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Volcano Hazard Program images.

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Airborne images of Tern Lake, Yellowstone 1994 2006 2017
High-spatial-resolution airborne images of Tern Lake, Yellowstone
High-spatial-resolution airborne images of Tern Lake, Yellowstone
High-spatial-resolution airborne images of Tern Lake, Yellowstone

High-spatial-resolution airborne images of the Tern Lake area from 1994, 2006, and 2017. The area of bright pixels identified in the Landsat-8 thermal infrared image corresponds to a newly emerging area of warm ground and tree kills about 32,500 m2 (8 acres, or 4 soccer fields) in area.

High-spatial-resolution airborne images of the Tern Lake area from 1994, 2006, and 2017. The area of bright pixels identified in the Landsat-8 thermal infrared image corresponds to a newly emerging area of warm ground and tree kills about 32,500 m2 (8 acres, or 4 soccer fields) in area.

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Native sulfur crystals precipitate at Sulphur Banks via a chemical reaction betw
Native sulfur crystals precipitate at Sulphur Banks via a chemical reaction betw
Native sulfur crystals precipitate at Sulphur Banks via a chemical reaction betw

Native sulfur crystals precipitate at Sulphur Banks via a chemical reaction between different sulfur-bearing volcanic gases. USGS image by P. Nadeau.

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Collecting gas samples at Sulphur Banks
Collecting gas samples at Sulphur Banks
Collecting gas samples at Sulphur Banks

HVO gas geochemists periodically collect gas samples at Sulphur Banks, near the Kīlauea Visitor Center, in Hawai‘i Volcanoes National Park. Samples are analyzed for bulk chemistry and for helium isotopes. The results are compared to previous measurements to evaluate potential changes in activity at the volcano.

HVO gas geochemists periodically collect gas samples at Sulphur Banks, near the Kīlauea Visitor Center, in Hawai‘i Volcanoes National Park. Samples are analyzed for bulk chemistry and for helium isotopes. The results are compared to previous measurements to evaluate potential changes in activity at the volcano.

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An HVO geologist removes the sampling tube following the gas collection. Inserti
An HVO geologist removes the sampling tube following the gas collection. Inserti
An HVO geologist removes the sampling tube following the gas collection. Inserti

An HVO geologist removes the sampling tube following the gas collection. Inserting the tube down into the degassing source limits contamination of the volcanic gas sample by atmospheric gases. USGS image by P. Nadeau.

NASA Yellowstone astrobiology team at Great Fountain Geyser
NASA Yellowstone astrobiology team at Great Fountain Geyser
NASA Yellowstone astrobiology team at Great Fountain Geyser
NASA Yellowstone astrobiology team at Great Fountain Geyser

NASA Yellowstone astrobiology expedition team members stand in front of Great Fountain Geyser after completion of field work, February 28, 2019. Research conducted under Yellowstone Research Permit YELL-2019-SCI-8094.

NASA Yellowstone astrobiology expedition team members stand in front of Great Fountain Geyser after completion of field work, February 28, 2019. Research conducted under Yellowstone Research Permit YELL-2019-SCI-8094.

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Reading the rainbow: How to interpret an interferogram
Reading the rainbow: How to interpret an interferogram
Reading the rainbow: How to interpret an interferogram

COSMO-SkyMed (CSK) Interferogram for the period from April 6 to June 2, 2019, covering Kīlauea Volcano's summit region. Each color fringe represents 1.65 centimeters (0.65 inches) of ground displacement.

COSMO-SkyMed (CSK) Interferogram for the period from April 6 to June 2, 2019, covering Kīlauea Volcano's summit region. Each color fringe represents 1.65 centimeters (0.65 inches) of ground displacement.

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Montana State University students at an outcrop along Highway 20, in Idaho, samp
Montana State University students at an outcrop along Highway 20, in Idaho, samp
Montana State University students at an outcrop along Highway 20, in Idaho, samp

Montana State University students at an outcrop along Highway 20, in Idaho, sampling the Mesa Falls Tuff fall deposit exposed just beneath the ignimbrite. Photo by Madison Myers (Montana State University) on June 9, 2019.

Montana State University students at an outcrop along Highway 20, in Idaho, sampling the Mesa Falls Tuff fall deposit exposed just beneath the ignimbrite. Photo by Madison Myers (Montana State University) on June 9, 2019.

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The California Volcano Observatory Magma Dynamics Lab in Menlo Park.
The California Volcano Observatory Magma Dynamics Lab in Menlo Park.
The California Volcano Observatory Magma Dynamics Lab in Menlo Park.

Magma dynamics experiments seek to recreate the pressure and temperature at depths far beneath a volcano, in order to determine how the magma forms, evolves, and ascends prior to eruption.

Magma dynamics experiments seek to recreate the pressure and temperature at depths far beneath a volcano, in order to determine how the magma forms, evolves, and ascends prior to eruption.

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USGS to survey Kīlauea Volcano from its summit to Kumukahi
USGS to survey Kīlauea Volcano from its summit to Kumukahi
USGS to survey Kīlauea Volcano from its summit to Kumukahi

Areas on Kīlauea that will be covered by a helicopter lidar survey in June 2019. Red lines enclose areas over which the survey helicopter will fly at 396 m (1,300 ft) above ground level. Green lines enclose areas over which the helicopter will fly at 151 m (500 ft) above ground level. USGS map.

Areas on Kīlauea that will be covered by a helicopter lidar survey in June 2019. Red lines enclose areas over which the survey helicopter will fly at 396 m (1,300 ft) above ground level. Green lines enclose areas over which the helicopter will fly at 151 m (500 ft) above ground level. USGS map.

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Map showing the three types of young faults in Yellowstone National Park.
Map showing the three types of young faults in Yellowstone National Park.
Map showing the three types of young faults in Yellowstone National Park.

Map showing the three types of young faults in Yellowstone National Park. Courtesy of the Wyoming State Geological Survey.

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Schematic illustration showing the inferred irregular conduit geometries of (a)
Schematic illustration showing the inferred irregular conduit geometries of (a)
Schematic illustration showing the inferred irregular conduit geometries of (a)

Schematic illustration showing the inferred irregular conduit geometries of (a) Old Faithful geyser, in Yellowstone National Park; (b) Velikan geyser, in Kamchatka, Russia, with boulders at the bottom depicted in brown; and (c) Geysir, in Iceland. The walls of the conduits are lined with white silica sinter similar to that exposed on the surface.

Schematic illustration showing the inferred irregular conduit geometries of (a) Old Faithful geyser, in Yellowstone National Park; (b) Velikan geyser, in Kamchatka, Russia, with boulders at the bottom depicted in brown; and (c) Geysir, in Iceland. The walls of the conduits are lined with white silica sinter similar to that exposed on the surface.

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Schematic illustration showing the inferred subsurface structure of Geyser Flat,
Schematic illustration showing the inferred subsurface structure of Geyser Flat,
Schematic illustration showing the inferred subsurface structure of Geyser Flat,

Schematic illustration showing the inferred subsurface structure of Geyser Flat, Whakarewarewa, in the Taupo Volcanic Zone, New Zealand. From manuscript by Hurwitz and Manga (Annual Review of Earth and Planetary Sciences, 2017. Vol. 45, pp. 31–59).

Schematic illustration showing the inferred subsurface structure of Geyser Flat, Whakarewarewa, in the Taupo Volcanic Zone, New Zealand. From manuscript by Hurwitz and Manga (Annual Review of Earth and Planetary Sciences, 2017. Vol. 45, pp. 31–59).

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Kīlauea Summit
Kīlauea Summit
Kīlauea Summit

USGS geologists are conducting field work at the summit today to make observations of volcanic ash and measure volcanic gas. This photograph is taken on Crater Rim Drive where the road intersects the Southwest Rift Zone. Rockfall dust and volcanic ash covers the ground and cracks in line with the Southwest Rift Zone trace traverse the pavement.

USGS geologists are conducting field work at the summit today to make observations of volcanic ash and measure volcanic gas. This photograph is taken on Crater Rim Drive where the road intersects the Southwest Rift Zone. Rockfall dust and volcanic ash covers the ground and cracks in line with the Southwest Rift Zone trace traverse the pavement.

Geological time scale showing the geologic eons, eras, periods, epochs, and associated ages in millions of years ago (MYA)
Geological time scale showing the geologic eons, eras, periods, epochs, and associated ages in millions of years ago (MYA)
Geological time scale showing the geologic eons, eras, periods, epochs, and associated ages in millions of years ago (MYA)
Geological time scale showing the geologic eons, eras, periods, epochs, and associated ages in millions of years ago (MYA)

Geologic time scale showing the geologic eons, eras, periods, epochs, and associated ages in millions of years ago (MYA). The time scale also shows major evolutionary and tectonic events in North America.

A two part figure with a shaded-relief map view of the Long Valley Caldera marked with the outlines of its resurgent dome, Mammoth Mountain, Crowley Lake, the caldera outline, and major roads. Below is a west-to-east cross-section cartoon of the caldera, showing the locations of these features as well as the depth of caldera fill, basement rocks, and the paths of cold and hot water near magmatic intrusions.
Simplified geologic map (left) and diagrammatic cross section (right) of Long Valley Caldera.
Simplified geologic map (left) and diagrammatic cross section (right) of Long Valley Caldera.
Views of Mauna Loa Volcano during clear weather day (left) and on d...
Views of Mauna Loa Volcano during clear weather day and on day when...
Views of Mauna Loa Volcano during clear weather day and on day when...
Views of Mauna Loa Volcano during clear weather day and on day when...

These views of Mauna Loa are from near the Hawaiian Volcano Observatory looking toward the west. The view on left is typical during strong trade winds that blow the plume from Halema‘uma‘u Crater southwest of the summit area. The view on right is common during slack winds that allow vog conditions to develop in the summit area of Kīlauea.

These views of Mauna Loa are from near the Hawaiian Volcano Observatory looking toward the west. The view on left is typical during strong trade winds that blow the plume from Halema‘uma‘u Crater southwest of the summit area. The view on right is common during slack winds that allow vog conditions to develop in the summit area of Kīlauea.

 Department of Interior UAS pilots
UAS pilots at Kilauea
UAS pilots at Kilauea
UAS pilots at Kilauea

Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb

Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb

Map showing the locations of all U.S. volcanoes
Map of volcano threat category designated by color
Map of volcano threat category designated by color
Map of volcano threat category designated by color

Map showing the locations of all U.S. volcanoes with their threat category designated by color. Very high threat is red, high is orange, moderate is yellow, low is green, and very low is blue. 

Map showing the locations of all U.S. volcanoes with their threat category designated by color. Very high threat is red, high is orange, moderate is yellow, low is green, and very low is blue. 

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