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Volcano Hazard Program images.

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Thickness of ash (and larger-sized particles within 20-40 km) that ...
Thickness of ash (and larger-sized particles within 20-40 km) that ...
Thickness of ash (and larger-sized particles within 20-40 km) that ...
Thickness of ash (and larger-sized particles within 20-40 km) that ...

Graph shows thickness of ash (and larger-sized particles within 20-40 km) that fell to the ground downwind of Mount St. Helens during the eruption on May 18, 1980. The volcano ejected a minimum of 1.1 km3 of uncompacted tephra, which is equivalent to 0.20-0.25 km3 of magma or solid rock.

Graph shows thickness of ash (and larger-sized particles within 20-40 km) that fell to the ground downwind of Mount St. Helens during the eruption on May 18, 1980. The volcano ejected a minimum of 1.1 km3 of uncompacted tephra, which is equivalent to 0.20-0.25 km3 of magma or solid rock.

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

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