Map of the Uhl Hill fault in eastern Grand Teton National Park. Base map is a 1-meter lidar hillshade. Black arrows mark the visible fault scarp, and red lines mark locations where scarp profiles were generated from lidar data or field surveying.
Images
Images related to Yellowstone Volcano Observatory.
![Map of the Uhl Hill fault in eastern Grand Teton National Park, Wyoming](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/UHF_map.png?itok=YaYwv8MK)
Map of the Uhl Hill fault in eastern Grand Teton National Park. Base map is a 1-meter lidar hillshade. Black arrows mark the visible fault scarp, and red lines mark locations where scarp profiles were generated from lidar data or field surveying.
![Scarp of the Uhl Hill fault in eastern Grand Teton National Park, Wyoming](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/UHF_photo_and_profile.png?itok=d1zqhXDb)
Scarp of the Uhl Hill fault. Photo (top) is looking west at the east-facing fault scarp, with a geologist at the top of the scarp for scale. Here, the fault cuts through Pinedale-1 glacial deposits just south of a Pinedale-2 end moraine. Plot (bottom) is a scarp profile generated from lidar elevation data.
Scarp of the Uhl Hill fault. Photo (top) is looking west at the east-facing fault scarp, with a geologist at the top of the scarp for scale. Here, the fault cuts through Pinedale-1 glacial deposits just south of a Pinedale-2 end moraine. Plot (bottom) is a scarp profile generated from lidar elevation data.
![Difference in mapped rock units for Mount Everts, Yellowstone National Park](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/Mount%20Everts%20mapping%20comparison.jpg?itok=9eRjbf2o)
Simplified geologic maps showing the difference in mapped rock units from the current, large-scale geologic maps dividing Mount Everts and that join along the boundary between Montana and Wyoming.
Simplified geologic maps showing the difference in mapped rock units from the current, large-scale geologic maps dividing Mount Everts and that join along the boundary between Montana and Wyoming.
![Reconstructed fossil horse skeleton found at Hagerman Fossil Beds National Monument, Idaho](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/Fig_5_equus-simplicidens-display-2000-px.jpg?itok=8KDbMNog)
Reconstructed fossil horse skeleton found at Hagerman Fossil Beds National Monument, Idaho. National Park Service photo, https://www.nps.gov/articles/000/equus_simplicidens.htm.
Reconstructed fossil horse skeleton found at Hagerman Fossil Beds National Monument, Idaho. National Park Service photo, https://www.nps.gov/articles/000/equus_simplicidens.htm.
Screenshot of the December 8, 2021 Yellowstone volcano monitoring map. Seismometers, GPS, and earthquakes are the displayed icons, which can be filtered in the right menu.
Screenshot of the December 8, 2021 Yellowstone volcano monitoring map. Seismometers, GPS, and earthquakes are the displayed icons, which can be filtered in the right menu.
![Regional map of southeastern Idaho showing Stanley earthquakes](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/Stanley_and_Yellowstone_Map_YNP.jpg?itok=55ojr5nk)
Regional map of southeastern Idaho showing the relative location of Yellowstone National Park and the Stanley earthquake aftershocks. Yellowstone National Park (outlined in yellow) is at least 275 km away from the 2020 Mw6.5 Stanley earthquake. Several active faults (in red) are located between the Stanley earthquake and Yellowstone Caldera.
Regional map of southeastern Idaho showing the relative location of Yellowstone National Park and the Stanley earthquake aftershocks. Yellowstone National Park (outlined in yellow) is at least 275 km away from the 2020 Mw6.5 Stanley earthquake. Several active faults (in red) are located between the Stanley earthquake and Yellowstone Caldera.
![Cumulative number of aftershocks greater than magnitude 2.5 following the 2020 magnitude 6.5 Stanley earthquake](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/Stanley_Aftershocks.jpg?itok=7AN06CuP)
Cumulative number of aftershocks greater than magnitude 2.5 following the 2020 magnitude 6.5 Stanley earthquake
linkCumulative number of aftershocks greater than magnitude 2.5 following the March 30, 2020, magnitude-6.5 Stanley earthquake in central Idaho. The black line shows the observed aftershocks, the red line shows the predicted number of aftershocks. Aftershocks are a normal and expected phenomenon following strong tectonic earthquakes.
Cumulative number of aftershocks greater than magnitude 2.5 following the 2020 magnitude 6.5 Stanley earthquake
linkCumulative number of aftershocks greater than magnitude 2.5 following the March 30, 2020, magnitude-6.5 Stanley earthquake in central Idaho. The black line shows the observed aftershocks, the red line shows the predicted number of aftershocks. Aftershocks are a normal and expected phenomenon following strong tectonic earthquakes.
![A branching root cast from grasses that grew on the ashy lahars deposited along the ancestral Missouri River system](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/Figure%203.jpeg?itok=nXHrAvjn)
A branching root cast from grasses that grew on the ashy lahars deposited along the ancestral Missouri River system
linkA branching root cast from grasses that grew on the ashy lahars deposited along the ancestral Missouri River system. Plant roots growing in calcareous soils made holes that were filled with calcite after the organics rotted away. Photo by Rob Thomas, August 2021.
A branching root cast from grasses that grew on the ashy lahars deposited along the ancestral Missouri River system
linkA branching root cast from grasses that grew on the ashy lahars deposited along the ancestral Missouri River system. Plant roots growing in calcareous soils made holes that were filled with calcite after the organics rotted away. Photo by Rob Thomas, August 2021.
Comparison of (a) 1904 Historical map with (b) 1988 USGS map. Colloidal Pool is a large, labeled pool roughly located on a straight line between Hurricane vent and Whirligig Geyser on the 1988 map (b); this same transect on the 1904 map (a) shows no feature at that location (white circle).
Comparison of (a) 1904 Historical map with (b) 1988 USGS map. Colloidal Pool is a large, labeled pool roughly located on a straight line between Hurricane vent and Whirligig Geyser on the 1988 map (b); this same transect on the 1904 map (a) shows no feature at that location (white circle).
Scanning electron microscopy (SEM) images of the Colloidal Pool colloids (images are a combination of backscatter and secondary electrons). The colloids are a mixture of clay particles, hydrated silica, alunite, and diatoms.
Scanning electron microscopy (SEM) images of the Colloidal Pool colloids (images are a combination of backscatter and secondary electrons). The colloids are a mixture of clay particles, hydrated silica, alunite, and diatoms.
Microscope thin-section photo of Lava Creek Tuff “unit 2.” Photo by Ray Salazar (Montana State University) on October 28, 2021.
Microscope thin-section photo of Lava Creek Tuff “unit 2.” Photo by Ray Salazar (Montana State University) on October 28, 2021.
![View of White Mountain from the Sunlight Basin Road](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/whitemtn.jpg?itok=_r99UZox)
A view of White Mountain -- a deposit of the Heart Mountain detachment -- from the Sunlight Basin Road in Wyoming. Much of the evidence supporting the lamprophyre diatreme triggering mechanism theory for the landslide was gathered at White Mountain.
A view of White Mountain -- a deposit of the Heart Mountain detachment -- from the Sunlight Basin Road in Wyoming. Much of the evidence supporting the lamprophyre diatreme triggering mechanism theory for the landslide was gathered at White Mountain.
![Different views of an eruption from two predictable geysers](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/calderachronicles_nurschuba_fig01-2.jpg?itok=irCpPPVp)
Different views of an eruption from two predictable geysers. (a, c) Graphs showing water temperatures recorded by data loggers stationed near Beehive and Old Faithful Geysers, respectively. These data loggers were deployed by the Yellowstone Geology Program, configured to capture temperatures at one-minute intervals (indicated by blue dots).
Different views of an eruption from two predictable geysers. (a, c) Graphs showing water temperatures recorded by data loggers stationed near Beehive and Old Faithful Geysers, respectively. These data loggers were deployed by the Yellowstone Geology Program, configured to capture temperatures at one-minute intervals (indicated by blue dots).
![Example initial analyses on the water temperature data](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/calderachronicles_nurschuba_fig02-2.jpg?itok=JLWe2Hgm)
Example initial analyses on the water temperature data. (a, c) Graphs showing the calculated time between eruptions. (b, d) Histograms demonstrating the distribution of eruption intervals.
Example initial analyses on the water temperature data. (a, c) Graphs showing the calculated time between eruptions. (b, d) Histograms demonstrating the distribution of eruption intervals.
![Research Vessel Annie and Remotely Operated Vehicle Yogi](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/F02_RV_Annie_YOGI.jpg?itok=xi6-mDPj)
Research Vessel Annie and Remotely Operated Vehicle Yogi. a) R/V Annie on Yellowstone Lake operated by the Global Foundation for Ocean Exploration. Image Rob Harris, OSU. b) ROV Yogi with GFOE President Dave Lovalvo. Image Todd Gregory, GFOE. C) ROV Yogi and 1-m heat flow probe. This pr
Research Vessel Annie and Remotely Operated Vehicle Yogi. a) R/V Annie on Yellowstone Lake operated by the Global Foundation for Ocean Exploration. Image Rob Harris, OSU. b) ROV Yogi with GFOE President Dave Lovalvo. Image Todd Gregory, GFOE. C) ROV Yogi and 1-m heat flow probe. This pr
![Yellowstone Lake bathymetry showing the location of the Deep Hole vent field](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/lake%20bathy%20and%20deephole%20zoom.jpg?itok=L26SqX5Y)
Yellowstone Lake bathymetry showing the location of the Deep Hole vent field. Inset shows locations of heat-flux measurements (red dots) in the Deep Hole vent field.
Yellowstone Lake bathymetry showing the location of the Deep Hole vent field. Inset shows locations of heat-flux measurements (red dots) in the Deep Hole vent field.
![USGS Earth Explorer web tool showing an example of the geographic area and date range search criteria for Yellowstone](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Figure%202_11.jpg?itok=aWllOG5Q)
Screen shot of the USGS Earth Explorer web tool showing an example of the geographic area and date range search criteria for Yellowstone.
Screen shot of the USGS Earth Explorer web tool showing an example of the geographic area and date range search criteria for Yellowstone.
![USGS Earth Explorer screen shot showing example of selecting the Data Sets to search](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Figure%203_5.jpg?itok=gG5fMmko)
USGS Earth Explorer screen shot showing example of selecting the Data Sets to search.
USGS Earth Explorer screen shot showing example of selecting the Data Sets to search.
![USGS Earth Explorer screen shot showing example of Landsat 8 search results over Yellowstone](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Figure%204_2.jpg?itok=iCuaPi2g)
USGS Earth Explorer screen shot showing example of Landsat 8 search results over Yellowstone.
USGS Earth Explorer screen shot showing example of Landsat 8 search results over Yellowstone.
![Site of the former Fountain Hotel in Yellowstone National Park](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/media/images/pipe.jpg?itok=b3ot0jmi)
Site of the former Fountain Hotel in Yellowstone National Park. Red arrows indicate the location of the pipe that ran through the meadow between Leather Pool and the site of the Fountain Hotel (yellow arrow). Yellowstone National Park photo by Annie Carlson, October 2021.
Site of the former Fountain Hotel in Yellowstone National Park. Red arrows indicate the location of the pipe that ran through the meadow between Leather Pool and the site of the Fountain Hotel (yellow arrow). Yellowstone National Park photo by Annie Carlson, October 2021.
![Shaded relief map of Henrys Fork Caldera and vicinity](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/Henry%27s%20Fork%20area%20map.jpg?itok=52F48Veq)
Shaded relief map of Henrys Fork Caldera and vicinity. The margin of Henrys Fork Caldera is shown in blue. Note the smooth, low-relief topography within the caldera compared to the steep and dynamic topography associated with Yellowstone Caldera (at the right side of the image).
Shaded relief map of Henrys Fork Caldera and vicinity. The margin of Henrys Fork Caldera is shown in blue. Note the smooth, low-relief topography within the caldera compared to the steep and dynamic topography associated with Yellowstone Caldera (at the right side of the image).