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Images related to natural hazards.

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Subduction of the Juan de Fuca plate beneath the North American pla...
Subduction of the Juan de Fuca plate beneath the North American pla...
Subduction of the Juan de Fuca plate beneath the North American pla...
Subduction of the Juan de Fuca plate beneath the North American pla...

Oceanic crust forms by eruptions along the Juan de Fuca ridge. As the Juan de Fuca plate drifts eastward, it cools, becomes more dense, and eventually dives under the less dense continental plate at the Cascadia trench.

Oceanic crust forms by eruptions along the Juan de Fuca ridge. As the Juan de Fuca plate drifts eastward, it cools, becomes more dense, and eventually dives under the less dense continental plate at the Cascadia trench.

Columbian photographer Reid Blackburn's camera, recovered from the ...
Columbian photographer Reid Blackburn's camera, recovered from the ...
Columbian photographer Reid Blackburn's camera, recovered from the ...
Columbian photographer Reid Blackburn's camera, recovered from the ...

Columbian photographer Reid Blackburn's camera, recovered from the Mount St. Helens blast zone in 1980. The film in it was too damaged to yield images.

Volcano Disaster Assistance scientists working with colleagues from...
Volcano Disaster Assistance scientists working with colleagues from...
Volcano Disaster Assistance scientists working with colleagues from...
Volcano Disaster Assistance scientists working with colleagues from...

The station is a lahar monitoring station with a broadband seismometer and video camera. Data from the station use radio telemetry to send real time information to the Instituto Geofisico of Ecuador.

The station is a lahar monitoring station with a broadband seismometer and video camera. Data from the station use radio telemetry to send real time information to the Instituto Geofisico of Ecuador.

Pyroclastic flow cartoon depicting the flow moving down the slope o...
Pyroclastic flow cartoon depicting the flow moving down the slope o...
Pyroclastic flow cartoon depicting the flow moving down the slope o...
Example of an event-tree schematic used when forecasting the probab...
Example of an event-tree schematic used when forecasting the probab...
Example of an event-tree schematic used when forecasting the probab...
Example of an event-tree schematic used when forecasting the probab...

Example of an event-tree schematic used when forecasting the probable scenarios that may play out in the event of volcanic unrest or eruption. Scenarios are updated as events unfold.

Example of an event-tree schematic used when forecasting the probable scenarios that may play out in the event of volcanic unrest or eruption. Scenarios are updated as events unfold.

Emergency response planning exercise for a volcanic event with Wash...
Emergency response planning exercise for a volcanic event with WA S...
Emergency response planning exercise for a volcanic event with WA S...
Emergency response planning exercise for a volcanic event with WA S...

Emergency response planning exercise for a volcanic event with Washington State and local government officials.

Ash Homepage Sidebar...
Ash Homepage Sidebar
Ash Homepage Sidebar
Ash Homepage Sidebar

Three images of crop damage, ash plume and cleanup for the homepage

Three images of crop damage, ash plume and cleanup for the homepage

ash damage to sewage pump impellers...
Ash damage to sewage pump impellers.
Ash damage to sewage pump impellers.
Ash damage to sewage pump impellers.

Ashfall will cause accelerated wear and tear on sewage pump impellers (metal pitting and thinning).

Ashfall will cause accelerated wear and tear on sewage pump impellers (metal pitting and thinning).

Shield-building is second, most voluminous, stage of Hawaiian volca...
Shield-building is second, most voluminous, stage of Hawaiian volca...
Shield-building is second, most voluminous, stage of Hawaiian volca...
Shield-building is second, most voluminous, stage of Hawaiian volca...

Drill records have found traces of previously formed shorelines (strandlines) depressed below the current sea level - further evidence of subsidence due to the added weight of the volcano.

Drill records have found traces of previously formed shorelines (strandlines) depressed below the current sea level - further evidence of subsidence due to the added weight of the volcano.

American and Colombian exchange participants among the ruins in Ame...
American and Colombian exchange participants among the ruins in Ame...
American and Colombian exchange participants among the ruins in Ame...
American and Colombian exchange participants among the ruins in Ame...

American and Colombian exchange participants among the ruins in Amero, which was destroyed by an eruption of Nevado del Ruiz in 1985.

Relative explosiveness and resulting height of eruption columns typ...
Relative explosiveness and resulting height of eruption columns typ...
Relative explosiveness and resulting height of eruption columns typ...
Relative explosiveness and resulting height of eruption columns typ...

Relative explosiveness and resulting height of eruption columns typically associated with different styles of eruption

Trace of Augustine ash on car hood, Homer, Alaska, January 2006....
Trace of Aug.ine ash on car hood, Homer, AK, Jan 2006.
Trace of Aug.ine ash on car hood, Homer, AK, Jan 2006.
Geomorphic response to the breaching of the Condit Dam, White Salmo...
Geomorphic response to breaching of Condit Dam, White Salmon River, WA
Geomorphic response to breaching of Condit Dam, White Salmon River, WA
Geomorphic response to breaching of Condit Dam, White Salmon River, WA

White Salmon River (Washington) at USGS gauge site, 2.3 km downstream of Condit Dam, looking downstream: (a) 53 min before breaching; (b) 20 min after breaching, at discharge peak; (c) 76 min after breaching, at peak sediment concentration, with high water line evident; (d) ~2.5 h after breaching, discharge has returned to background and sediment concentration is f

White Salmon River (Washington) at USGS gauge site, 2.3 km downstream of Condit Dam, looking downstream: (a) 53 min before breaching; (b) 20 min after breaching, at discharge peak; (c) 76 min after breaching, at peak sediment concentration, with high water line evident; (d) ~2.5 h after breaching, discharge has returned to background and sediment concentration is f

Hood to protect air intake from ashfall for GenSet equipment in Bar...
Hood to protect air intake from ashfall for GenSet equipment in Bar...
Hood to protect air intake from ashfall for GenSet equipment in Bar...
Hood to protect air intake from ashfall for GenSet equipment in Bar...

Hood to protect air intake from ashfall for GenSet equipment in Bariloche, Argentina, following 2011-2012 eruption of Cordon Caulle volcano, Chile.

Field guide tracks flood basalts, rhyolites and post-plume volcanis...
Field guide tracks flood basalts, rhyolites and post-plume volcanism
Field guide tracks flood basalts, rhyolites and post-plume volcanism
Field guide tracks flood basalts, rhyolites and post-plume volcanism

Field-trip guide to Columbia River flood basalts, associated rhyolites, and diverse post-plume volcanism in eastern Oregon available at https://pubs.er.usgs.gov/publication/sir20175022O.

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