Images

High-resolution Planet satellite image of Biscuit Basin, Yellowstone National Park, from July 24, 2024.  The image shows changes that occurred as a result of the July 23, 2024, hydrothermal explosion from Black Diamond Pool, including deposition of material in the vicinity of the pool and a plume of discolored water in the Forehole River.

Webicorders of Yellowstone Seismic Network stations YMR (West Entrance road) and YNM (Norris Geyser Basin Museum) showing traffic signals (left) and visitors walking (right) during daytime hours.  Both records span the entire 24-hour period of July 23, 2024, MDT. 

Webicorders of Yellowstone Seismic Network stations YMR (West Entrance road) and YNM (Norris Geyser Basin Museum) showing traffic signals (left) and visitors walking (right) during daytime hours.  Both records span the entire 24-hour period of July 23, 2024, MDT. 

Aerial view of Biscuit Basin, Yellowstone National Park, showing debris deposited by the July 23, 2024, hydrothermal explosion from Black Diamond Pool.  Major features are labeled.  The main debris field (within dashed yellow line) has a gray appearance.  Photo taken by Joe Bueter, Yellowstone National Park, on July 23, 2024.

Webicorders of Yellowstone Seismic Network stations YMR (West Entrance road) and YNM (Norris Geyser Basin Museum) showing traffic signals (left) and visitors walking (right) during daytime hours.  Both records span the entire 24-hour period of July 23, 2024, MDT. 

Cover of the Yellowstone Volcano Observatory response plan for geological hazards in the Yellowstone region.  The report can be accessed at https://pubs.usgs.gov/circ/1351/.  Cover features a photograph by Mike Poland and frame captures from a video by Juliet Su.

Webicorders of Yellowstone Seismic Network stations YMR (West Entrance road) and YNM (Norris Geyser Basin Museum) showing traffic signals (left) and visitors walking (right) during daytime hours.  Both records span the entire 24-hour period of July 23, 2024, MDT. 

Webicorders of Yellowstone Seismic Network stations YMR (West Entrance road) and YNM (Norris Geyser Basin Museum) showing traffic signals (left) and visitors walking (right) during daytime hours.  Both records span the entire 24-hour period of July 23, 2024, MDT. 

High-resolution Planet satellite image of Biscuit Basin, Yellowstone National Park, from July 21, 2024.  This work utilized data made available through the NASA Commercial Smallsat Data Acquisition (CSDA) Program.  Data are copyright, Planet Labs Inc. 2024, all rights reserved.
 

Map of major thermal features in Biscuit Basin, Yellowstone National Park.  Base map from Google Earth

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.

Coronal mass ejections (CMEs) move from the surface of the Sun towards Earth through space. Top: CME is generated as an outflow of plasma and magnetic fields from the Sun, moving through space to Earth over a matter of hours. Bottom: The magnetic fields of the CME and outflowing solar wind interact with Earth’s magnetic field, which shields it from greater effect.

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.  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.  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

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.

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.

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.

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.

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.

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.