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Volcano Hazard Program images.

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Seismic hazard for the State of Hawaii based on past earthquakes an...
Seismic hazard for the State of Hawaii based on past earthquakes an...
Seismic hazard for the State of Hawaii based on past earthquakes an...
Seismic hazard for the State of Hawaii based on past earthquakes an...

Seismic hazard across the State of Hawaii, with high seismic hazards depicted with warm colors (red-orange) and relatively low seismic hazards depicted with cool colors (green). Engineers use these types of maps to prescribe building codes known as Seismic Design Codes (SDC) and create earthquake resistant structures.

Seismic hazard across the State of Hawaii, with high seismic hazards depicted with warm colors (red-orange) and relatively low seismic hazards depicted with cool colors (green). Engineers use these types of maps to prescribe building codes known as Seismic Design Codes (SDC) and create earthquake resistant structures.

The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...
The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...
The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...
The Hawaiian Islands (red) and Hawaiian Ridge-Emperor Seamounts vol...

Vectors indicate Pacific Plate motion relative to presumed fixed mantle hot spot in millimeters per year. Gray lines indicate fracture zones. Isochrons along the Emperor Seamounts chain show the age of volcanism in millions of years. Ocean floor ages from imagery available on EarthByte.

Vectors indicate Pacific Plate motion relative to presumed fixed mantle hot spot in millimeters per year. Gray lines indicate fracture zones. Isochrons along the Emperor Seamounts chain show the age of volcanism in millions of years. Ocean floor ages from imagery available on EarthByte.

Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...
Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...
Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...
Before the eruption of May 18, 1980, Mount St. Helens' elevation wa...

Mount Adams elevation is 3,745 m (12, 286 ft). Mount St. Helens was the smallest of five major volcanic peaks in Washington State.

South Sister northwest flank. Right shoulder at skyline is thin she...
South Sister NW flank. Right shoulder at skyline is thin sheet of m...
South Sister NW flank. Right shoulder at skyline is thin sheet of m...
South Sister NW flank. Right shoulder at skyline is thin sheet of m...

South Sister northwest flank. Right shoulder at skyline is thin sheet of mafic material from 22ka summit eruption. Red cinders in headwall cirques are layered with dipping lava flows.

South Sister northwest flank. Right shoulder at skyline is thin sheet of mafic material from 22ka summit eruption. Red cinders in headwall cirques are layered with dipping lava flows.

USGS-CVO building sign, Vancouver, Washington....
USGS-CVO building sign, Vancouver, WA.
USGS-CVO building sign, Vancouver, WA.
Geologic Map of the Washougal Quadrangle, Clark County, Washington ...
Geologic Map of Washougal Quadrangle
Geologic Map of Washougal Quadrangle
Geologic Map of Washougal Quadrangle

Geologic Map of the Washougal Quadrangle, Clark County, Washington and Multnomah County, Oregon (Scientific Investigation Map 3257).

Geologic Map of the Washougal Quadrangle, Clark County, Washington and Multnomah County, Oregon (Scientific Investigation Map 3257).

Postshield eruption are the fourth stage of a Hawaiian volcano's ev...
Postshield eruption are the fourth stage of a Hawaiian volcano's ev...
Postshield eruption are the fourth stage of a Hawaiian volcano's ev...
Postshield eruption are the fourth stage of a Hawaiian volcano's ev...

Postshield eruption are the fourth stage of a Hawaiian volcano's evolution. A cap of evolved magma erupts to cover the surface of the volcano. Not all volcanoes have evidence for this phase.

Postshield eruption are the fourth stage of a Hawaiian volcano's evolution. A cap of evolved magma erupts to cover the surface of the volcano. Not all volcanoes have evidence for this phase.

Rejuvenated stage volcanism occurs after the volcano has moved away...
Rejuvenated stage volcanism occurs after the volcano has moved away...
Rejuvenated stage volcanism occurs after the volcano has moved away...
Rejuvenated stage volcanism occurs after the volcano has moved away...

Rejuvenated stage volcanism occurs after the volcano has moved away from the mantle hot spot. Eruptions occur in sporadic locations and may be interspersed with long periods of erosion.

Rejuvenated stage volcanism occurs after the volcano has moved away from the mantle hot spot. Eruptions occur in sporadic locations and may be interspersed with long periods of erosion.

Examples of seismograms of different types of earthquakes and tremo...
Examples of seismograms of different types of earthquakes and tremo...
Examples of seismograms of different types of earthquakes and tremo...
Examples of seismograms of different types of earthquakes and tremo...

Examples of seismograms of different types of earthquakes and tremor (constant ground shaking) recorded in Hawai‘i.

An American exchange participant views the former hospital in Amero...
An American exchange participant views the former hospital in Amero...
An American exchange participant views the former hospital in Amero...
An American exchange participant views the former hospital in Amero...

An American exchange participant views the former hospital in Amero where the entire first floor was buried by lahars from Nevado del Ruiz (the second floor is visible).

U.S. and Chilean scientists prepare for a research flight during th...
U.S. and Chilean scientists prepare for a research flight during th...
U.S. and Chilean scientists prepare for a research flight during th...
U.S. and Chilean scientists prepare for a research flight during th...

U.S. and Chilean scientists prepare for a research flight during the 2008 VDAP eruption response at Chaitén.

Michael Poland, Scientist-in-Charge of the Yellowstone Volcano Obse...
Michael Poland, Scientist-in-Charge of the YVO
Michael Poland, Scientist-in-Charge of the YVO
Michael Poland, Scientist-in-Charge of the YVO

Michael Poland, Scientist-in-Charge of the Yellowstone Volcano Observatory.

Digital topography from high-resolution digital elevation dataset u...
Digital topography from high-resolution digital elevation dataset u...
Digital topography from high-resolution digital elevation dataset u...
Digital topography from high-resolution digital elevation dataset u...

View of Mount Baker from the west. Summit area draped with aerial imagery from National Agriculture Imagery Program (NAIP) collected in September 2015. Digital topography from High-resolution digital elevation dataset for Mount Baker and vicinity, Washington, based on lidar surveys of 2015: U.S.

View of Mount Baker from the west. Summit area draped with aerial imagery from National Agriculture Imagery Program (NAIP) collected in September 2015. Digital topography from High-resolution digital elevation dataset for Mount Baker and vicinity, Washington, based on lidar surveys of 2015: U.S.

Collapsed roofs after severe ashfall from Galunggung Volcano, West ...
Collapsed roofs after ashfall from Galunggung Volcano, Indonesia
Collapsed roofs after ashfall from Galunggung Volcano, Indonesia
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...

Block diagram showing subduction of the Juan de Fuca Plate beneath the North American Plate along the Cascadia Trench, which is the western edge of the Cascadia subduction zone. Oceanic crust forms by eruptions along the Juan de Fuca Ridge.

Block diagram showing subduction of the Juan de Fuca Plate beneath the North American Plate along the Cascadia Trench, which is the western edge of the Cascadia subduction zone. Oceanic crust forms by eruptions along the Juan de Fuca Ridge.

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