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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.

Gray flowage deposit on white ground, with lodgepole pine trees and blue sky in the background
Sulfur flow at Brimstone Basin, Yellowstone National Park
Sulfur flow at Brimstone Basin, Yellowstone National Park
Sulfur flow at Brimstone Basin, Yellowstone National Park

A sulfur flow over acid-sulfate ground at Brimstone Basin near the eastern shore of Yellowstone Lake. The flows formed when native sulfur deposits were ignited during a forest fire. Photo by Shaul Hurwitz, September 2008.

A sulfur flow over acid-sulfate ground at Brimstone Basin near the eastern shore of Yellowstone Lake. The flows formed when native sulfur deposits were ignited during a forest fire. Photo by Shaul Hurwitz, September 2008.

Pink roadcut about 20 feet nigh. Lodgepole pines are atop the roadcut, and the sky is mostly blue with thin whispy clouds.
Roadcut in the Lava Creek Tuff near Tuff Cliff, Yellowstone National Park
Roadcut in the Lava Creek Tuff near Tuff Cliff, Yellowstone National Park
Roadcut in the Lava Creek Tuff near Tuff Cliff, Yellowstone National Park

Roadcut in light pink ash-flow deposits of the Lava Creek Tuff on Grand Loop Road near Tuff Cliff.  The color and closely spaced jointing are characteristic of the Lava Creek Tuff map unit.  The steep faces and dense nature of the roadcut exposures indicate that a moderate degree of welding occurred and has not been subsequently modified by hydrothermal al

Roadcut in light pink ash-flow deposits of the Lava Creek Tuff on Grand Loop Road near Tuff Cliff.  The color and closely spaced jointing are characteristic of the Lava Creek Tuff map unit.  The steep faces and dense nature of the roadcut exposures indicate that a moderate degree of welding occurred and has not been subsequently modified by hydrothermal al

Waterfall in the distance that feeds a roaring river in a steep canyon with pale beige/yellow/red walls under a blue sky.
Lower Falls and Grand Canyon of the Yellowstone River
Lower Falls and Grand Canyon of the Yellowstone River
Lower Falls and Grand Canyon of the Yellowstone River

Lower Falls and Grand Canyon of the Yellowstone River.  The river here is eroding young, post-caldera rhyolite that was softened by hydrothermal alteration.  The V shape of the canyon indicates that the river is actively eroding in response to regional uplift.  Photo by Richard Tollo, George Washington University, August 12, 2008.

Lower Falls and Grand Canyon of the Yellowstone River.  The river here is eroding young, post-caldera rhyolite that was softened by hydrothermal alteration.  The V shape of the canyon indicates that the river is actively eroding in response to regional uplift.  Photo by Richard Tollo, George Washington University, August 12, 2008.

Narrow Gauge spring, Mammoth Hot Springs, Yellowstone National Park
Narrow Gauge spring, Mammoth Hot Springs, Yellowstone National Park
Narrow Gauge spring, Mammoth Hot Springs, Yellowstone National Park
Narrow Gauge spring, Mammoth Hot Springs, Yellowstone National Park

Narrow Gauge spring, Mammoth Hot Springs, Yellowstone National Park.  Vent area is between the two trees on top of the travertine deposits.  Terraced pools form due to deposition of travertine from the fluids as they cool and degas carbon dioxide.

Narrow Gauge spring, Mammoth Hot Springs, Yellowstone National Park.  Vent area is between the two trees on top of the travertine deposits.  Terraced pools form due to deposition of travertine from the fluids as they cool and degas carbon dioxide.

GPS antenna and solar panel in a lightly wooded area under partly cloudy skies
GPS station P714 in Panther Meadow, Yellowstone National Park
GPS station P714 in Panther Meadow, Yellowstone National Park
GPS station P714 in Panther Meadow, Yellowstone National Park

GPS station P714, located in Panther Meadow south of Mammoth Hot Springs in Yellowstone National Park. Photo by EarthScope Consortium, June 2008.

Bison standing in the snow
Bison being fed on the National Elk Refuge
Bison being fed on the National Elk Refuge
Bison being fed on the National Elk Refuge

Supplemental feeding of bison on the National Elk Refuge, Wyoming in February 2008.

Bison standing in the snow
Bison being fed on the National Elk Refuge
Bison being fed on the National Elk Refuge
Bison being fed on the National Elk Refuge

Supplemental feeding of bison on the National Elk Refuge, Wyoming in February 2008.

Elk and bison standing in the snow
Elk and bison being fed on the National Elk Refuge
Elk and bison being fed on the National Elk Refuge
Elk and bison being fed on the National Elk Refuge

Elk and bison being fed on the National Elk Refuge, Wyoming. Grand Teton and Grand Teton National Park are in the background.

Aerial view of the National Elk Refuge
Aerial view of the National Elk Refuge
Aerial view of the National Elk Refuge
Aerial view of the National Elk Refuge

Aerial view of the National Elk Refuge (left) and the town of Jackson, Wyoming (right) in 2007.

Eruption of Daisy Geyser, Yellowstone National Park
Eruption of Daisy Geyser, Yellowstone National Park
Eruption of Daisy Geyser, Yellowstone National Park
Eruption of Daisy Geyser, Yellowstone National Park

An eruption of Daisy Geyser in the Upper Geyser Basin of Yellowstone National Park. The geyser erupts boiling water at about 93 °C (200 °F). Photo by Shaul Hurwitz on April 12, 2007.

An eruption of Daisy Geyser in the Upper Geyser Basin of Yellowstone National Park. The geyser erupts boiling water at about 93 °C (200 °F). Photo by Shaul Hurwitz on April 12, 2007.

Air photo showing newly thermal areas on Mallard Lake resurgent dome
Air photo showing newly thermal areas on Mallard Lake resurgent dome
Air photo showing newly thermal areas on Mallard Lake resurgent dome
Air photo showing newly thermal areas on Mallard Lake resurgent dome

National Agriculture Imagery Program natural-color image from September 9, 2006, showing newly mapped thermal areas (outlined in yellow) on the north side of the Mallard Lake resurgent dome.

Upper Lebo Member of the Fort Union Formation near Gillette, Wyoming
Upper Lebo Member of the Fort Union Formation near Gillette, Wyoming
Upper Lebo Member of the Fort Union Formation near Gillette, Wyoming
Upper Lebo Member of the Fort Union Formation near Gillette, Wyoming

Upper Lebo Member of the Fort Union Formation. Photo taken fro the top of Cow Creek Buttes in the Burnt Hollow BLM recreation area about 20 miles northeast of Gillette, Wyoming.

Tamarisk growing along a river
A single species stand of nonnative tamarisk
A single species stand of nonnative tamarisk
A single species stand of nonnative tamarisk

Single species stand of nonnative tamarisk on the Lower Colorado River at Cibola National Wildlife Refuge, California

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