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Volcano Hazard Program images.

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Technologies track surface changes at Yellowstone....
Technologies track surface changes at Yellowstone.
Technologies track surface changes at Yellowstone.
Technologies track surface changes at Yellowstone.

Summer geology intern Mindy Juergenson climbs over downed lodgepole pine trees killed in the fire of 1988 as she packs a GPS station out of the field (inset). Nine temporary stations are deployed each April/May and retrieved in October/November. The temporary stations supplement a network of permanent stations that record ground deformation data year-round.

Summer geology intern Mindy Juergenson climbs over downed lodgepole pine trees killed in the fire of 1988 as she packs a GPS station out of the field (inset). Nine temporary stations are deployed each April/May and retrieved in October/November. The temporary stations supplement a network of permanent stations that record ground deformation data year-round.

Horizontal displacement vectors for GPS stations at Mount St. Helen...
Horizontal displacement vectors at Mount St. Helens (2008-2014)
Horizontal displacement vectors at Mount St. Helens (2008-2014)
Horizontal displacement vectors at Mount St. Helens (2008-2014)

Map of horizontal displacement vectors for Global Positioning System (GPS) stations in and around Mount St. Helens. Blue arrows show the direction and magnitude of horizontal movement, as measured at the GPS station from 2008-2014. The total horizontal displacement is indicated in millimeters (mm) and inches (in).

Map of horizontal displacement vectors for Global Positioning System (GPS) stations in and around Mount St. Helens. Blue arrows show the direction and magnitude of horizontal movement, as measured at the GPS station from 2008-2014. The total horizontal displacement is indicated in millimeters (mm) and inches (in).

Children pose with 8 ton ballistic block at Kīlauea volcano, Hawai‘...
Children pose with 8 ton ballistic block at Kīlauea, Hawai‘i.
Children pose with 8 ton ballistic block at Kīlauea, Hawai‘i.
Children pose with 8 ton ballistic block at Kīlauea, Hawai‘i.

Some of the large ballistic blocks from the Kīlauea eruption of 1924 later became visitor attractions. Many of these blocks remain in place today as evidence of the forces unleashed at Kīlauea during the eruption of 1924.

Some of the large ballistic blocks from the Kīlauea eruption of 1924 later became visitor attractions. Many of these blocks remain in place today as evidence of the forces unleashed at Kīlauea during the eruption of 1924.

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.

Screenshot from HVO's seismic-event-review software AQMS....
Screenshot from HVO's seismic-event-review software AQMS.
Screenshot from HVO's seismic-event-review software AQMS.
Screenshot from HVO's seismic-event-review software AQMS.

HVO seismologists use this to review automatically generated earthquake parameters (location, depth, magnitude), measure P- and S-wave arrival times, and re-compute earthquake hypocenter and magnitudes for cataloging and distribution to the public.

HVO seismologists use this to review automatically generated earthquake parameters (location, depth, magnitude), measure P- and S-wave arrival times, and re-compute earthquake hypocenter and magnitudes for cataloging and distribution to the public.

The Modified Mercalli Intensity (MMI) Scale assigns intensities as ...
The Modified Mercalli Intensity (MMI) Scale assigns intensities as ...
The Modified Mercalli Intensity (MMI) Scale assigns intensities as ...
The Modified Mercalli Intensity (MMI) Scale assigns intensities as ...

Although numerous intensity scales have been developed over the last several hundred years to evaluate the effects of earthquakes, the one currently used in the United States is the Modified Mercalli Intensity (MMI) Scale. It was developed in 1931 by the American seismologists Harry Wood and Frank Neumann.

Although numerous intensity scales have been developed over the last several hundred years to evaluate the effects of earthquakes, the one currently used in the United States is the Modified Mercalli Intensity (MMI) Scale. It was developed in 1931 by the American seismologists Harry Wood and Frank Neumann.

Researchers generate a bathymetric contour map of Castle Lake, near...
A bathymetric contour map of Castle Lake, Mount St. Helens.
A bathymetric contour map of Castle Lake, Mount St. Helens.
A bathymetric contour map of Castle Lake, Mount St. Helens.

Researchers map the bottom of Castle Lake, near Mount St. Helens. For three days, researchers ran a small boat over the lake surface equipped with an acoustic Doppler current profiler (ADCP). The ADCP bounces an acoustic wave off the bottom that is reflected back to a mobile receiver in the boat.

Researchers map the bottom of Castle Lake, near Mount St. Helens. For three days, researchers ran a small boat over the lake surface equipped with an acoustic Doppler current profiler (ADCP). The ADCP bounces an acoustic wave off the bottom that is reflected back to a mobile receiver in the boat.

CalVO staff assembled in the Rambo Auditorium, Menlo Park, CA...
CalVO staff
CalVO staff
CalVO staff

CalVO staff assembled in the Rambo Auditorium, Menlo Park, CA

CalVO staff assembled in the Rambo Auditorium, Menlo Park, CA

Scientist collects a sample of gas in a vacuum sealed glass bottle ...
Scientist collect sample of gas near Nymph Lake
Scientist collect sample of gas near Nymph Lake
Scientist collect sample of gas near Nymph Lake

Scientist collects a sample of gas in a vacuum sealed glass bottle near Nymph Lake, Yellowstone National Park.

Location of magma formation, accumulation, and storage beneath Moun...
Location of magma formation, accumulation, and storage beneath Moun...
Location of magma formation, accumulation, and storage beneath Moun...
Location of magma formation, accumulation, and storage beneath Moun...

Magma forms above the subducting slab of oceanic crust and accumulates at the base of Earth's rigid crust before collecting in a storage zone 13 km (8 mi) beneath the volcano prior to eruption.

Magma forms above the subducting slab of oceanic crust and accumulates at the base of Earth's rigid crust before collecting in a storage zone 13 km (8 mi) beneath the volcano prior to eruption.

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.

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.

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.

Monitoring the Aleutian Volcanic Arc from Space...
Monitoring the Aleutian Volcanic Arc from Space
Monitoring the Aleutian Volcanic Arc from Space
Monitoring the Aleutian Volcanic Arc from Space

InSAR (Interferometric Synthetic Aperture Radar) is a technique for mapping subtle ground deformation using radar images from Earth-orbiting satellites. With its global coverage and all-weather imaging capability, InSAR has become an increasingly important technique for studying volcanoes in remote regions such as the Aleutian Islands.

InSAR (Interferometric Synthetic Aperture Radar) is a technique for mapping subtle ground deformation using radar images from Earth-orbiting satellites. With its global coverage and all-weather imaging capability, InSAR has become an increasingly important technique for studying volcanoes in remote regions such as the Aleutian Islands.

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

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).

Ash buries cars and buildings after the 1984 eruption of Rabaul, Pa...
Ash buries cars and buildings after 1984 eruption of Rabaul
Ash buries cars and buildings after 1984 eruption of Rabaul
Ash buries cars and buildings after 1984 eruption of Rabaul

Ash buries cars and buildings after the 1984 eruption of Rabaul, Papua New Guinea.

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