Frying Pan Lake (also called Waimangu Cauldron), in New Zealand, sits within Echo Crater, which formed during the 1886 eruption of Tarawera. A hydrothermal explosion from the crater in 1917 resulted in the formation of the hot spring "lake" by 1918.
Images
Images related to Yellowstone Volcano Observatory.
Frying Pan Lake (also called Waimangu Cauldron), in New Zealand, sits within Echo Crater, which formed during the 1886 eruption of Tarawera. A hydrothermal explosion from the crater in 1917 resulted in the formation of the hot spring "lake" by 1918.
Subtle thermal ground revealed by wintertime satellite imagery of Twin Buttes, Yellowstone National Park
Subtle thermal ground revealed by wintertime satellite imagery of Twin Buttes, Yellowstone National ParkWorldView-2 natural-color satellite image from February 3, 2023, showing snow-free zones around Twin Buttes, just beyond the southwest portion of Lower Geyser Basin. At the time and date this image was acquired, there was extensive
Subtle thermal ground revealed by wintertime satellite imagery of Twin Buttes, Yellowstone National Park
Subtle thermal ground revealed by wintertime satellite imagery of Twin Buttes, Yellowstone National ParkWorldView-2 natural-color satellite image from February 3, 2023, showing snow-free zones around Twin Buttes, just beyond the southwest portion of Lower Geyser Basin. At the time and date this image was acquired, there was extensive
Map of the distribution of pH for thermal pools within Norris Geyser Basin, Yellowstone National Park
Map of the distribution of pH for thermal pools within Norris Geyser Basin, Yellowstone National ParkMap of the distribution of pH for thermal pools within Norris Geyser Basin, Yellowstone National Park. Cool colors are acidic, and warm colors are neutral to slightly basic. These data were collected and organized using Geographic Information System (GIS) tools. Map by Jefferson Hungerford and Kiernan Folz-Donahue, Yellowstone National Park.
Map of the distribution of pH for thermal pools within Norris Geyser Basin, Yellowstone National Park
Map of the distribution of pH for thermal pools within Norris Geyser Basin, Yellowstone National ParkMap of the distribution of pH for thermal pools within Norris Geyser Basin, Yellowstone National Park. Cool colors are acidic, and warm colors are neutral to slightly basic. These data were collected and organized using Geographic Information System (GIS) tools. Map by Jefferson Hungerford and Kiernan Folz-Donahue, Yellowstone National Park.
Volcanic deposits associated with the Absaroka volcanic province along the eastern and northern boundaries of Yellowstone National Park
Volcanic deposits associated with the Absaroka volcanic province along the eastern and northern boundaries of Yellowstone National ParkVolcanic deposits associated with the Absaroka volcanic province along the eastern and northern boundaries of Yellowstone National Park. The left panel shows the spread of the Absaroka Volcanic Supergroup (AVS) throughout Wyoming and Montana.
Volcanic deposits associated with the Absaroka volcanic province along the eastern and northern boundaries of Yellowstone National Park
Volcanic deposits associated with the Absaroka volcanic province along the eastern and northern boundaries of Yellowstone National ParkVolcanic deposits associated with the Absaroka volcanic province along the eastern and northern boundaries of Yellowstone National Park. The left panel shows the spread of the Absaroka Volcanic Supergroup (AVS) throughout Wyoming and Montana.
Isotopic composition of units within the Absaroka volcanic province
Isotopic composition of units within the Absaroka volcanic provinceIsotopic composition of the primary volcanic groups of the Absaroka volcanic province (the Washburn, Sunlight, and Thorofare groups) and two volcaniclastic units, the Sepulcher formation and the Daly formation.
Isotopic composition of units within the Absaroka volcanic province
Isotopic composition of units within the Absaroka volcanic provinceIsotopic composition of the primary volcanic groups of the Absaroka volcanic province (the Washburn, Sunlight, and Thorofare groups) and two volcaniclastic units, the Sepulcher formation and the Daly formation.
Landsat 8 nighttime thermal infrared image of Yellowstone National Park from January 31, 2023
Landsat 8 nighttime thermal infrared image of Yellowstone National Park from January 31, 2023Landsat 8 nighttime thermal infrared image of Yellowstone National Park from January 31, 2023. Satellite-based thermal infrared data show areas on the surface that are warmer versus cooler, and they can be used to estimate surface temperature and the geothermal radiative heat output from the Yellowstone magmatic and hydrothermal system.
Landsat 8 nighttime thermal infrared image of Yellowstone National Park from January 31, 2023
Landsat 8 nighttime thermal infrared image of Yellowstone National Park from January 31, 2023Landsat 8 nighttime thermal infrared image of Yellowstone National Park from January 31, 2023. Satellite-based thermal infrared data show areas on the surface that are warmer versus cooler, and they can be used to estimate surface temperature and the geothermal radiative heat output from the Yellowstone magmatic and hydrothermal system.
Geology of the unconformity on Mount Everts in Yellowstone National Park
Geology of the unconformity on Mount Everts in Yellowstone National ParkGeology of the unconformity on Mount Everts in Yellowstone National Park. Sketch at the top was made by geologist William Henry Holmes in 1878 and correctly identifies Cretaceous sediments overlain by much younger rhyolite rocks, including fine ash deposits (“tufa”). The photo at the bottom shows the same outcrop as viewed from Mammoth Hot Springs (USGS
Geology of the unconformity on Mount Everts in Yellowstone National Park
Geology of the unconformity on Mount Everts in Yellowstone National ParkGeology of the unconformity on Mount Everts in Yellowstone National Park. Sketch at the top was made by geologist William Henry Holmes in 1878 and correctly identifies Cretaceous sediments overlain by much younger rhyolite rocks, including fine ash deposits (“tufa”). The photo at the bottom shows the same outcrop as viewed from Mammoth Hot Springs (USGS
Plot of Yellowstone Lake level in June 13, 2021, showing a repeating seiche wave
Plot of Yellowstone Lake level in June 13, 2021, showing a repeating seiche waveAn example of the repeating seiche—a long-period oscillatory wave that can be present on a lake—measured over the course of a day by the lake-level sensor at the Grant Village boat dock on the West Thumb of Yellowstone Lake. The plot shows a cyclic variation of about 2 centimeters that occurs numerous times during June 13, 2021.
Plot of Yellowstone Lake level in June 13, 2021, showing a repeating seiche wave
Plot of Yellowstone Lake level in June 13, 2021, showing a repeating seiche waveAn example of the repeating seiche—a long-period oscillatory wave that can be present on a lake—measured over the course of a day by the lake-level sensor at the Grant Village boat dock on the West Thumb of Yellowstone Lake. The plot shows a cyclic variation of about 2 centimeters that occurs numerous times during June 13, 2021.
SP Crater in the San Francisco volcanic field of northern Arizona
SP Crater in the San Francisco volcanic field of northern ArizonaSP Crater (right foreground), like many volcanoes in Arizona’s San Francisco volcanic field, erupted mafic lava that lacks sanidine crystals.
SP Crater in the San Francisco volcanic field of northern Arizona
SP Crater in the San Francisco volcanic field of northern ArizonaSP Crater (right foreground), like many volcanoes in Arizona’s San Francisco volcanic field, erupted mafic lava that lacks sanidine crystals.
Map of arsenic concentrations in Yellowstone National Park rivers
Map of arsenic concentrations in Yellowstone National Park riversMap of Yellowstone National Park lakes, rivers, and streams, with colors indicating the amount of arsenic in the water. The Maximum Contaminant Level (MCL) defined by the Environmental Protection Agency for arsenic in drinking water is 10 micrograms per liter (µg/L). In the vicinity of major geyser basins, especially on the Firehole and Madison Rivers, a
Map of arsenic concentrations in Yellowstone National Park rivers
Map of arsenic concentrations in Yellowstone National Park riversMap of Yellowstone National Park lakes, rivers, and streams, with colors indicating the amount of arsenic in the water. The Maximum Contaminant Level (MCL) defined by the Environmental Protection Agency for arsenic in drinking water is 10 micrograms per liter (µg/L). In the vicinity of major geyser basins, especially on the Firehole and Madison Rivers, a
Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National Park
Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National ParkPie diagram showing the chloride flux, in kilotons per year (kt/yr), measured in 2022, with percentages for the four major rivers (Madison, Yellowstone, Snake, and Falls rivers) that drain Yellowstone National Park. Figure developed by Baine McCleskey.
Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National Park
Pie diagram showing chloride flux measured in 2022 in rivers of Yellowstone National ParkPie diagram showing the chloride flux, in kilotons per year (kt/yr), measured in 2022, with percentages for the four major rivers (Madison, Yellowstone, Snake, and Falls rivers) that drain Yellowstone National Park. Figure developed by Baine McCleskey.
Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park
Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National ParkImages of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park. A, WorldView-3 satellite image from September 2014. B, National Park Service (NPS) aerial photograph from 2017. Images A and B were acquired before the feature went largely dry in late 2019 or 2020. C, WorldView-3 satellite image from June 2020.
Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park
Images of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National ParkImages of an unnamed thermal feature in the Three River Junction thermal area in southwest Yellowstone National Park. A, WorldView-3 satellite image from September 2014. B, National Park Service (NPS) aerial photograph from 2017. Images A and B were acquired before the feature went largely dry in late 2019 or 2020. C, WorldView-3 satellite image from June 2020.
Map of seismicity (red circles) in the Yellowstone region during 2022. 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.
Map of seismicity (red circles) in the Yellowstone region during 2022. 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.
3D rendering of the shear-wave-speed anomaly below Yellowstone
3D rendering of the shear-wave-speed anomaly below Yellowstone3D rendering of the shear-wave-speed anomaly (ɗVS) below Yellowstone. Regions of strongly reduced shear-wave speed most likely indicate volumes of partially molten crust. Iso-surfaces (surfaces of constant ɗVS) are shown in increments of 5%.
3D rendering of the shear-wave-speed anomaly below Yellowstone
3D rendering of the shear-wave-speed anomaly below Yellowstone3D rendering of the shear-wave-speed anomaly (ɗVS) below Yellowstone. Regions of strongly reduced shear-wave speed most likely indicate volumes of partially molten crust. Iso-surfaces (surfaces of constant ɗVS) are shown in increments of 5%.
Seismic data coverage of the Yellowstone region and example of seismic noise records
Seismic data coverage of the Yellowstone region and example of seismic noise recordsSeismic data coverage of the Yellowstone region and example of seismic noise records. By cross-correlating signals of the background noise recorded at two seismic stations and stacking the signals over many days, useful seismic waveforms can be extracted.
Seismic data coverage of the Yellowstone region and example of seismic noise records
Seismic data coverage of the Yellowstone region and example of seismic noise recordsSeismic data coverage of the Yellowstone region and example of seismic noise records. By cross-correlating signals of the background noise recorded at two seismic stations and stacking the signals over many days, useful seismic waveforms can be extracted.
Google Earth image of the north part of Lower Geyser Basin, Yellowstone National Park, showing the site of the Fountain Hotel
Google Earth image of the north part of Lower Geyser Basin, Yellowstone National Park, showing the site of the Fountain HotelGoogle Earth image of the north part of Lower Geyser Basin showing the site of the Fountain Hotel and nearby Leather Pool, which was tapped to provide a source of hot water for the hotel.
Google Earth image of the north part of Lower Geyser Basin, Yellowstone National Park, showing the site of the Fountain Hotel
Google Earth image of the north part of Lower Geyser Basin, Yellowstone National Park, showing the site of the Fountain HotelGoogle Earth image of the north part of Lower Geyser Basin showing the site of the Fountain Hotel and nearby Leather Pool, which was tapped to provide a source of hot water for the hotel.
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National Park
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National ParkGraph showing the discharge (blue) and specific conductance (black) measured at the Gardner River monitoring station in Yellowstone National Park during the June 10–13, 2022, flood.
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National Park
Discharge and specific conductance measured in June 2022 at the Gardner River, Yellowstone National ParkGraph showing the discharge (blue) and specific conductance (black) measured at the Gardner River monitoring station in Yellowstone National Park during the June 10–13, 2022, flood.
Map of southern Idaho and the Snake River Plain, showing the eastern (ESRP) and western (WSRP) parts of the geologic province. Map by Zach Lifton, Idaho Geological Survey.
Map of southern Idaho and the Snake River Plain, showing the eastern (ESRP) and western (WSRP) parts of the geologic province. Map by Zach Lifton, Idaho Geological Survey.
Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage SitesJamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites during the 60th anniversary IUGS meeting in Zumaia, Spain in October, 2022. Photo by Marjorie Chan.
Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Jamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage SitesJamie Farrell presents Yellowstone as one of the first 100 IUGS Geological Heritage Sites during the 60th anniversary IUGS meeting in Zumaia, Spain in October, 2022. Photo by Marjorie Chan.
Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage SitesDocument certifying The Yellowstone Volcanic and Hydrothermal System, USA, as one of the first 100 IUGS Geological Heritage Sites as declared during the 60th anniversary IUGS meeting held in Zumaia, Spain in October 2022.
Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage Sites
Certificate for Yellowstone as one of the first 100 IUGS Geological Heritage SitesDocument certifying The Yellowstone Volcanic and Hydrothermal System, USA, as one of the first 100 IUGS Geological Heritage Sites as declared during the 60th anniversary IUGS meeting held in Zumaia, Spain in October 2022.
Wapi lava shield, eastern Snake River Plain, Idaho
Wapi lava shield, eastern Snake River Plain, IdahoLow shield volcano that was the source of the Wapi lava flow on the eastern Snake River Plain of Idaho. Photo my Michael Ort, October 14, 2022.
Wapi lava shield, eastern Snake River Plain, Idaho
Wapi lava shield, eastern Snake River Plain, IdahoLow shield volcano that was the source of the Wapi lava flow on the eastern Snake River Plain of Idaho. Photo my Michael Ort, October 14, 2022.