Photographs of the two dominant rock types found on Mount Everts: the Everts Formation (photo by Natali Kragh, May 18, 2021) and the Landslide Creek Formation (photo by Emma Kerins, May 2021). Notice the difference in scale between these two units, indicated by the pencil and field book.
Images
Images of Yellowstone.
![The two dominant rock types found on Mount Everts, Yellowstone National Park](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/geologic%20units.jpg?itok=7-ydgeTy)
Photographs of the two dominant rock types found on Mount Everts: the Everts Formation (photo by Natali Kragh, May 18, 2021) and the Landslide Creek Formation (photo by Emma Kerins, May 2021). Notice the difference in scale between these two units, indicated by the pencil and field book.
Photographs of travertine in Yellowstone. A) Travertine terraces actively forming at Mammoth Hot Springs.
Photographs of travertine in Yellowstone. A) Travertine terraces actively forming at Mammoth Hot Springs.
![Location of major travertine deposits in Yellowstone National Park](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/travertine_locations%20NEW.jpg?itok=NfX7aojl)
Map of Yellowstone National Park showing the location of major travertine deposits. The green dashed line is the outline of Yellowstone Caldera and red lines are major paved roads.
Map of Yellowstone National Park showing the location of major travertine deposits. The green dashed line is the outline of Yellowstone Caldera and red lines are major paved roads.
Travertine sample from the Hillside Springs Group in Upper Geyser Basin, sampled under permit YELL-2020-SCI-8030. (Left) Cut and polished sample slab showing the different layers of travertine; dashed circles indicate where subsamples were taken for geochronology analysis.
Travertine sample from the Hillside Springs Group in Upper Geyser Basin, sampled under permit YELL-2020-SCI-8030. (Left) Cut and polished sample slab showing the different layers of travertine; dashed circles indicate where subsamples were taken for geochronology analysis.
Map of Yellowstone’s thermal areas. Thermally active thermal areas (known to have thermal features with above-background temperatures) are shown in red. Inactive and cold, degassing thermal areas are shown in blue. Areas that are unknown or inconclusive in terms of their thermal activity are shown in purple.
Map of Yellowstone’s thermal areas. Thermally active thermal areas (known to have thermal features with above-background temperatures) are shown in red. Inactive and cold, degassing thermal areas are shown in blue. Areas that are unknown or inconclusive in terms of their thermal activity are shown in purple.
![Visible and thermal maps of Brimstone Basin (top) and Midway / Lower Geyser Basins (bottom).](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Figure%202_9.jpg?itok=8nzy_4ob)
Visible and thermal maps of Brimstone Basin (top) and Midway / Lower Geyser Basins (bottom). The images on the left are high-resolution (1-m pixels) visible images acquired by the NAIP program in 2019. In these images, the extent of the bright white surface cover is visual evidence for the thermal area, and the yellow thermal area boundaries have been di
Visible and thermal maps of Brimstone Basin (top) and Midway / Lower Geyser Basins (bottom). The images on the left are high-resolution (1-m pixels) visible images acquired by the NAIP program in 2019. In these images, the extent of the bright white surface cover is visual evidence for the thermal area, and the yellow thermal area boundaries have been di
![Outline of the Steamboat and Cistern plumbing systems from seismic data](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Figure8_Plumbing_geometry_v1.jpg?itok=AsQ5Yw7j)
Outline of the Steamboat and Cistern plumbing systems, with two viewing angles. The structure, color-coded by depth, delineates the observed seismically active area during eruption cycles of Steamboat Geyser. The solid star, solid square, and open triangles denote Steamboat Geyser, Cistern Spring, and seismic station locations on the surface, respectively.
Outline of the Steamboat and Cistern plumbing systems, with two viewing angles. The structure, color-coded by depth, delineates the observed seismically active area during eruption cycles of Steamboat Geyser. The solid star, solid square, and open triangles denote Steamboat Geyser, Cistern Spring, and seismic station locations on the surface, respectively.
![colored areas showing seismic views](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Steamboat%20seismic%20thumbnail.jpg?itok=ceDRGjfZ)
Outline of the Steamboat and Cistern plumbing systems. The structure, color-coded by depth, delineates the observed seismically active area during eruption cycles of Steamboat Geyser. The solid star, solid square, and open triangles denote Steamboat Geyser, Cistern Spring, and seismic station locations on the surface, respectively.
Outline of the Steamboat and Cistern plumbing systems. The structure, color-coded by depth, delineates the observed seismically active area during eruption cycles of Steamboat Geyser. The solid star, solid square, and open triangles denote Steamboat Geyser, Cistern Spring, and seismic station locations on the surface, respectively.
![Crinoid fossil from northern Yellowstone National Park](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Yellowstone%20Crinoid.jpg?itok=8Zv9_sXJ)
Crinoid fossil from a Paleozoic rock unit found in northern Yellowstone National Park.
Crinoid fossil from a Paleozoic rock unit found in northern Yellowstone National Park.
Example of some of the new layers available in the Geology of Yellowstone Map as of early 2021. Shown here are the locations of various monitoring instruments and water sample sites overlain on a thermal infrared satellite image. Lighter colors on the infrared image show more radiant (warmer) areas, whereas dark areas are less radiant (cooler).
Example of some of the new layers available in the Geology of Yellowstone Map as of early 2021. Shown here are the locations of various monitoring instruments and water sample sites overlain on a thermal infrared satellite image. Lighter colors on the infrared image show more radiant (warmer) areas, whereas dark areas are less radiant (cooler).
Seismic stations (white triangles) around Yellowstone Lake as seen on the online Geology of Yellowstone Map. Inset shows a seismogram for station YLA that can be accessed by clicking on the feature and following the “Seismogram” link in the popup box.
Seismic stations (white triangles) around Yellowstone Lake as seen on the online Geology of Yellowstone Map. Inset shows a seismogram for station YLA that can be accessed by clicking on the feature and following the “Seismogram” link in the popup box.
![Rhyolite alteration viewed by a Secondary Electron Microscope](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Rhyolite_SEM-images.jpg?itok=cVZaWXU8)
Photos from a Scanning Electron Microscope (SEM) showing reacted rhyolite fragments at the end of the laboratory experiments. (a) Image magnified by 500 times showing the rhyolite after it reacted with water at 250 degrees Celsius (482 F). The reacted rhyolite fragments show very little change compared with the unreacted fragments.
Photos from a Scanning Electron Microscope (SEM) showing reacted rhyolite fragments at the end of the laboratory experiments. (a) Image magnified by 500 times showing the rhyolite after it reacted with water at 250 degrees Celsius (482 F). The reacted rhyolite fragments show very little change compared with the unreacted fragments.
Mudpot located in the Mud Volcano thermal area of Yellowstone National Park. This type of thermal feature indicates an acid-sulfate system.
Mudpot located in the Mud Volcano thermal area of Yellowstone National Park. This type of thermal feature indicates an acid-sulfate system.
Steam vents along the Yellowstone River near Mud Volcano thermal area, Yellowstone National Park.
Steam vents along the Yellowstone River near Mud Volcano thermal area, Yellowstone National Park.
![Thermal anomaly map of Yellowstone National Park based on a Landsat 8 nighttime thermal infrared image from 9 January 2021](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/TIR%20map%20from%20L7%202021%20Jan%209.jpg?itok=pkKxS-Cm)
Thermal anomaly map of Yellowstone National Park based on a Landsat 8 nighttime thermal infrared image from 9 January 2021
linkThermal anomaly map of Yellowstone National Park, based on a Landsat 8 nighttime thermal infrared image from 9 January 2021. The color ramp indicates the intensity of the above-background thermal anomaly for each thermal area. Lakes are blue. Yellowstone caldera and resurgent domes are outlined in black.
Thermal anomaly map of Yellowstone National Park based on a Landsat 8 nighttime thermal infrared image from 9 January 2021
linkThermal anomaly map of Yellowstone National Park, based on a Landsat 8 nighttime thermal infrared image from 9 January 2021. The color ramp indicates the intensity of the above-background thermal anomaly for each thermal area. Lakes are blue. Yellowstone caldera and resurgent domes are outlined in black.
![Columbia River Basalts seen at Steens Mountain, Oregon](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Steens%20mountain%20summit%20area.jpg?itok=ZTygqE39)
Looking southwest from the Steens Mountain summit area into the Alvord desert of eastern Oregon. This fault-block escarpment reveals the oldest lava flows of the Columbia River Flood Basalts, which erupted about 17 million years ago. Three or four vertical dikes that feed these flows are evident in the midground ridge where they stand as rock walls cutti
Looking southwest from the Steens Mountain summit area into the Alvord desert of eastern Oregon. This fault-block escarpment reveals the oldest lava flows of the Columbia River Flood Basalts, which erupted about 17 million years ago. Three or four vertical dikes that feed these flows are evident in the midground ridge where they stand as rock walls cutti
Eruptions of Steamboat Geyser over time. (A) Cumulative eruptions of Steamboat Geyser since 1960. Each dot represents an eruption. (B) Comparative plot of the cumulative eruptions in each active phase (1960s, 1980s, and 2018-). Data from GeyserTimes.
Eruptions of Steamboat Geyser over time. (A) Cumulative eruptions of Steamboat Geyser since 1960. Each dot represents an eruption. (B) Comparative plot of the cumulative eruptions in each active phase (1960s, 1980s, and 2018-). Data from GeyserTimes.
Steamboat Geyser eruption signals recorded by nearby monitoring instruments. The vertical pink lines mark when the signal first appears. (A) Seismic station YNM records a signal which slowly tapers as the eruption decreases in intensity. Spikes seen before the eruption are mostly due to human activity.
Steamboat Geyser eruption signals recorded by nearby monitoring instruments. The vertical pink lines mark when the signal first appears. (A) Seismic station YNM records a signal which slowly tapers as the eruption decreases in intensity. Spikes seen before the eruption are mostly due to human activity.
![Map of seismicity in the Yellowstone region during 2020](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/fig1%20-%20EQmap%202020.jpg?itok=ZePg38x2)
Map of seismicity (red circles) in the Yellowstone region during 2020. Gray lines are roads, red line shows the caldera boundary, Yellowstone National Park is outlined by black dashed line, and gray dashed lines denote state boundaries.
Map of seismicity (red circles) in the Yellowstone region during 2020. Gray lines are roads, red line shows the caldera boundary, Yellowstone National Park is outlined by black dashed line, and gray dashed lines denote state boundaries.
![Section from the piston core YL92-1C, collected in south-central Yellowstone Lake](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/Y92-1C%20core%20Elliott%27s%20Crater.jpg?itok=pl6ykzMG)
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.
![Satellite view of Ngorongoro volcano, in Tanzania, east Africa](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/caldera%20from%20space.jpg?itok=OoyusHS7)
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.