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Images of Yellowstone.
Experimental apparatus for reacting hot water and rhyolite. The photo on the left shows the inert gold bags into which the rhyolite fragments and water were inserted. After being sealed, the gold bag is then placed into a steel pressure vessel, which itself is loaded into a furnace (photo on the right).
Experimental apparatus for reacting hot water and rhyolite. The photo on the left shows the inert gold bags into which the rhyolite fragments and water were inserted. After being sealed, the gold bag is then placed into a steel pressure vessel, which itself is loaded into a furnace (photo on the right).
Yellowstone rangers -- and tourists, too! -- can determine the height of a geyser eruption with some simple trigonometry.
Yellowstone rangers -- and tourists, too! -- can determine the height of a geyser eruption with some simple trigonometry.
Absolute versus relative earthquake locations associated with 2019 Ridgecrest, California, foreshock and aftershock sequence. Animated GIF image compares the routine catalog earthquake locations with those from an enhanced catalog employing precise relative locations. Depths are color-coded as shown. Triangles indicate seismic stations.
Absolute versus relative earthquake locations associated with 2019 Ridgecrest, California, foreshock and aftershock sequence. Animated GIF image compares the routine catalog earthquake locations with those from an enhanced catalog employing precise relative locations. Depths are color-coded as shown. Triangles indicate seismic stations.
Ngorongoro volcano, in Tanzania, east Africa, is a caldera that formed 2-3 million years ago. The Ngorongoro Conservation Area is a UNESCO World Heritage Site and home to one of the densest concentrations of wildlife in Africa. Satellite Image from CNES/Airbus via Google Earth.
Ngorongoro volcano, in Tanzania, east Africa, is a caldera that formed 2-3 million years ago. The Ngorongoro Conservation Area is a UNESCO World Heritage Site and home to one of the densest concentrations of wildlife in Africa. Satellite Image from CNES/Airbus via Google Earth.
Section from the piston core YL92-1C, collected in south-central Yellowstone Lake. The core is viewed horizontally, with the top of core to the left. The core section shown is from 5.21–5.63 meters (17–18.4 feet) depth.
Section from the piston core YL92-1C, collected in south-central Yellowstone Lake. The core is viewed horizontally, with the top of core to the left. The core section shown is from 5.21–5.63 meters (17–18.4 feet) depth.
Swath bathymetric image of the Elliott’s Crater explosion crater in Yellowstone Lake. Inset shows location of the crater and the swath image (red box) within the northern part of the lake.
Swath bathymetric image of the Elliott’s Crater explosion crater in Yellowstone Lake. Inset shows location of the crater and the swath image (red box) within the northern part of the lake.
Research drilling in Yellowstone National Park. (A) is an image from Fenner (1936) of the drilling setup in the Upper Geyser Basin during the 1929 field season. (B) is an image from White et al. (1975) of the USGS drill rig set up in the Norris Geyser Basin in 1967-68 during a steam eruption.
Research drilling in Yellowstone National Park. (A) is an image from Fenner (1936) of the drilling setup in the Upper Geyser Basin during the 1929 field season. (B) is an image from White et al. (1975) of the USGS drill rig set up in the Norris Geyser Basin in 1967-68 during a steam eruption.
The right side of the figure is an image of a small piece of the Y-9 core from the USGS 1967-68 drilling expedition to Yellowstone National Park. The black area was analyzed using a scanning electron microscope (SEM) at the University of Wyoming to determine mineralogy and dispersion of elements.
The right side of the figure is an image of a small piece of the Y-9 core from the USGS 1967-68 drilling expedition to Yellowstone National Park. The black area was analyzed using a scanning electron microscope (SEM) at the University of Wyoming to determine mineralogy and dispersion of elements.
Map of earthquakes that occurred beneath Yellowstone Lake as parts of seismic swarms in 2008-2009 (green) and 2020 (red). Orange line is the boundary of Yellowstone Caldera, which formed 631,000 years ago.
Map of earthquakes that occurred beneath Yellowstone Lake as parts of seismic swarms in 2008-2009 (green) and 2020 (red). Orange line is the boundary of Yellowstone Caldera, which formed 631,000 years ago.
Rate of earthquake occurrence for the 2008-2009 Yellowstone Lake swarm (green) and 2020 swarm (red).
Rate of earthquake occurrence for the 2008-2009 Yellowstone Lake swarm (green) and 2020 swarm (red).
Lidar hillshade map of part of the Blackfoot Volcanic Field, showing rhyolite domes and fault scarps.
Lidar hillshade map of part of the Blackfoot Volcanic Field, showing rhyolite domes and fault scarps.
Map of southeastern Idaho showing volcanic rocks related to the Yellowstone hotspot. Basalt is shown in red and rhyolite in yellow. Blue circles indicate the location of past Yellowstone calderas; caldera names and approximate ages are shown (Ma = million years old).
Map of southeastern Idaho showing volcanic rocks related to the Yellowstone hotspot. Basalt is shown in red and rhyolite in yellow. Blue circles indicate the location of past Yellowstone calderas; caldera names and approximate ages are shown (Ma = million years old).
Year-long (August 2017 to August 2018) temperature records from two hydrothermal vents (“A” and “B”) in the Deep Hole area of Yellowstone Lake.
Year-long (August 2017 to August 2018) temperature records from two hydrothermal vents (“A” and “B”) in the Deep Hole area of Yellowstone Lake.
Old Faithful bathhouse as it appeared in 1914-1933 (top) and 1934-1951 (bottom).
Old Faithful bathhouse as it appeared in 1914-1933 (top) and 1934-1951 (bottom).
Photograph of Obsidian Cliff along Grand Loop Road between Norris and Mammoth Hot Springs. Photograph by John Good, U.S. National Park Service, 1965.
Photograph of Obsidian Cliff along Grand Loop Road between Norris and Mammoth Hot Springs. Photograph by John Good, U.S. National Park Service, 1965.
Map of Yellowstone National Park adapted from Christiansen and others (2007). The pink regions are rhyolite flows erupted within Yellowstone caldera; these flows contain 5% to 15% crystals by volume. The purple region is the Obsidian Cliff flow, which contains close to 0% crystals.
Map of Yellowstone National Park adapted from Christiansen and others (2007). The pink regions are rhyolite flows erupted within Yellowstone caldera; these flows contain 5% to 15% crystals by volume. The purple region is the Obsidian Cliff flow, which contains close to 0% crystals.
Crested Pool, in Upper Geyser Basin near Castle Geyser. Geyser Hill is in the background, and Old Faithful is the steaming feature at the upper right. USGS photo by Mike Poland, October 12, 2020.
Crested Pool, in Upper Geyser Basin near Castle Geyser. Geyser Hill is in the background, and Old Faithful is the steaming feature at the upper right. USGS photo by Mike Poland, October 12, 2020.
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
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.
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.
Panoramic photo of Pocket Basin, a hydrothermal explosion crater in Yellowstone National Park's Lower Geyser Basin, taken from the northeast rim looking southwest into the crater. Pocket Basin is a U-shaped crater that is dissected on the SW edge by the Firehole River, visible on the far-right of the photo.
Panoramic photo of Pocket Basin, a hydrothermal explosion crater in Yellowstone National Park's Lower Geyser Basin, taken from the northeast rim looking southwest into the crater. Pocket Basin is a U-shaped crater that is dissected on the SW edge by the Firehole River, visible on the far-right of the photo.