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Images related to natural hazards.

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Map showing the thickness of a relatively young Pleistocene outwash lobe
Map showing the thickness of a relatively young Pleistocene outwash
Map showing the thickness of a relatively young Pleistocene outwash
Map showing the thickness of a relatively young Pleistocene outwash

 

Map showing the thickness of a relatively young Pleistocene outwash lobe in meters mapped using chirp seismic-reflection profiles collected in 2011, overlain on acoustic backscatter imagery. Regional bathymetric contours are in meters.

 

Map showing the thickness of a relatively young Pleistocene outwash lobe in meters mapped using chirp seismic-reflection profiles collected in 2011, overlain on acoustic backscatter imagery. Regional bathymetric contours are in meters.

Numerical model grids
Numerical model grids
Numerical model grids
Numerical model grids

Numerical model grids showing downscaling from larger regional grid (far right) to more refined coastal grid (left). Colors are bathymetry (m).

Numerical model grids showing downscaling from larger regional grid (far right) to more refined coastal grid (left). Colors are bathymetry (m).

Example of a rip current experiment.
Example of a rip current experiment.
Example of a rip current experiment.
Example of a rip current experiment.

Example of a rip current experiment. Colors show bathymetry and arrows show velocity vectors after 1 h of model simulation. Similar to results in Kumar and others, 2012.

Example of a rip current experiment. Colors show bathymetry and arrows show velocity vectors after 1 h of model simulation. Similar to results in Kumar and others, 2012.

Ice-chilled lava columns at the end of a Glacier Peak lava flow, Wa...
Ice-chilled lava columns at the end of a Glacier Peak lava flow, WA.
Ice-chilled lava columns at the end of a Glacier Peak lava flow, WA.
Ice-chilled lava columns at the end of a Glacier Peak lava flow, WA.

Impressive columns like these form along the margins of ice-confined lava flows but usually are eroded off the sides due to continued glacial movement after an eruption ceases. Columns are better preserved at the ends of the flows (this photo) where they are protected somewhat from the ice.

Impressive columns like these form along the margins of ice-confined lava flows but usually are eroded off the sides due to continued glacial movement after an eruption ceases. Columns are better preserved at the ends of the flows (this photo) where they are protected somewhat from the ice.

Map of the extent of Newberry lavas including approximate ages of s...
Extent of Newberry lavas including approximate ages of surficial flows
Extent of Newberry lavas including approximate ages of surficial flows
Extent of Newberry lavas including approximate ages of surficial flows

Extending approximately 75 miles north to south and 27 miles east to west, Newberry Volcano and its broad apron of lavas (light yellow shaded area) cover a total area of almost 1,200 square miles, making it the largest volcano of the Cascades volcanic chain. Its lavas stretch north beyond Smith Rock State Park, and south almost to Fort Rock State Natural Area.

Extending approximately 75 miles north to south and 27 miles east to west, Newberry Volcano and its broad apron of lavas (light yellow shaded area) cover a total area of almost 1,200 square miles, making it the largest volcano of the Cascades volcanic chain. Its lavas stretch north beyond Smith Rock State Park, and south almost to Fort Rock State Natural Area.

building damaged by an earthquake
Earthquake-damaged building
Earthquake-damaged building
Earthquake-damaged building

Building damanged by the February 2011 earthquake in Christchurch, New Zealand.

Building damanged by the February 2011 earthquake in Christchurch, New Zealand.

Toe of the active Cleveland Corral landslide in 2011
Cleveland Corral landslide in 2011
Cleveland Corral landslide in 2011
Cleveland Corral landslide in 2011

Toe of the active Cleveland Corral landslide in 2011, perched above US Highway 50 in distance.  Movement typically only occurs during wet winter and spring months.

Toe of the active Cleveland Corral landslide in 2011, perched above US Highway 50 in distance.  Movement typically only occurs during wet winter and spring months.

Map showing Holocene (modern) sediment thickness in meters
Map showing Holocene (modern) sediment thickness
Map showing Holocene (modern) sediment thickness
Map showing Holocene (modern) sediment thickness

Map showing Holocene (modern) sediment thickness in meters overlain on bathymetry. Regional bathymetric contours are in meters. Note the shoreface-attached sand ridges west of Watch Hill.

Map showing Holocene (modern) sediment thickness in meters overlain on bathymetry. Regional bathymetric contours are in meters. Note the shoreface-attached sand ridges west of Watch Hill.

Geologists examining ash layers associated with the Dusty assemblag...
Geologists examining ash layers associated with the Dusty assemblag...
Geologists examining ash layers associated with the Dusty assemblag...
Geologists examining ash layers associated with the Dusty assemblag...

The orange layer just below geologist's hiking pole is the Mazama ash (about 7700 ybp). Below that are glacial deposits. Above the Mazama is about a meter consisting mostly of fine-grained tephras from Glacier Peak, capped by soil and plants. That the tephras sit directly on top of the Mazama indicates that "Dusty" eruptions commenced about 7,000 years ago.

The orange layer just below geologist's hiking pole is the Mazama ash (about 7700 ybp). Below that are glacial deposits. Above the Mazama is about a meter consisting mostly of fine-grained tephras from Glacier Peak, capped by soil and plants. That the tephras sit directly on top of the Mazama indicates that "Dusty" eruptions commenced about 7,000 years ago.

Computer-generated illustration of high-resolution seafloor maps created with data collected.
San Diego Trough fault
San Diego Trough fault
San Diego Trough fault

Bird's-eye view map of a section of the seafloor off southern California, made with depth data. The map shows a channel wall that has been cut by the San Diego Trough fault and moved about 20 meters. This feature is about 1,000 meters below sea level.

Bird's-eye view map of a section of the seafloor off southern California, made with depth data. The map shows a channel wall that has been cut by the San Diego Trough fault and moved about 20 meters. This feature is about 1,000 meters below sea level.

Map of backscatter intensity and sun-illuminated topography on Stellwagen Bank
Backscatter intensity on Stellwagen Bank
Backscatter intensity on Stellwagen Bank
Backscatter intensity on Stellwagen Bank

Map C.  Backscatter intensity and sun-illuminated topography.  Blue= "soft" seabed, Green, orange = "hard" seabed

Map of Worldwide distribution of observed and inferred gas hydrates
Worldwide distribution of observed and inferred gas hydrates
Worldwide distribution of observed and inferred gas hydrates
Worldwide distribution of observed and inferred gas hydrates

Worldwide distribution of observed and inferred gas hydrates in marine and permafrost-associated settings that have been the subject of drilling programs. The color coding refers to the primary sediment type in each location and therefore designates the likely type of gas hydrate reservoir at each site.

Worldwide distribution of observed and inferred gas hydrates in marine and permafrost-associated settings that have been the subject of drilling programs. The color coding refers to the primary sediment type in each location and therefore designates the likely type of gas hydrate reservoir at each site.

Deployment period storm analysis.
Deployment period storm analysis.
Deployment period storm analysis.
Deployment period storm analysis.

Deployment period storm analysis. (A) significant wave height (red line) and wind speed and direction (arrows). Shading represents storm type (blue = cold front, red = warm front, yellow = low-pressure). (B) Vertical profiles of suspended-sediment concentration. (C) Cumulative along-shore and cross-shore sediment flux.

Deployment period storm analysis. (A) significant wave height (red line) and wind speed and direction (arrows). Shading represents storm type (blue = cold front, red = warm front, yellow = low-pressure). (B) Vertical profiles of suspended-sediment concentration. (C) Cumulative along-shore and cross-shore sediment flux.

Mount Rainier rises above Tacoma, Washington and boat harbor, which...
Mount Rainier rises above Tacoma, WA and boat harbor, which may be ...
Mount Rainier rises above Tacoma, WA and boat harbor, which may be ...
Mount Rainier rises above Tacoma, WA and boat harbor, which may be ...

Mount Rainier rises above Tacoma, Washington and boat harbor, which may be impacted during the next eruption of the volcano.

Three men and one woman stand, smiling, on the fantail of a docked boat in a marina, holding an instrument used to collect data.
PCMSC Magnetometer
PCMSC Magnetometer
PCMSC Magnetometer

USGS Pacific Coastal and Marine Science Center field crew showing off the new magnetometer, named Magnetron, on fantail of Research Vessel (R/V) Parke Snavely.

USGS Pacific Coastal and Marine Science Center field crew showing off the new magnetometer, named Magnetron, on fantail of Research Vessel (R/V) Parke Snavely.

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