Images

Wahb Springs in Yellowstone National Park.  Left: zoomed-out photo of the springs (photo by David Roth, September 2024). Right: close-up photo showing the unique organic material floating on the spring water (photo by Shaul Hurwitz, September 2024).

Photo of dead trees along the edge of Nuphar Lake.  The white staining at the base of the trees is a telltale sign that the trees were immersed in thermal water containing silica.  USGS photo by Mike Poland, September 1, 2024.

Looking south from near a pullout along the Mammoth to Norris road just north of the Nymph Lake overlook. On the other side of the marsh is a tree-covered rhyolite lava flow, and at the base of the flow is a new thermal feature marked by a plume of steam and that formed in early August 2024.   Photo by Mike Poland, USGS, September 1, 2024.

Gibbon River near Norris Geyser Basin in Yellowstone National Park at sunset.  USGS Photo by Mike Poland, August 28, 2024.

Professor C.J.N. Wilson, FRS, pays due homage to the Lava Creek Tuff ashfall bed in a basin just east of Shell, Wyoming. Photo by Madison Myers, Montana State University, August 9, 2024.

Drew Robinson, a USGS hydrological technician, is putting a Rapid Deployment Gauge together for the Georgia Department of Transportation on Wednesday, August 7. He built the RDG and deployed it in Statesboro in the early evening. That RDG was used to help the local community experiencing bad floods on Lotts Creek.

Looking southeast at the hydrothermal feature that formed in August 2024 just north of Nymph Lake. Steam is emanating from a vent that is partially full of water to create the frying pan feature nestled in the newly formed vent. A thin grey layer of silica mud covers the vent area.  Photo by Jefferson Hungerford, Yellowstone National Park, August 2024.

Plot of size versus annual probability for hydrothermal explosion craters in Yellowstone National Park. The line is a model based on the energy required to form a crater of a specific size, and it is fit to known hydrothermal explosion craters in Yellowstone National Park.

(A) Water distribution in a quartz-hosted embayment measured with synchrotron Fourier Transform Infrared spectroscopy. Warmer colors indicate higher concentrations of water.  Dashed line shows a transect of water content that is modeled in panel (B) to indicate that the emplacement temperature of the ash flow deposit must have been about 500 °C (930 °F).

A clean hand sample of the Mount Jackson vitrophyre. This sample has a black, glassy groundmass with large (1–3 mm, or a small fraction of an inch), white phenocrysts suspended in the glass. Photo by Liv Wheeler, Montana State University, August 2024.

Shaded relief location map for the East Gallatin-Reese Creek fault system (EGRCFS) in northwest Yellowstone National Park (YNP). The location of the EGRCFS is shown as mapped in the U.S.

Abyss Pool is about 16 m (53 ft) deep and contains alkaline-chloride hydrothermal fluids that in the summer of 2024 had a temperature of 181 °F (83 °C).

Mud pots form in a few selected areas of West Thumb Geyser Basin where low-pH acidic fluids dissolve rocks and soil to produce clay-rich muds.  USGS photo by Pat Shanks, 2024.

Graph showing explosions recorded at Black Diamond Pool in Biscuit Basin, Yellowstone National Park, during 2006 through 2016. Confirmed events refer to eruptions that were witnessed, recorded by temperature loggers, or inferred from their aftermath. Unconfirmed events refer to eruptions that were questionable or might have been misattributed to Black Diamond.

Lidar hillshade maps of fault scarps that offset Pinedale glacial till along the East Gallatin-Reese Creek fault system (EGRCFS) near Fawn Creek (A) and Panther Creek (B). Fault scarps are visible as darker lineaments in the hillshade and are marked by the black arrows. Red rectangles on inset maps show location along the EGRCFS.

(A) Photomicrograph of a quartz-hosted embayment from the Mesa Falls Tuff. “MI” indicates a glassy inclusion of melt within the crystal. (B) Thickness (in centimeters) and extent of the Mesa Falls ash flow deposit (pink areas) and its source, Henrys Fork Caldera (dashed line).  Figure by Kenneth Befus, University of Texas at Austin.

Cinder Pool, located in the southwest part of 100 Spring Plain in Norris Geyser Basin, Yellowstone National Park. The pool was known for “cinders” made of sulfur that condensed after rising from a molten layer at the bottom of the pool, but after 2019 those cinders disappeared.  Photos from June 2018 (left) and June 2023 (right) by Lauren Harrison.

Exposure of the Mount Jackson Rhyolite Series vitrophyre at Gibbon River. Boulders of weathered, lichen-covered rock show how easy it is to overlook these new units. Photo by Liv Wheeler, Montana State University, August 2024.

This boulder is the largest that is confirmed to have been part of the July 23, 2024, hydrothermal explosion from Black Diamond Pool, Biscuit Basin, Yellowstone National Park.  The tape measure is 50 centimeters (20 inches) long.  Black Diamond Pool and a boardwalk are in the background.

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.