouth
Evolution of shoreline around Elwha River mouth
Evolution of shoreline around Elwha River mouth

Evolution of the shoreline around the Elwha River mouth, Washington, before, during and after dam removal, 2011–2017. Two large dams were removed from the Elwha River between 2011 and 2014 in the largest dam removal worldwide thus far, releasing more than 20 million tons of sediment downstream.

Evolution of the shoreline around the Elwha River mouth, Washington, before, during and after dam removal, 2011–2017. Two large dams were removed from the Elwha River between 2011 and 2014 in the largest dam removal worldwide thus far, releasing more than 20 million tons of sediment downstream.

A coral reef in the Turks and Caicos Islands dominated by the weedy coral species, Porites astreoides
Modern coral reef dominated by weedy coral species
Modern coral reef dominated by weedy coral species
Modern coral reef dominated by weedy coral species

A coral reef in the Turks and Caicos Islands dominated by the weedy coral species, Porites astreoides. The relative dominance of this taxa has increased throughout the western Atlantic.

A coral reef in the Turks and Caicos Islands dominated by the weedy coral species, Porites astreoides. The relative dominance of this taxa has increased throughout the western Atlantic.

Two men work on a boat pulling up a long cable from the water.
Retrieving a core sampler
Retrieving a core sampler
Retrieving a core sampler

USGS scientists Dan Powers (left) and Andy Ritchie retrieving a core sample from beneath Lake Ozette aboard research vessel Hadai.

USGS scientists Dan Powers (left) and Andy Ritchie retrieving a core sample from beneath Lake Ozette aboard research vessel Hadai.

Diagram of a series of tubes connected to a well head, with an inset showing the structure inside the tubes
Above ground mesocosm with biofilm growth reactors
Above ground mesocosm with biofilm growth reactors
Above ground mesocosm with biofilm growth reactors

Above ground mesocosm with biofilm growth reactors. Groundwater from the well head is directly transferred to the mesocosm via PTFE tubing into a high flow rate control valve (a) that diverts groundwater into a flow cell containing a water quality measurement meter (b) and a low flow control valve (c).

Above ground mesocosm with biofilm growth reactors. Groundwater from the well head is directly transferred to the mesocosm via PTFE tubing into a high flow rate control valve (a) that diverts groundwater into a flow cell containing a water quality measurement meter (b) and a low flow control valve (c).

Four photos show scientists working in the field collecting data using various methods.
Field work in the Columbia River Littoral Cell
Field work in the Columbia River Littoral Cell
Field work in the Columbia River Littoral Cell

Photographs showing equipment used during bathymetric and topographic surveys along the Columbia River littoral cell, Washington and Oregon.

Photograph of Dr. Ben Gutierrez moderating a session at the 2019 diversity workshop
Ben Gutierrez moderating Partnership in Education Program (PEP) panel
Ben Gutierrez moderating Partnership in Education Program (PEP) panel
Ben Gutierrez moderating Partnership in Education Program (PEP) panel

Woods Hole Coastal and Marine Science Center geologist, Ben Gutierrez, moderates a panel at the 2019 Partnership Eucation Program (PEP) 10th Anniversity Conference and Celebration, Woods Hole, MA June 28-30, 2019.

Collage of images showing the area of study with underwater photographs of the seafloor and dots on the map to show photo locations.
squid-5StudyAreaMap.jpg
squid-5StudyAreaMap.jpg
squid-5StudyAreaMap.jpg

Image map of study area showing (a) study region, (b) study sites, (c, d) example orthomosaic images, and (e) photo of SET 1.

Illustration helps visualize the seafloor character offshore of the continental United States showing canyons and other features
Astoria Canyon multibeam bathymetry
Astoria Canyon multibeam bathymetry
Astoria Canyon multibeam bathymetry

Multibeam bathymetry shown in the spectrum from red (shallower) to blue (deeper) for depths greater than 200 m across the head of Astoria Canyon. The land and continental shelf are shown in grayscale slope shading where darker colors represent steeper slopes.  The modern Columbia River is far right.

Multibeam bathymetry shown in the spectrum from red (shallower) to blue (deeper) for depths greater than 200 m across the head of Astoria Canyon. The land and continental shelf are shown in grayscale slope shading where darker colors represent steeper slopes.  The modern Columbia River is far right.

Illustration helps visualize the seafloor character showing canyons and and the rivers that form them.
Southern Cascadia topography and bathymetry
Southern Cascadia topography and bathymetry
Southern Cascadia topography and bathymetry

Topography and bathymetry of southern Cascadia, which includes southern Oregon and northern California (seafloor depths between 200 and 3000 m are shown in the spectrum color scale from red (shallower) to purple (deeper). The land and continental shelf are shown in grayscale slope shading where darker colors represent steeper slopes.

Topography and bathymetry of southern Cascadia, which includes southern Oregon and northern California (seafloor depths between 200 and 3000 m are shown in the spectrum color scale from red (shallower) to purple (deeper). The land and continental shelf are shown in grayscale slope shading where darker colors represent steeper slopes.

A scientist on an all-terrain vehicle next to a tall permafrost bluff on a sandy coastline
Mapping Barter Island on an All Terrain Vehicle (ATV)
Mapping Barter Island on an All Terrain Vehicle (ATV)
Mapping Barter Island on an All Terrain Vehicle (ATV)

High ice content permafrost bluff erosion at Barter Island in 2019 after several coastal storms and a prolonged time of anomalously high air temperatures. 

3 separate images of sediment samples
Sediment Samples
Sediment Samples
Sediment Samples

Once removed from the pressure core testing tool, this specimen shows that it is not a homogeneous sediment.  The mostly fine-grained sample (dark sediment in all three images) easily breaks apart at a thin layer of coarse-grained sediment (light sediment on the inner core surfaces of images (i) and (ii).

Once removed from the pressure core testing tool, this specimen shows that it is not a homogeneous sediment.  The mostly fine-grained sample (dark sediment in all three images) easily breaks apart at a thin layer of coarse-grained sediment (light sediment on the inner core surfaces of images (i) and (ii).

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