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Volcano Hazard Program images.

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Angular unconformity atop Mount Everts, Yellowstone National Park
Angular unconformity atop Mount Everts, Yellowstone National Park
Angular unconformity atop Mount Everts, Yellowstone National Park
Angular unconformity atop Mount Everts, Yellowstone National Park

An unconformity at the top of Mount Everts is located where the Huckleberry Ridge Tuff, 2.1 million years old, lies directly on top of Cretaceous sediments that are ~60 million years old and greater.  Right at the unconformity are conspicuous orange and black colors.  The orange is oxidation of the sedimentary unit where it is in contact with the ash, whic

An unconformity at the top of Mount Everts is located where the Huckleberry Ridge Tuff, 2.1 million years old, lies directly on top of Cretaceous sediments that are ~60 million years old and greater.  Right at the unconformity are conspicuous orange and black colors.  The orange is oxidation of the sedimentary unit where it is in contact with the ash, whic

Silver Gate landslide complex in Yellowstone National Park
Silver Gate landslide complex in Yellowstone National Park
Silver Gate landslide complex in Yellowstone National Park
Silver Gate landslide complex in Yellowstone National Park

Silver Gate landslide complex in Yellowstone National Park. The jumbled nature of the calcium-carbonate rocks is evidence that the deposit was formed by collapse of a travertine hot-spring terrace that might once have looked like Mammoth Hot Springs does today.

Silver Gate landslide complex in Yellowstone National Park. The jumbled nature of the calcium-carbonate rocks is evidence that the deposit was formed by collapse of a travertine hot-spring terrace that might once have looked like Mammoth Hot Springs does today.

Highway 89 winding through Silver Gate in Yellowstone National Park
Highway 89 winding through Silver Gate in Yellowstone National Park
Highway 89 winding through Silver Gate in Yellowstone National Park
Highway 89 winding through Silver Gate in Yellowstone National Park

A few miles south of Mammoth Hot Springs in Yellowstone National Park, Highway 89 winds through the white/gray jumble of rocks known as the Hoodoos, or Silver Gate, that formed when travertine from Terrace Mountain collapsed in a landslide.

A few miles south of Mammoth Hot Springs in Yellowstone National Park, Highway 89 winds through the white/gray jumble of rocks known as the Hoodoos, or Silver Gate, that formed when travertine from Terrace Mountain collapsed in a landslide.

Geophysicist checks data output at Mount Rainier station
Geophysicist checks data output at Mount Rainier station
Geophysicist checks data output at Mount Rainier station
Geophysicist checks data output at Mount Rainier station

A seismologist with the Cascades Volcano Observatory checks the data output on a newly installed monitoring station at Mount Rainier.

A seismologist with the Cascades Volcano Observatory checks the data output on a newly installed monitoring station at Mount Rainier.

Station PARA at Mount Rainier
Mount Rainier's seismic and infrasound station PARA
Mount Rainier's seismic and infrasound station PARA
Mount Rainier's seismic and infrasound station PARA

Seismic and infrasound station PARA, installed October 6-8, 2020 at Mount Rainier.

Geophysicist takes notes after installing a seismometer at Mount Rainier
A geophysicist notes location of new seismometer at Mount Rainier
A geophysicist notes location of new seismometer at Mount Rainier
A geophysicist notes location of new seismometer at Mount Rainier

A geophysicist from the Cascades Volcano Observatory notes the location of a newly buried seismometer at station PARA, on Mount Rainier.

A geophysicist from the Cascades Volcano Observatory notes the location of a newly buried seismometer at station PARA, on Mount Rainier.

NAGT intern installs an infrasound array at Mount Rainier
NAGT intern installs infrasound sensors at Mount Rainier
NAGT intern installs infrasound sensors at Mount Rainier
NAGT intern installs infrasound sensors at Mount Rainier

NAGT intern Emily Bryant installs one of three infrasound sensors at volcano monitoring station PARA, at Mount Rainier.

NAGT intern Emily Bryant installs one of three infrasound sensors at volcano monitoring station PARA, at Mount Rainier.

4 images showing boxes of equipment with wires being put into the ground in a forest setting.
Scientists installing a lahar monitoring station.
Scientists installing a lahar monitoring station.
Scientists installing a lahar monitoring station.

Lahar monitoring equipment is housed in a secure box with multiple types of instruments to detect approaching lahars.  

Lahar monitoring equipment is housed in a secure box with multiple types of instruments to detect approaching lahars.  

Seismic/GPS station YOCR, at Mount Hood
Seismic/GPS station YOCR, at Mount Hood
Seismic/GPS station YOCR, at Mount Hood
Seismic/GPS station YOCR, at Mount Hood

A Cascades Volcano Observatory field team completes the installation of the combined seismic/GPS station YOCR, at Mount Hood.

A Cascades Volcano Observatory field team completes the installation of the combined seismic/GPS station YOCR, at Mount Hood.

Volcano monitoring station BRSP, on the north flank of Mount Hood
Volcano monitoring station BRSP, on the north flank of Mount Hood
Volcano monitoring station BRSP, on the north flank of Mount Hood
Volcano monitoring station BRSP, on the north flank of Mount Hood

View of the combined seismic/GPS station BRSP, on the north flank of Mount Hood, Oregon. Mount Hood is pictured in the distance.

View of the combined seismic/GPS station BRSP, on the north flank of Mount Hood, Oregon. Mount Hood is pictured in the distance.

Finishing the installation of seismic/GPS station YOCR, at Mount Hood
Finishing the installation of seismic/GPS station YOCR, at Mount Hood
Finishing the installation of seismic/GPS station YOCR, at Mount Hood
Finishing the installation of seismic/GPS station YOCR, at Mount Hood

A USGS Cascades Volcano Observatory field team finishes the installation of the combined seismic/GPS station, YOCR, at Mount Hood, Oregon.

A USGS Cascades Volcano Observatory field team finishes the installation of the combined seismic/GPS station, YOCR, at Mount Hood, Oregon.

Combined seismic/GPS station LSON on Mount Hood
Combined seismic/GPS station LSON on Mount Hood
Combined seismic/GPS station LSON on Mount Hood
Combined seismic/GPS station LSON on Mount Hood

Combined seismic/GPS station LSON, on Mount Hood, installed at the end of September 2020. LSON is one of three new stations that enhance the existing monitoring network at this high-threat volcano.

Combined seismic/GPS station LSON, on Mount Hood, installed at the end of September 2020. LSON is one of three new stations that enhance the existing monitoring network at this high-threat volcano.

GPS mast installed at station LSON, on Mount Hood
CVO geophysicist installs a GPS mast at station LSON, Mount Hood
CVO geophysicist installs a GPS mast at station LSON, Mount Hood
CVO geophysicist installs a GPS mast at station LSON, Mount Hood

USGS Cascades Volcano Observatory Geophysicist Rebecca Kramer works on the installation of the GPS mast at new station LSON, at Mount Hood. The GPS measures subtle ground deformation that can occur in response to magma entering or leaving the magma reservoir several miles below the summit.

USGS Cascades Volcano Observatory Geophysicist Rebecca Kramer works on the installation of the GPS mast at new station LSON, at Mount Hood. The GPS measures subtle ground deformation that can occur in response to magma entering or leaving the magma reservoir several miles below the summit.

Color photograph of two scientists sampling a volcanic fumarole
HVO gas scientists collected helium samples
HVO gas scientists collected helium samples
HVO gas scientists collected helium samples

As part of routine monitoring efforts, HVO gas scientists collected helium samples from fumaroles in the Sulphur Banks, or Ha‘akulamanu, area of Hawai‘i Volcanoes National Park on September 30, 2020. Helium can pass through the glass of typical gas sampling bottles, so copper tubing is necessary for the specialized sample.

As part of routine monitoring efforts, HVO gas scientists collected helium samples from fumaroles in the Sulphur Banks, or Ha‘akulamanu, area of Hawai‘i Volcanoes National Park on September 30, 2020. Helium can pass through the glass of typical gas sampling bottles, so copper tubing is necessary for the specialized sample.

Color photograph of native sulfur crystals
Crystals of pure native sulfur at sites of degassing called fumaroles
Crystals of pure native sulfur at sites of degassing called fumaroles
Crystals of pure native sulfur at sites of degassing called fumaroles

Different sulfur gases, including sulfur dioxide (SO2) and hydrogen sulfide (H2S), can react with each other to deposit crystals of pure native sulfur at sites of degassing called fumaroles. The crystals picture here formed within a Sulphur Banks area fumarole in Hawai‘i Volcanoes National Park. USGS photo by T. Elias.

Different sulfur gases, including sulfur dioxide (SO2) and hydrogen sulfide (H2S), can react with each other to deposit crystals of pure native sulfur at sites of degassing called fumaroles. The crystals picture here formed within a Sulphur Banks area fumarole in Hawai‘i Volcanoes National Park. USGS photo by T. Elias.

Color photograph of yellow native sulfur crystals
Close-up image of native sulfur crystals
Close-up image of native sulfur crystals
Close-up image of native sulfur crystals

A close-up image of native sulfur crystals that formed within fumaroles at the Sulphur Banks in Hawai‘i Volcanoes National Park. In addition to sulfur species and other gases, volcanoes emit water vapor. Here, some of the vapor has condensed to liquid water and formed droplets visible on the sulfur crystals. USGS photo by P. Nadeau. 

A close-up image of native sulfur crystals that formed within fumaroles at the Sulphur Banks in Hawai‘i Volcanoes National Park. In addition to sulfur species and other gases, volcanoes emit water vapor. Here, some of the vapor has condensed to liquid water and formed droplets visible on the sulfur crystals. USGS photo by P. Nadeau. 

Photograph of tubing inserted into a fumarole
Tubing inserted into a fumarole
Tubing inserted into a fumarole
Tubing inserted into a fumarole

Tubing inserted into a fumarole at the Sulphur Banks in Hawai‘i Volcanoes National Park allows HVO gas scientists to sample gas. The gas travels through the tube into gas sampling bottles for later analyses. USGS photo by M. Warren.

Tubing inserted into a fumarole at the Sulphur Banks in Hawai‘i Volcanoes National Park allows HVO gas scientists to sample gas. The gas travels through the tube into gas sampling bottles for later analyses. USGS photo by M. Warren.

Installation of GPS mast at station BRSP on Mount Hood
Installation of GPS mast at station BRSP on Mount Hood
Installation of GPS mast at station BRSP on Mount Hood
Installation of GPS mast at station BRSP on Mount Hood

USGS Cascades Volcano Observatory Geophysicist Emily Montgomery-Brown uses a drill to create a small hole in volcanic rock that will support a GPS mast. The effort was part of a three-station installation project at Mount Hood in 2020. This station location is called BRSP.

USGS Cascades Volcano Observatory Geophysicist Emily Montgomery-Brown uses a drill to create a small hole in volcanic rock that will support a GPS mast. The effort was part of a three-station installation project at Mount Hood in 2020. This station location is called BRSP.

Installing a seismometer at station BRSP on Mount Hood
Installing a seismometer at station BRSP on Mount Hood
Installing a seismometer at station BRSP on Mount Hood
Installing a seismometer at station BRSP on Mount Hood

Volcano Disaster Assistance Program Geophysicist Jeremy Pesicek digs a hole for a seismometer at station BRSP, on the north flank of Mount Hood. The seismometer, which detects earthquakes, is buried at a depth of at least 1 meter (3 feet).

Volcano Disaster Assistance Program Geophysicist Jeremy Pesicek digs a hole for a seismometer at station BRSP, on the north flank of Mount Hood. The seismometer, which detects earthquakes, is buried at a depth of at least 1 meter (3 feet).

New seismic/GPS station (LSON) installed at Mount Hood
New seismic/GPS station (LSON) installed at Mount Hood
New seismic/GPS station (LSON) installed at Mount Hood
New seismic/GPS station (LSON) installed at Mount Hood

USGS Cascades Volcano Observatory Geophysicist Wes Thelen, removes ropes from new station LSON, at Mount Hood (Mount Hood is pictured in the distance).

USGS Cascades Volcano Observatory Geophysicist Wes Thelen, removes ropes from new station LSON, at Mount Hood (Mount Hood is pictured in the distance).

Helicopter delivers equipment to station BRSP on Mount Hood
Helicopter delivers equipment to station BRSP on Mount Hood
Helicopter delivers equipment to station BRSP on Mount Hood
Helicopter delivers equipment to station BRSP on Mount Hood

A USGS Cascades Volcano Observatory field team waits on this remote north flank of Mount Hood, as a helicopter delivers supplies and equipment to station BRSP. The station was installed with minimal impact on the environment. A helicopter delivered equipment via external sling load and USGS personnel accessed the site by foot.

A USGS Cascades Volcano Observatory field team waits on this remote north flank of Mount Hood, as a helicopter delivers supplies and equipment to station BRSP. The station was installed with minimal impact on the environment. A helicopter delivered equipment via external sling load and USGS personnel accessed the site by foot.