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Volcano Hazard Program images.

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HVO scientists inspect a seismic station on Mauna Loa to evaluate for a possible
HVO scientists inspect a seismic station on Mauna Loa to evaluate for a possible
HVO scientists inspect a seismic station on Mauna Loa to evaluate for a possible

HVO scientists inspect a seismic station on Mauna Loa to evaluate for a possible equipment upgrade in the near future.

HVO scientists inspect a seismic station on Mauna Loa to evaluate for a possible equipment upgrade in the near future.

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MultiGAS instruments monitor volcanic gases at the summit
MultiGAS instruments monitor volcanic gases at the summit
MultiGAS instruments monitor volcanic gases at the summit

Hawaiian Volcano Observatory field crews establish a new MultiGAS volcanic gas monitoring station on the south side of Kīlauea Volcano's caldera. Currently, sulfur dioxide emission rates from the summit remain low. The station will collect data to track emission rates and concentrations over time. Photo by Frank Younger.

Hawaiian Volcano Observatory field crews establish a new MultiGAS volcanic gas monitoring station on the south side of Kīlauea Volcano's caldera. Currently, sulfur dioxide emission rates from the summit remain low. The station will collect data to track emission rates and concentrations over time. Photo by Frank Younger.

large crater with volcanic gas rising from yellow spots in crater wall.
Kilauea summit crater after collapse in 2018
Kilauea summit crater after collapse in 2018
Kilauea summit crater after collapse in 2018

This is a view of the summit area from the southwest, showing the collapsed area of Halema‘uma‘u and the adjacent caldera floor. A section of Crater Rim Drive preserved on a down-dropped block is visible at the far right.

This is a view of the summit area from the southwest, showing the collapsed area of Halema‘uma‘u and the adjacent caldera floor. A section of Crater Rim Drive preserved on a down-dropped block is visible at the far right.

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HVO scientists check out monitoring instruments on Mauna Loa
HVO scientists check out monitoring instruments on Mauna Loa
HVO scientists check out monitoring instruments on Mauna Loa

HVO scientists measure a GPS instrument to ensure its stability during a multi-day deployment in the Kahuku Unit of Hawai‘i Volcanoes National Park.

HVO scientists measure a GPS instrument to ensure its stability during a multi-day deployment in the Kahuku Unit of Hawai‘i Volcanoes National Park.

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What caused—or did not cause—the 2018 Kīlauea eruption?
What caused—or did not cause—the 2018 Kīlauea eruption?
What caused—or did not cause—the 2018 Kīlauea eruption?

Earthquakes (red dots) track the progression of the magmatic intrusion from Kīlauea Volcano's middle East Rift Zone to the lower East Rift Zone between April 30 and May 3, 2018. Orange triangles show the locations of fissure 1 (right), which erupted on May 3, and Pu‘u ‘Ō‘ō (left).

Earthquakes (red dots) track the progression of the magmatic intrusion from Kīlauea Volcano's middle East Rift Zone to the lower East Rift Zone between April 30 and May 3, 2018. Orange triangles show the locations of fissure 1 (right), which erupted on May 3, and Pu‘u ‘Ō‘ō (left).

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Maps displaying the stages of evolution of the more recent cycle of volcanism as
Maps displaying the stages of evolution of the more recent cycle of volcanism as
Maps displaying the stages of evolution of the more recent cycle of volcanism as

Maps displaying the stages of evolution of the more recent cycle of volcanism associated with Yellowstone Caldera. From Finn and Morgan, 2002 (High-resolution aeromagnetic mapping of volcanic terrain, Yellowstone National Park).

Maps displaying the stages of evolution of the more recent cycle of volcanism associated with Yellowstone Caldera. From Finn and Morgan, 2002 (High-resolution aeromagnetic mapping of volcanic terrain, Yellowstone National Park).

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Color-shaded topographic relief map of the Yellowstone Plateau-Snake River Plain
Color-shaded topographic relief map of the Yellowstone Plateau-Snake River Plain
Color-shaded topographic relief map of the Yellowstone Plateau-Snake River Plain

Color-shaded topographic relief map of the Yellowstone Plateau-Snake River Plain volcanic province showing the track of the Yellowstone hot spot. Figure by Ken Pierce and Lisa Morgan.

Color-shaded topographic relief map of the Yellowstone Plateau-Snake River Plain volcanic province showing the track of the Yellowstone hot spot. Figure by Ken Pierce and Lisa Morgan.

Landscape photo of mountains in distance with low clouds filling valley in mid-ground and pine tress on slope in foreground
Sunrise at Mount St. Helens
Sunrise at Mount St. Helens
Sunrise at Mount St. Helens

The sun rises at Mount St. Helens (pictured in the distance), with low-level clouds covering Coldwater Lake. The view is from the Coldwater Science and Learning Center, the site of the 2018 GeoGirls field camp program.

The sun rises at Mount St. Helens (pictured in the distance), with low-level clouds covering Coldwater Lake. The view is from the Coldwater Science and Learning Center, the site of the 2018 GeoGirls field camp program.

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Thermal map of Kīlauea Caldera
Thermal map of Kīlauea Caldera
Thermal map of Kīlauea Caldera

This thermal map was constructed by merging about 1300 images from a morning helicopter overflight, and shows the distribution of some of the prominent thermal features in the caldera. The most conspicuous area is a region of high temperatures in the deepest part of the collapse depression, in the area of Halema‘uma‘u.

This thermal map was constructed by merging about 1300 images from a morning helicopter overflight, and shows the distribution of some of the prominent thermal features in the caldera. The most conspicuous area is a region of high temperatures in the deepest part of the collapse depression, in the area of Halema‘uma‘u.

View of a clear blue hot spring pool of alkaline chloride fluid with silica sinter apron around it at Biscuit Basin.
View of a clear blue hot spring pool of alkaline chloride fluid
View of a clear blue hot spring pool of alkaline chloride fluid
View of a clear blue hot spring pool of alkaline chloride fluid

View of a clear blue hot spring pool of alkaline chloride fluid with silica sinter apron around it at Biscuit Basin.  This pool is generally close to the boiling temperature (200℉, 93℃) at this altitude (7200 ft, 2195 m).

View of a clear blue hot spring pool of alkaline chloride fluid with silica sinter apron around it at Biscuit Basin.  This pool is generally close to the boiling temperature (200℉, 93℃) at this altitude (7200 ft, 2195 m).

Alkaline-chloride waters from Old Faithful flow over the edge of the white silica sinter terrace into the Firehole River
Alkaline-chloride waters from Old Faithful
Alkaline-chloride waters from Old Faithful
Alkaline-chloride waters from Old Faithful

Alkaline-chloride waters from an eruption of Old Faithful flow over the edge of the white silica sinter terrace into the Firehole River.  The orange coloration on the sinter terrace is due to thermophilic (high temperature) bacteria living in the warm fluids.  Old Faithful Inn is in the background, with the wooded Summit Lake rhyolitic lava flow behind.&nb

Alkaline-chloride waters from an eruption of Old Faithful flow over the edge of the white silica sinter terrace into the Firehole River.  The orange coloration on the sinter terrace is due to thermophilic (high temperature) bacteria living in the warm fluids.  Old Faithful Inn is in the background, with the wooded Summit Lake rhyolitic lava flow behind.&nb

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Eruption pause provides an opportunity to probe volcanic pollution
Eruption pause provides an opportunity to probe volcanic pollution
Eruption pause provides an opportunity to probe volcanic pollution

Only small amounts of sulfur dioxide (SO2) and hydrogen sulfide (H2S) are currently being released from Kīlauea, but they chemically react with each other (oxidation-reduction reaction) to form the bright yellow sulfur deposits visible on the crater walls within Halema‘uma‘u.

Only small amounts of sulfur dioxide (SO2) and hydrogen sulfide (H2S) are currently being released from Kīlauea, but they chemically react with each other (oxidation-reduction reaction) to form the bright yellow sulfur deposits visible on the crater walls within Halema‘uma‘u.

Laboratory computers and equipment.
Argon geochronology lab in Menlo Park, California.
Argon geochronology lab in Menlo Park, California.
Argon geochronology lab in Menlo Park, California.

Argon geochronology lab in Menlo Park, California.

Microprobe and computer in a laboratory.
Microprobe laboratory in Menlo Park, California.
Microprobe laboratory in Menlo Park, California.
Microprobe laboratory in Menlo Park, California.

Microprobe laboratory in Menlo Park, California.

USGS Hawaiian Volcano Observatory staff, September 2018.
USGS Hawaiian Volcano Observatory staff, September 2018.
USGS Hawaiian Volcano Observatory staff, September 2018.
USGS Hawaiian Volcano Observatory staff, September 2018.

USGS Hawaiian Volcano Observatory staff, September 2018.

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A scientist takes a gravity reading at a station located on the down-dropped blo
A scientist takes a gravity reading at a station located on the down-dropped blo
A scientist takes a gravity reading at a station located on the down-dropped blo

A scientist takes a gravity reading at a station located on the down-dropped block of Kīlauea caldera, which subsided as an intact structure, while a second gravity instrument (foreground) records data. Many of the preexisting gravity stations, which have been measured for years, survived Kīlauea's 2018 summit collapse.

A scientist takes a gravity reading at a station located on the down-dropped block of Kīlauea caldera, which subsided as an intact structure, while a second gravity instrument (foreground) records data. Many of the preexisting gravity stations, which have been measured for years, survived Kīlauea's 2018 summit collapse.

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New outcrops make good geology
New outcrops make good geology
New outcrops make good geology

This aerial view of the western part of Kīlauea Volcano's caldera was taken on August 6, 2018. The down-dropped block is faulted about 120 m (400 feet) below the caldera floor. Many 19th-century lava flows are exposed in the fault scarps. Halema‘uma‘u (not visible) is to the left of this photo. USGS photo by D.Swanson.

This aerial view of the western part of Kīlauea Volcano's caldera was taken on August 6, 2018. The down-dropped block is faulted about 120 m (400 feet) below the caldera floor. Many 19th-century lava flows are exposed in the fault scarps. Halema‘uma‘u (not visible) is to the left of this photo. USGS photo by D.Swanson.

Upper Geyser Basin boardwalk, Yellowstone
Ear Spring, Yellowstone National Park
Ear Spring, Yellowstone National Park
Ear Spring, Yellowstone National Park

New thermal feature beneath the boardwalk on Geyser Hill, Upper Geyser Basin. Boards removed for better observation. Pump Geyser is mound at end of boardwalk. Old Faithful Inn in distance.

New thermal feature beneath the boardwalk on Geyser Hill, Upper Geyser Basin. Boards removed for better observation. Pump Geyser is mound at end of boardwalk. Old Faithful Inn in distance.

Thermal feature along Ferris Fork near Bechler River, Yellowstone
Thermal feature along Ferris Fork near Bechler River, Yellowstone
Thermal feature along Ferris Fork near Bechler River, Yellowstone
Thermal feature along Ferris Fork near Bechler River, Yellowstone

An unnamed but charismatic thermal feature alongside Ferris Fork, near the Bechler River. The center of the pool is roiling with gas bubbles, but not boiling! The pool is only about 180 degrees F (81 degrees C), and all the gas is bubbling up from underground.

An unnamed but charismatic thermal feature alongside Ferris Fork, near the Bechler River. The center of the pool is roiling with gas bubbles, but not boiling! The pool is only about 180 degrees F (81 degrees C), and all the gas is bubbling up from underground.

Mules loaded with equipment, Yellowstone
Mules loaded with sampling equipment and supplies, Yellowstone
Mules loaded with sampling equipment and supplies, Yellowstone
Mules loaded with sampling equipment and supplies, Yellowstone

Mules loaded with sampling equipment and supplies for a mission to collect gas and thermal water samples from the Bechler River area in the southwest part of Yellowstone National Park. 

Mules loaded with sampling equipment and supplies for a mission to collect gas and thermal water samples from the Bechler River area in the southwest part of Yellowstone National Park. 

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Following the draining of magma from Pu‘u ‘Ō‘ō on Ap
Following the draining of magma from Pu‘u ‘Ō‘ō on Ap
Following the draining of magma from Pu‘u ‘Ō‘ō on Ap

Following the draining of magma from Pu‘u ‘Ō‘ō on April 30, 2018, the crater was roughly 356 meters (1168 feet) deep. The upper part of the crater was flaring, with the deepest portion a narrower cylindrical shaft.

Following the draining of magma from Pu‘u ‘Ō‘ō on April 30, 2018, the crater was roughly 356 meters (1168 feet) deep. The upper part of the crater was flaring, with the deepest portion a narrower cylindrical shaft.