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Images of Yellowstone.

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Visible and thermal maps of Brimstone Basin (top) and Midway / Lower Geyser Basins (bottom).
Visible/thermal maps of Brimstone Basin & Midway/Lower Geyser Basins
Visible/thermal maps of Brimstone Basin & Midway/Lower Geyser Basins
Visible/thermal maps of Brimstone Basin & Midway/Lower Geyser Basins

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
Outline of the Steamboat and Cistern plumbing systems from seismicity
Outline of the Steamboat and Cistern plumbing systems from seismicity
Outline of the Steamboat and Cistern plumbing systems from seismicity

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
Seismic view of Steamboat Geyser and Cistern Spring
Seismic view of Steamboat Geyser and Cistern Spring
Seismic view of Steamboat Geyser and Cistern Spring

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
Crinoid fossil from northern Yellowstone National Park
Crinoid fossil from northern Yellowstone National Park
Crinoid fossil from 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
Example of new layers in the Geology of Yellowstone Map
Example of new layers in the Geology of Yellowstone Map
Example of new layers in the Geology of Yellowstone Map

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 data available from online Geology of Yellowstone Map
Seismic data available from online Geology of Yellowstone Map
Seismic data available from online Geology of Yellowstone Map
Seismic data available from online Geology of Yellowstone Map

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
Rhyolite alteration viewed by a Scanning Electron Microscope
Rhyolite alteration viewed by a Scanning Electron Microscope
Rhyolite alteration viewed by a Scanning Electron Microscope

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 near Mud Volcano in Yellowstone National Park
Mudpot located near Mud Volcano in Yellowstone National Park
Mudpot located near Mud Volcano in Yellowstone National Park
Mudpot located near Mud Volcano in Yellowstone National Park

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
Steam vents along the Yellowstone River near Mud Volcano thermal area
Steam vents along the Yellowstone River near Mud Volcano thermal area
Steam vents along the Yellowstone River near Mud Volcano thermal area

Steam vents along the Yellowstone River near Mud Volcano thermal area, Yellowstone National Park.

Columbia River Basalts seen at Steens Mountain, Oregon
Columbia River Basalts seen at Steens Mountain, Oregon
Columbia River Basalts seen at Steens Mountain, Oregon
Columbia River Basalts seen at Steens Mountain, Oregon

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

Thermal anomaly map of Yellowstone National Park based on a Landsat 8 nighttime thermal infrared image from 9 January 2021
Thermal anomaly map of Yellowstone National Park based on a Landsat 8 nighttime thermal infrared image from 9 January 2021
Thermal anomaly map of Yellowstone National Park based on a Landsat 8 nighttime thermal infrared image from 9 January 2021
Thermal anomaly map of Yellowstone National Park based on a Landsat 8 nighttime thermal infrared image from 9 January 2021

Thermal 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.  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.

Eruptions of Steamboat Geyser over time
Eruptions of Steamboat Geyser over time
Eruptions of Steamboat Geyser over time
Eruptions of Steamboat Geyser over time

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
Steamboat Geyser eruption signals
Steamboat Geyser eruption signals
Steamboat Geyser eruption signals

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
Map of seismicity in the Yellowstone region during 2020
Map of seismicity in the Yellowstone region during 2020
Map of seismicity in the Yellowstone region during 2020

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
Section from the piston core YL92-1C, collected in south-central Yellowstone Lake
Section from the piston core YL92-1C, collected in south-central Yellowstone Lake
Section from the piston core YL92-1C, collected in south-central Yellowstone Lake

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
Satellite view of Ngorongoro volcano, in Tanzania, east Africa
Satellite view of Ngorongoro volcano, in Tanzania, east Africa
Satellite view of Ngorongoro volcano, in Tanzania, east Africa

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.

Absolute versus relative earthquake locations associated with 2019 Ridgecrest, California, foreshock and aftershock sequence
Absolute versus relative earthquake locations associated with 2019 Ridgecrest, California, foreshock and aftershock sequence
Absolute versus relative earthquake locations associated with 2019 Ridgecrest, California, foreshock and aftershock sequence
Absolute versus relative earthquake locations associated with 2019 Ridgecrest, California, foreshock and aftershock sequence

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. 

Experimental apparatus for reacting hot water and rhyolite
Experimental apparatus for reacting hot water and rhyolite
Experimental apparatus for reacting hot water and rhyolite
Experimental apparatus for reacting hot water and rhyolite

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).

Determining the height of a geyser eruption with trigonometry
Determining the height of a geyser eruption with trigonometry
Determining the height of a geyser eruption with trigonometry
Determining the height of a geyser eruption with trigonometry

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.

Swath bathymetric image of the Elliott’s Crater explosion crater in Yellowstone Lake
Swath bathymetric image of the Elliott’s Crater explosion crater
Swath bathymetric image of the Elliott’s Crater explosion crater
Swath bathymetric image of the Elliott’s Crater explosion crater

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.

Scanning electron microscope image of Yellowstone drill core
Scanning electron microscope image of Yellowstone drill core
Scanning electron microscope image of Yellowstone drill core
Scanning electron microscope image of Yellowstone drill core

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.