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Volcano Science Center images.

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Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National Park
Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National Park
Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National Park
Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National Park

Pie diagram showing the chloride flux, in kilotons per year (kt/yr), measured in 2022, with percentages for the four major rivers (Madison, Yellowstone, Snake, and Falls rivers) that drain Yellowstone National Park. Figure developed by Baine McCleskey.

Pie diagram showing the chloride flux, in kilotons per year (kt/yr), measured in 2022, with percentages for the four major rivers (Madison, Yellowstone, Snake, and Falls rivers) that drain Yellowstone National Park. Figure developed by Baine McCleskey.

Satellite, airborne, and ground-based images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park
Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park
Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park
Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park

Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park. A, WorldView-3 satellite image from September 2014. B, National Park Service (NPS) aerial photograph from 2017. Images A and B were acquired before the feature went largely dry in late 2019 or 2020. C, WorldView-3 satellite image from June 2020.

Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park. A, WorldView-3 satellite image from September 2014. B, National Park Service (NPS) aerial photograph from 2017. Images A and B were acquired before the feature went largely dry in late 2019 or 2020. C, WorldView-3 satellite image from June 2020.

3D rendering of the shear-wave-speed anomaly below Yellowstone
3D rendering of the shear-wave-speed anomaly below Yellowstone
3D rendering of the shear-wave-speed anomaly below Yellowstone
3D rendering of the shear-wave-speed anomaly below Yellowstone

3D rendering of the shear-wave-speed anomaly (ɗVS) below Yellowstone. Regions of strongly reduced shear-wave speed most likely indicate volumes of partially molten crust. Iso-surfaces (surfaces of constant ɗVS) are shown in increments of 5%.

3D rendering of the shear-wave-speed anomaly (ɗVS) below Yellowstone. Regions of strongly reduced shear-wave speed most likely indicate volumes of partially molten crust. Iso-surfaces (surfaces of constant ɗVS) are shown in increments of 5%.

Seismic data coverage of the Yellowstone region and example of seismic noise records
Seismic data coverage of the Yellowstone region and example of seismic noise records
Seismic data coverage of the Yellowstone region and example of seismic noise records
Seismic data coverage of the Yellowstone region and example of seismic noise records

Seismic data coverage of the Yellowstone region and example of seismic noise records. By cross-correlating signals of the background noise recorded at two seismic stations and stacking the signals over many days, useful seismic waveforms can be extracted.

Seismic data coverage of the Yellowstone region and example of seismic noise records. By cross-correlating signals of the background noise recorded at two seismic stations and stacking the signals over many days, useful seismic waveforms can be extracted.

Seismicity in the Yellowstone region during 2022
Seismicity in the Yellowstone region during 2022
Seismicity in the Yellowstone region during 2022
Seismicity in the Yellowstone region during 2022

Map of seismicity (red circles) in the Yellowstone region during 2022. Gray lines are roads, black dashed line shows the caldera boundary, Yellowstone National Park is outlined by black dot-dashed line, and gray dashed lines denote state boundaries.

Map of seismicity (red circles) in the Yellowstone region during 2022. Gray lines are roads, black dashed line shows the caldera boundary, Yellowstone National Park is outlined by black dot-dashed line, and gray dashed lines denote state boundaries.

glowing red and orange lava flows moving down a dark slope with orange and red clouds in the sky.
Mauna Loa eruption from the Northeast Rift Zone sends lava flows to the north downslope toward Saddle Road. As of 6am local time, flows were 6 miles from Saddle Road.
Mauna Loa eruption from the Northeast Rift Zone sends lava flows to the north downslope toward Saddle Road. As of 6am local time, flows were 6 miles from Saddle Road.
Mauna Loa eruption from the Northeast Rift Zone sends lava flows to the north downslope toward Saddle Road. As of 6am local time, flows were 6 miles from Saddle Road.

Photograph taken from Saddle Road at 6AM Hawaii time on November 29, 2022 shows lava flows moving northeast downslope of Mauna Loa volcano from the Northeast Rift Zone eruption.

glowing red and orange lava flows moving down a dark slope with orange and red clouds in the sky.
Mauna Loa eruption from the Northeast Rift Zone sends lava flows to the north downslope. As of 6am local time, flows were 6 miles from Saddle Road.
Mauna Loa eruption from the Northeast Rift Zone sends lava flows to the north downslope. As of 6am local time, flows were 6 miles from Saddle Road.
Mauna Loa eruption from the Northeast Rift Zone sends lava flows to the north downslope. As of 6am local time, flows were 6 miles from Saddle Road.

Photograph taken from Saddle Road at 6AM Hawaii time on November 29, 2022 shows lava flows moving northeast downslope of Mauna Loa volcano from the Northeast Rift Zone eruption.

Google Earth image of the north part of Lower Geyser Basin, Yellowstone National Park, showing the site of the Fountain Hotel
Google Earth image of the north part of Lower Geyser Basin, Yellowstone National Park, showing the site of the Fountain Hotel
Google Earth image of the north part of Lower Geyser Basin, Yellowstone National Park, showing the site of the Fountain Hotel
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National Park
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National Park
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National Park
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National Park

Graph showing the discharge (blue) and specific conductance (black) measured at the Gardner River monitoring station in Yellowstone National Park during the June 10–13, 2022, flood.

Map of southern Idaho and the Snake River Plain
Map of southern Idaho and the Snake River Plain
Map of southern Idaho and the Snake River Plain
Map of southern Idaho and the Snake River Plain

Map of southern Idaho and the Snake River Plain, showing the eastern (ESRP) and western (WSRP) parts of the geologic province. Map by Zach Lifton, Idaho Geological Survey.

Map of southern Idaho and the Snake River Plain, showing the eastern (ESRP) and western (WSRP) parts of the geologic province. Map by Zach Lifton, Idaho Geological Survey.

Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage Sites

Document certifying The Yellowstone Volcanic and Hydrothermal System, USA, as one of the first 100 IUGS Geological Heritage Sites as declared during the 60th anniversary IUGS meeting held in Zumaia, Spain in October 2022.

Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites

Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites during the 60th anniversary IUGS meeting in Zumaia, Spain in October, 2022.  Photo by Marjorie Chan.

A USGS scientists collects a sample from the surface of a dark-colored rock using a hammer and chisel
USGS scientist collects a sample from a basalt lava flow for cosmogenic surface exposure dating
USGS scientist collects a sample from a basalt lava flow for cosmogenic surface exposure dating
USGS scientist collects a sample from a basalt lava flow for cosmogenic surface exposure dating

A USGS scientists uses a hammer and chisel to collect a sample from the surface of a basalt boulder in the San Francisco Volcanic Field of northern Arizona.  The age of the sample will be determined using a technique called cosmogenic surface exposure dating, which determines how long the rock has been exposed to cosmic rays at the surface of the Earth.

A USGS scientists uses a hammer and chisel to collect a sample from the surface of a basalt boulder in the San Francisco Volcanic Field of northern Arizona.  The age of the sample will be determined using a technique called cosmogenic surface exposure dating, which determines how long the rock has been exposed to cosmic rays at the surface of the Earth.

Yellowstone interferogram from Sentinel-1 spanning September 29, 2021, to October 6, 2022
Yellowstone interferogram from Sentinel-1 spanning September 29, 2021, to October 6, 2022
Yellowstone interferogram from Sentinel-1 spanning September 29, 2021, to October 6, 2022
Yellowstone interferogram from Sentinel-1 spanning September 29, 2021, to October 6, 2022

Interferogram created from data collected on September 29, 2021, and October 6, 2022, by the Sentinel-1 satellite system. Colored fringes indicate a change in distance (called range change) between the satellite and ground surface that is caused by surface deformation.

Interferogram created from data collected on September 29, 2021, and October 6, 2022, by the Sentinel-1 satellite system. Colored fringes indicate a change in distance (called range change) between the satellite and ground surface that is caused by surface deformation.

Atmospheric water vapor and river level during June 2022 in the NE part of Yellowstone National Park
Atmospheric water vapor and river level during June 2022 in the NE part of Yellowstone National Park
Atmospheric water vapor and river level during June 2022 in the NE part of Yellowstone National Park
Atmospheric water vapor and river level during June 2022 in the NE part of Yellowstone National Park

Atmospheric water vapor and river level measured during June 2022 in the northeast part of Yellowstone National Park. Gray line is the level of the Lamar River. Blue line is the amount of water vapor in the atmosphere above GPS station P720.

Barren ground with some equipment and solar panels in front of steaming pools.  Grassy meadow and forested area behind.
Multi-GAS station installed in the Mud Volcano area of Yellowstone National Park
Multi-GAS station installed in the Mud Volcano area of Yellowstone National Park
Multi-GAS station installed in the Mud Volcano area of Yellowstone National Park

Multi-GAS station installed in the Mud Volcano area of Yellowstone National Park under permit YELL-2022-SCI-7082.  The station was situated on stable, cool ground away from the edge of thermal features to ensure no impact to the features.

Multi-GAS station installed in the Mud Volcano area of Yellowstone National Park under permit YELL-2022-SCI-7082.  The station was situated on stable, cool ground away from the edge of thermal features to ensure no impact to the features.

Cutbank exposure near West DuNoir Creek, Wyoming, illustrates the differences between bedrock and surficial geologic mapping
Cutbank exposure near West DuNoir Creek, Wyoming
Cutbank exposure near West DuNoir Creek, Wyoming
Cutbank exposure near West DuNoir Creek, Wyoming

A cutbank exposure near West DuNoir Creek, Wyoming, illustrates the differences between bedrock and surficial geologic mapping. On bedrock maps this location is mapped as the Eocene (55–34 million years old) Indian Meadows Formation, which corresponds to the bedrock visible in the stream bed.

A cutbank exposure near West DuNoir Creek, Wyoming, illustrates the differences between bedrock and surficial geologic mapping. On bedrock maps this location is mapped as the Eocene (55–34 million years old) Indian Meadows Formation, which corresponds to the bedrock visible in the stream bed.

Photo of a newly eroded cliff along the Gardner River, Yellowstone National Park
Photo of a newly eroded cliff along the Gardner River, Yellowstone National Park
Photo of a newly eroded cliff along the Gardner River, Yellowstone National Park
Photo of a newly eroded cliff along the Gardner River, Yellowstone National Park

Photo of a newly eroded cliff along the Gardner River, Yellowstone National Park, showing the unconsolidated layers of sandstone and gravel. USGS photo by David Roth, September 5, 2022.

Sediment cores from Twin Butte Lake, Yellowstone National Park, being analyzed in the laboratory
Sediment cores from Twin Butte Lake, Yellowstone National Park, being analyzed in the laboratory
Sediment cores from Twin Butte Lake, Yellowstone National Park, being analyzed in the laboratory
Sediment cores from Twin Butte Lake, Yellowstone National Park, being analyzed in the laboratory

Sediment cores from Twin Butte Lake, Yellowstone National Park, being analyzed in the laboratory.  (a) Photo of a freshly split core that exhibits a transition in lake productivity (grey sediment on bottom to dark organic rich sediment on top). One half of the core is scanned for multiple types of data and sampled while the other half of the core is archived.

Sediment cores from Twin Butte Lake, Yellowstone National Park, being analyzed in the laboratory.  (a) Photo of a freshly split core that exhibits a transition in lake productivity (grey sediment on bottom to dark organic rich sediment on top). One half of the core is scanned for multiple types of data and sampled while the other half of the core is archived.

Two people standing in a shallow trench a few feet wide and deep in a forested landscape. They are examining the trench wall
Geologists examining a paleoseismic trench across the Sawtooth fault, Idaho
Geologists examining a paleoseismic trench across the Sawtooth fault, Idaho
Geologists examining a paleoseismic trench across the Sawtooth fault, Idaho

Photograph of geologists examining a paleoseismic trench across the Sawtooth fault, Idaho. Trenches like this provide geologists an opportunity to date sediments that were offset by past earthquakes, thus determining the rupture history of the fault. Photo by Zach Lifton, Idaho Geological Survey, September 2022.

Photograph of geologists examining a paleoseismic trench across the Sawtooth fault, Idaho. Trenches like this provide geologists an opportunity to date sediments that were offset by past earthquakes, thus determining the rupture history of the fault. Photo by Zach Lifton, Idaho Geological Survey, September 2022.

Method of rapidly cooling an experiment that involves molten rock
Method of rapidly cooling an experiment that involves molten rock
Method of rapidly cooling an experiment that involves molten rock
Method of rapidly cooling an experiment that involves molten rock

One method of rapidly cooling an experiment that involves molten rock. The volcanic material is dropped from inside the furnace (at ~1000 °C or 1830 °F!) down a vertical tube and into a bulb of room-temperature water.

One method of rapidly cooling an experiment that involves molten rock. The volcanic material is dropped from inside the furnace (at ~1000 °C or 1830 °F!) down a vertical tube and into a bulb of room-temperature water.

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