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Earthquakes located at Mount St. Helens from 2008-2024, a non-eruptive period.
Earthquakes located at Mount St. Helens from 2008-2024, a non-eruptive period.
Earthquakes located at Mount St. Helens from 2008-2024, a non-eruptive period.
Earthquakes located at Mount St. Helens from 2008-2024, a non-eruptive period.

Earthquakes located at Mount St. Helens from 2008-2024, a non-eruptive period. This activity is consistent with normal, background levels. Top: Earthquake events located per week. The orange color at the far right denotes earthquakes from February to June 2024. Bottom: Earthquake depths below sea level (bsl) in kilometers.

Earthquakes located at Mount St. Helens from 2008-2024, a non-eruptive period. This activity is consistent with normal, background levels. Top: Earthquake events located per week. The orange color at the far right denotes earthquakes from February to June 2024. Bottom: Earthquake depths below sea level (bsl) in kilometers.

Mount St Helens with a dusting of snow looking south in June 2024
Aerial photo of Mount St. Helens June 2024
Aerial photo of Mount St. Helens June 2024
Aerial photo of Mount St. Helens June 2024

Aerial photo of Mount St. Helens (center), with Mount Hood (in the distance, far left), Spirit Lake (on left with floating log mat), and St. Helens Lake with a little ice cover (lower left). USGS image taken by K. Spicer on June 6, 2024. 

Aerial photo of Mount St. Helens (center), with Mount Hood (in the distance, far left), Spirit Lake (on left with floating log mat), and St. Helens Lake with a little ice cover (lower left). USGS image taken by K. Spicer on June 6, 2024. 

Animation of annual Yellowstone seismicity 2017-2023
Animation of annual Yellowstone seismicity 2017-2023
Animation of annual Yellowstone seismicity 2017-2023
Animation of annual Yellowstone seismicity 2017-2023

This animation shows a map of of Yellowstone seismicity by year from 2017 through 2023.  Earthquakes are red circles, with the circle size indicating earthquake magnitude.  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.

This animation shows a map of of Yellowstone seismicity by year from 2017 through 2023.  Earthquakes are red circles, with the circle size indicating earthquake magnitude.  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.

Front cover of the Yellowstone Volcano Observatory 2023 annual report
Front cover of the Yellowstone Volcano Observatory 2023 annual report
Front cover of the Yellowstone Volcano Observatory 2023 annual report
Front cover of the Yellowstone Volcano Observatory 2023 annual report

Front cover of the Yellowstone Volcano Observatory 2023 annual report, which includes a summary of earthquake, deformation, and geyser activity, as well as research investigations and other information. The report is freely available online athttps://pubs.usgs.gov/publication/cir1524.

Front cover of the Yellowstone Volcano Observatory 2023 annual report, which includes a summary of earthquake, deformation, and geyser activity, as well as research investigations and other information. The report is freely available online athttps://pubs.usgs.gov/publication/cir1524.

Infographic giving earthquake, deformation, thermal emission, and geyser statistics for the Yellowstone region for the year 2023
Infographic giving earthquake, deformation, thermal emission, and geyser statistics for the Yellowstone region for the year 2023
Infographic giving earthquake, deformation, thermal emission, and geyser statistics for the Yellowstone region for the year 2023
Infographic giving earthquake, deformation, thermal emission, and geyser statistics for the Yellowstone region for the year 2023

Infographic giving earthquake, deformation, thermal emission, and geyser statistics for the Yellowstone region for the year 2023.  The graphic accompanies the Yellowstone Volcano Observatory 2023 annual report, freely available online athttps://pubs.usgs.gov/publication/cir1524.

Site of April 15, 2024, hydrothermal explosion on Porcelain Terrace, Norris Geyser Basin, Yellowstone National Park
Site of April 15, 2024, hydrothermal explosion on Porcelain Terrace, Norris Geyser Basin, Yellowstone National Park
Site of April 15, 2024, hydrothermal explosion on Porcelain Terrace, Norris Geyser Basin, Yellowstone National Park
Site of April 15, 2024, hydrothermal explosion on Porcelain Terrace, Norris Geyser Basin, Yellowstone National Park

Site of April 15, 2024, hydrothermal explosion on Porcelain Terrace, Norris Geyser Basin, Yellowstone National Park.  The small crater and disrupted ground are in silica sinter deposits that formed in the past two years, since water has been flowing from the terrace into Nuphar Lake (off photo to right), and angular fragments of ejecta on top of the sinter are

Site of April 15, 2024, hydrothermal explosion on Porcelain Terrace, Norris Geyser Basin, Yellowstone National Park.  The small crater and disrupted ground are in silica sinter deposits that formed in the past two years, since water has been flowing from the terrace into Nuphar Lake (off photo to right), and angular fragments of ejecta on top of the sinter are

Red, brown, yellow bacterial mats in shallow water. Blue-green steaming hot spring behind. Snow/tree-covered hill in backgrd.
Vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring, Yellowstone National Park
Vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring, Yellowstone National Park
Vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring, Yellowstone National Park

View of the vibrant, multicolored extremophilic bacteria in the outflow from Grand Prismatic Spring at the Midway Geyser Basin, Yellowstone National Park. Photo by Elizabeth Mordensky, May 12, 2024.

Rock outcrops showing rhyolite lava flow textures from Long Valley and Yellowstone calderas
Rhyolite lava flow textures from Long Valley and Yellowstone calderas
Rhyolite lava flow textures from Long Valley and Yellowstone calderas
Rhyolite lava flow textures from Long Valley and Yellowstone calderas

Rhyolite lava flow textures from Long Valley and Yellowstone calderas.  A) Photograph of well-developed spherulites in a lava flow from Long Valley Caldera in Eastern California. This high-silica rhyolite flow is very similar to the Central Plateau Member rhyolites of the Yellowstone Plateau Volcanic Field and exhibits many of the same textures.

Rhyolite lava flow textures from Long Valley and Yellowstone calderas.  A) Photograph of well-developed spherulites in a lava flow from Long Valley Caldera in Eastern California. This high-silica rhyolite flow is very similar to the Central Plateau Member rhyolites of the Yellowstone Plateau Volcanic Field and exhibits many of the same textures.

Total electron content data at three GPS stations in Yellowstone National Park
Total electron content data at three GPS stations in Yellowstone National Park
Total electron content data at three GPS stations in Yellowstone National Park
Total electron content data at three GPS stations in Yellowstone National Park

Total electron content (TEC) data—a measure of activity in the ionosphere—at three GPS stations in Yellowstone. Each line color is a measurement using a different satellite passing overhead. Note how the data are steady until the evening of May 10, 2024, when the signals start to fluctuate wildly due to the arrival of the Coronal Mass Ejection.

Total electron content (TEC) data—a measure of activity in the ionosphere—at three GPS stations in Yellowstone. Each line color is a measurement using a different satellite passing overhead. Note how the data are steady until the evening of May 10, 2024, when the signals start to fluctuate wildly due to the arrival of the Coronal Mass Ejection.

Rock outcrops that show banding in the interior of rhyolite lava flows
Central Plateau Member rhyolite flow structures from the Yellowstone Plateau Volcanic Field
Central Plateau Member rhyolite flow structures from the Yellowstone Plateau Volcanic Field
Central Plateau Member rhyolite flow structures from the Yellowstone Plateau Volcanic Field

Photos of Central Plateau Member rhyolite flow structures from the Yellowstone Plateau Volcanic Field. A) An ogive from a road cut along Firehole Lake Drive. Ogives are pressure ridges that form perpendicular to the direction of flow from the compressive stresses that deform the highly viscous lava as it moves.

Photos of Central Plateau Member rhyolite flow structures from the Yellowstone Plateau Volcanic Field. A) An ogive from a road cut along Firehole Lake Drive. Ogives are pressure ridges that form perpendicular to the direction of flow from the compressive stresses that deform the highly viscous lava as it moves.

Mass spectrometer, used to measure the ration of atoms with different masses, in the USGS laboratory at Moffett Field, California
Mass spectrometer, used to measure the ration of atoms with different masses, in the USGS laboratory at Moffett Field, California
Mass spectrometer, used to measure the ration of atoms with different masses, in the USGS laboratory at Moffett Field, California
Mass spectrometer, used to measure the ration of atoms with different masses, in the USGS laboratory at Moffett Field, California

A mass spectrometer is used to measure the ratio of atoms with different masses—in this case, the different isotopes of argon gas, which can be used to determine the age of a volcanic rock. Left: a side view of a mass spectrometer at the USGS Argon Geochronology Laboratory in Moffett Field, CA. Right: a close-up view of the sample chamber in this mass spectrometer.

Photos of flow breccia in Central Plateau Member rhyolites in Yellowstone National Park
Photos of flow breccia in Central Plateau Member rhyolites in Yellowstone National Park
Photos of flow breccia in Central Plateau Member rhyolites in Yellowstone National Park
Photos of flow breccia in Central Plateau Member rhyolites in Yellowstone National Park

Photos of flow breccia in Central Plateau Member rhyolites in Yellowstone National Park. A) Flow breccia observed in a drill core from the Lower Geyser Basin. The angular, light-colored clasts are fragments of the original lava carapace, broken and incorporated into the flow as it advanced. B) Flow breccia exposed in a road cut along Firehole Canyon Drive.

Photos of flow breccia in Central Plateau Member rhyolites in Yellowstone National Park. A) Flow breccia observed in a drill core from the Lower Geyser Basin. The angular, light-colored clasts are fragments of the original lava carapace, broken and incorporated into the flow as it advanced. B) Flow breccia exposed in a road cut along Firehole Canyon Drive.

Microscopic view of different groundmass textures in rocks
Microscopic view of different groundmass textures in rocks
Microscopic view of different groundmass textures in rocks
Microscopic view of different groundmass textures in rocks

Microscopic view of different groundmass textures in rocks. On the left, this groundmass is a good choice for argon dating, as it consists of abundant interconnected crystals. On the right, the groundmass consists predominantly of glass (black because it does not transmit cross-polarized light) and is a poor choice for argon dating.

Microscopic view of different groundmass textures in rocks. On the left, this groundmass is a good choice for argon dating, as it consists of abundant interconnected crystals. On the right, the groundmass consists predominantly of glass (black because it does not transmit cross-polarized light) and is a poor choice for argon dating.

SHaded relief map of central Idaho showing fault strands associated with the Sawtooth Fault
Map of the Sawtooth fault, Idaho
Map of the Sawtooth fault, Idaho
Map of the Sawtooth fault, Idaho

Map of the Sawtooth fault, Idaho, based on new lidar topographic maps. Map by Zach Lifton, Idaho Geological Survey, 2024.

Map of the Sawtooth fault, Idaho, based on new lidar topographic maps. Map by Zach Lifton, Idaho Geological Survey, 2024.

Seismic and infrasound data for the April 15, 2024, hydrothermal explosion on Porcelain Terrace at Norris Geyser Basin
Seismic and infrasound data for the April 15, 2024, hydrothermal explosion on Porcelain Terrace at Norris Geyser Basin
Seismic and infrasound data for the April 15, 2024, hydrothermal explosion on Porcelain Terrace at Norris Geyser Basin
Seismic and infrasound data for the April 15, 2024, hydrothermal explosion on Porcelain Terrace at Norris Geyser Basin

Seismic and infrasound data for the April 15, 2024, hydrothermal explosion on Porcelain Terrace at Norris Geyser Basin.  Top plot is seismic data from the YNM station, located at the Norris Geyser Basin Museum.  Middle plot is seismic data from station YNB, in the Ragged Hills of Norris Geyser Basin. Bottom plot is infrasound data from station YNB.&nb

Seismic and infrasound data for the April 15, 2024, hydrothermal explosion on Porcelain Terrace at Norris Geyser Basin.  Top plot is seismic data from the YNM station, located at the Norris Geyser Basin Museum.  Middle plot is seismic data from station YNB, in the Ragged Hills of Norris Geyser Basin. Bottom plot is infrasound data from station YNB.&nb

table of geochronology techniques
table of geochronology techniques
table of geochronology techniques
table of geochronology techniques

Table showing different types of geochronology techniques, the ages over which those techniques are best applied, and the meaning of the ages determined by the techniques.

Table showing different types of geochronology techniques, the ages over which those techniques are best applied, and the meaning of the ages determined by the techniques.

Plots showing the number of water samples collected over time (top) and by location (bottom) in the Yellowstone region since the late 1800s
Plots showing the number of water samples collected over time (top) and by location (bottom) in the Yellowstone region since the late 1800s
Plots showing the number of water samples collected over time (top) and by location (bottom) in the Yellowstone region since the late 1800s
Plots showing the number of water samples collected over time (top) and by location (bottom) in the Yellowstone region since the late 1800s

Plots showing the number of water samples collected over time (top) and by location (bottom) in the Yellowstone region since the late 1800s. Yellowstone’s archive of water-chemistry research data is a mosaic of scientific progress, built with the work of hundreds of people over more than a century and still growing today.

High-resolution satellite images of Norris Geyser Basin showing the area of Porcelain Basin and Nuphar Lake in April 2024
High-resolution satellite images of Norris Geyser Basin showing the area of Porcelain Basin and Nuphar Lake in April 2024
High-resolution satellite images of Norris Geyser Basin showing the area of Porcelain Basin and Nuphar Lake in April 2024
High-resolution satellite images of Norris Geyser Basin showing the area of Porcelain Basin and Nuphar Lake in April 2024

High-resolution satellite images of Norris Geyser Basin showing the area of Porcelain Basin and Nuphar Lake in April 2024.  In the left image, acquired on April 2, 2024, springs on Porcelain Terrace are full of water, and warm hydrothermal water is flowing into Nuphar Lake, keeping the north part of the lake free of ice.  Boardwalks in the area appear as w

High-resolution satellite images of Norris Geyser Basin showing the area of Porcelain Basin and Nuphar Lake in April 2024.  In the left image, acquired on April 2, 2024, springs on Porcelain Terrace are full of water, and warm hydrothermal water is flowing into Nuphar Lake, keeping the north part of the lake free of ice.  Boardwalks in the area appear as w

Text says Mount St. Helens, Land of Transformation
Mount St. Helens: Land of Transformation
Mount St. Helens: Land of Transformation
Mount St. Helens: Land of Transformation

Mount St. Helens: Land of Transformation video shows the changes to the landscape from before the May 18, 1980 eruption to today (2024).

Color photograph of volcano scientist accepting an award
Ed Brown, center, receiving an Information, Management and Technology award
Ed Brown, center, receiving an Information, Management and Technology award
Ed Brown, center, receiving an Information, Management and Technology award

Ed Brown, center, receiving an Information, Management and Technology award from the Office of the Associate Chief Information Officer for his leadership and commitment to the USGS. The award was presented by Alan Wiser (left) and Tim Quinn (right) at the Information Technology Exchange Meeting in April 2024. 

Ed Brown, center, receiving an Information, Management and Technology award from the Office of the Associate Chief Information Officer for his leadership and commitment to the USGS. The award was presented by Alan Wiser (left) and Tim Quinn (right) at the Information Technology Exchange Meeting in April 2024. 

History of travertine deposition in Yellowstone caldera and correlation with past climate conditions
History of travertine deposition in Yellowstone caldera and correlation with past climate conditions
History of travertine deposition in Yellowstone caldera and correlation with past climate conditions
History of travertine deposition in Yellowstone caldera and correlation with past climate conditions

History of travertine deposition in Yellowstone caldera and correlation with past climate conditions. a) The age of travertine samples (based on the U-230Th geochronometer) from Old Hillside Springs, Hillside Springs, North Hillside Springs, and Morning Glory in Upper Geyser Basin and from Firehole Lake in Lower Geyser Basin.

History of travertine deposition in Yellowstone caldera and correlation with past climate conditions. a) The age of travertine samples (based on the U-230Th geochronometer) from Old Hillside Springs, Hillside Springs, North Hillside Springs, and Morning Glory in Upper Geyser Basin and from Firehole Lake in Lower Geyser Basin.

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