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Images of Yellowstone.

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Looking west from the intersection of U.S. Route 20 and Old Hwy 47, in Idaho, at lava flows associated with the Henrys Fork caldera
Looking west from the intersection of U.S. Route 20 and Old Hwy 47, in Idaho, at lava flows associated with the Henrys Fork caldera
Looking west from the intersection of U.S. Route 20 and Old Hwy 47, in Idaho, at lava flows associated with the Henrys Fork caldera
Looking west from the intersection of U.S. Route 20 and Old Hwy 47, in Idaho, at lava flows associated with the Henrys Fork caldera

Google Maps photo taken at the intersection of U.S. Route 20 and Old Hwy 47 in Idaho, looking west. The tops of Moonshine Mountain and Silver Lake dome, rhyolite lava flows located inside the caldera, are indicated with a dashed black line.

USGS employees deploys a water conductivity/temperature/depth probe...
USGS employees deploys a water conductivity/temperature/depth probe...
USGS employees deploys a water conductivity/temperature/depth probe...
USGS employees deploys a water conductivity/temperature/depth probe...

USGS employees deploys a water conductivity/temperature/depth probe (AquaTroll) for a temporary study along the Madison River, Yellowstone.

Helicorder for Plate Boundary Observatory borehole seismometer
Helicorder for Plate Boundary Observatory borehole seismometer B207...
Helicorder for Plate Boundary Observatory borehole seismometer B207...
Helicorder for Plate Boundary Observatory borehole seismometer B207...

Seismicity is shown for January 17, 2010 through the Feb 8, 2010. Borehole seismometer B207 is located about 7 miles (12 km) northeast of the 2010 swarm. Seismic data are provided by the National Science Foundation funded Plate Boundary Observatory operated by UNAVCO.

Seismicity is shown for January 17, 2010 through the Feb 8, 2010. Borehole seismometer B207 is located about 7 miles (12 km) northeast of the 2010 swarm. Seismic data are provided by the National Science Foundation funded Plate Boundary Observatory operated by UNAVCO.

National Park Service employee inspects a Plate Boundary Observator...
NPS inspects Plate Boundary Observatory strainmeter/seismometer
NPS inspects Plate Boundary Observatory strainmeter/seismometer
NPS inspects Plate Boundary Observatory strainmeter/seismometer

National Park Service employee inspects a Plate Boundary Observatory strainmeter/seismometer station.

Two elk standing in from of burned trees, with a lake shoreline in the distance under a cloudy sky
Image of elk captured by the YVO mobile webcam on June 25, 2010
Image of elk captured by the YVO mobile webcam on June 25, 2010
Image of elk captured by the YVO mobile webcam on June 25, 2010

Image of elk captured by the YVO mobile webcam on June 25, 2010, when it was positioned atop Lake Butte with a view of the north side of Yellowstone Lake.

Cross section through the trunk of a Yellowstone lodgepole pine
Cross section through the trunk of a Yellowstone lodgepole pine
Cross section through the trunk of a Yellowstone lodgepole pine
Cross section through the trunk of a Yellowstone lodgepole pine

Cross section through the trunk of a lodgepole pine tree from Cooking Hillside near Mud Volcano, Yellowstone National Park.  The earliest date for this tree is 1916 and it died in 1990. Spongy white-gray areas are foam insulation that was injected into the sample to reinforce the structure of the wood.

Cross section through the trunk of a lodgepole pine tree from Cooking Hillside near Mud Volcano, Yellowstone National Park.  The earliest date for this tree is 1916 and it died in 1990. Spongy white-gray areas are foam insulation that was injected into the sample to reinforce the structure of the wood.

Temperature data is collected from this data logger that is placed ...
Temperature data is collected from this data logger that is placed ...
Temperature data is collected from this data logger that is placed ...
Temperature data is collected from this data logger that is placed ...

Data are collected every two minutes and sent by radio once per day to a server where values are plotted and released to the public internet.

Grey’s Landing Ignimbrite in Idaho part of Yellowstone Hotspot
Grey’s Landing Ignimbrite in Idaho part of Yellowstone Hotspot
Grey’s Landing Ignimbrite in Idaho part of Yellowstone Hotspot
Grey’s Landing Ignimbrite in Idaho part of Yellowstone Hotspot

The Grey’s Landing Ignimbrite in Idaho (Dr. Thomas Knott, of the University of Leicester, England, gives the scale of the cliff). The entire cliff (and more not seen!) would have been deposited in a matter of moments as it welded to the land surface during a super eruption about 8.7 million years ago.

The Grey’s Landing Ignimbrite in Idaho (Dr. Thomas Knott, of the University of Leicester, England, gives the scale of the cliff). The entire cliff (and more not seen!) would have been deposited in a matter of moments as it welded to the land surface during a super eruption about 8.7 million years ago.

Geysers on the south pole of Saturn's moon Enceladus
Geysers on the south pole of Saturn's moon Enceladus
Geysers on the south pole of Saturn's moon Enceladus
Geysers on the south pole of Saturn's moon Enceladus

This two-image mosaic is one of the highest resolution views acquired by the Cassini spacecraft during its imaging survey of the geyser basin capping the southern hemisphere of Saturn's moon Enceladus. 

This two-image mosaic is one of the highest resolution views acquired by the Cassini spacecraft during its imaging survey of the geyser basin capping the southern hemisphere of Saturn's moon Enceladus. 

Photo of the Madison Museum, Yellowstone National Park
Photo of the Madison Museum, Yellowstone National Park
Photo of the Madison Museum, Yellowstone National Park
Photo of the Madison Museum, Yellowstone National Park

Photo of the Madison Museum, built in 1930 and designed by Herbert Maier. This structure exemplifies the National Park Rustic style, using natural materials and artisan craftmanship that are intended to blend buildings into the surrounding environment, “suggesting the smallness of man in relation to nature” (Herbert Maier).

Photo of the Madison Museum, built in 1930 and designed by Herbert Maier. This structure exemplifies the National Park Rustic style, using natural materials and artisan craftmanship that are intended to blend buildings into the surrounding environment, “suggesting the smallness of man in relation to nature” (Herbert Maier).

Blue pools surrounded by beige and reddish mud and otherwise mostly barren ground. Pine trees and a lake are in the distance.
Overview of central West Thumb Geyser Basin
Overview of central West Thumb Geyser Basin
Overview of central West Thumb Geyser Basin

Overview of central West Thumb Geyser Basin.  USGS photo by Pat Shanks, 2009. 

Ken Pierce in the field with a large glacial erratic
Ken Pierce in the field with large glacial erratic
Ken Pierce in the field with large glacial erratic
Ken Pierce in the field with large glacial erratic

Ken Pierce in the field with a large glacial erratic in the Clarks Fork moraines taking detailed notes and annotating a map in progress.

Ken Pierce in the field with a large glacial erratic in the Clarks Fork moraines taking detailed notes and annotating a map in progress.

Bob Fournier measuring the gas-to-water ratio (gas/steam) at drill site Y2 in Yellowstone National Park
Bob Fournier measuring the gas-to-water ratio (gas/steam) at drill site Y2 in Yellowstone National Park
Bob Fournier measuring the gas-to-water ratio (gas/steam) at drill site Y2 in Yellowstone National Park
Bob Fournier measuring the gas-to-water ratio (gas/steam) at drill site Y2 in Yellowstone National Park

Bob Fournier measuring the gas-to-water ratio (gas/steam) at drill site Y2, near Hot Lake on Firehole Lake Drive in Lower Geyser Basin, Yellowstone National Park, in the late 1960s.  USGS Photo.

View from a mountain of a treed area with a canyon in the middle ground and mountains in the distance. Sky is mostly cloudy.
Yellowstone caldera viewed from Mount Washburn
Yellowstone caldera viewed from Mount Washburn
Yellowstone caldera viewed from Mount Washburn

Yellowstone caldera viewed from Mount Washburn.  The caldera is the low-lying area extending from the foothills of Mount Washburn in the foreground to the rugged mountains on the horizon.  The incised valley of the Yellowstone River stretches from left to right in the middle distance.  Steep valley walls are illuminated by sunlight in the center.&nbsp

Yellowstone caldera viewed from Mount Washburn.  The caldera is the low-lying area extending from the foothills of Mount Washburn in the foreground to the rugged mountains on the horizon.  The incised valley of the Yellowstone River stretches from left to right in the middle distance.  Steep valley walls are illuminated by sunlight in the center.&nbsp

Hydrothermal explosion at Biscuit Basin in Yellowstone National Par...
Hydrothermal explosion at Biscuit Basin in YNP. These types of even...
Hydrothermal explosion at Biscuit Basin in YNP. These types of even...
Hydrothermal explosion at Biscuit Basin in YNP. These types of even...

Hydrothermal explosion at Biscuit Basin in Yellowstone National Park. These types of events are the most likely explosive hazard from the Yellowstone Volcano.

Schematic illustration of waterfall formation
Schematic illustration of waterfall formation
Schematic illustration of waterfall formation
Schematic illustration of waterfall formation

Schematic illustration of waterfall formation in which a hard rock that is more resistant to erosion is atop a softer rock that is less resistant to erosion. Source: Wikimedia (https://commons.wikimedia.org/wiki/File:WaterfallCreationDiagram.svg).

Installing geophysical boreholes in Yellowstone
Installing geophysical boreholes in Yellowstone
Installing geophysical boreholes in Yellowstone
Installing geophysical boreholes in Yellowstone

UNAVCO engineers drilling a borehole for instrument installation (left). Aerial view of borehole casing used to protect instruments from the elements found below the surface (right).

UNAVCO engineers drilling a borehole for instrument installation (left). Aerial view of borehole casing used to protect instruments from the elements found below the surface (right).

Gas flows up, appearing to boil, through the water of Alluvium Cree...
Gas flows up, appearing to boil, through the water of Alluvium Cree...
Gas flows up, appearing to boil, through the water of Alluvium Cree...
Gas flows up, appearing to boil, through the water of Alluvium Cree...

Gas flows up, appearing to boil, through the water of Alluvium Creek, Brimstone Basin, Yellowstone. Large funnel is used to trap gas, which is then sent to a collection bottle through the tubing.

Terrace Springs, northeast of Madison Junction, Yellowstone National Park
Terrace Springs, northeast of Madison Junction, Yellowstone National Park
Terrace Springs, northeast of Madison Junction, Yellowstone National Park
Terrace Springs, northeast of Madison Junction, Yellowstone National Park

The water at Terrace Springs, northeast of Madison Junction in Yellowstone National Park, is relatively cold (about 60 °C or 140 °F), but the water is still saturated with CO2-rich bubbles. Photo by Shaul Hurwitz in September 2008.

The water at Terrace Springs, northeast of Madison Junction in Yellowstone National Park, is relatively cold (about 60 °C or 140 °F), but the water is still saturated with CO2-rich bubbles. Photo by Shaul Hurwitz in September 2008.

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