Lava Mountain, Wyoming. (A) View from Dubois, WY, in the Wind River basin looking northwest ~30 km toward Lava Mountain.
Images
Lava Mountain, Wyoming. (A) View from Dubois, WY, in the Wind River basin looking northwest ~30 km toward Lava Mountain.
View into Green River Basin from Wyoming Range, Dry Piney Basin
View into Green River Basin from Wyoming Range, Dry Piney BasinView into Green River Basin from Wyoming Range, Dry Piney Basin
View into Green River Basin from Wyoming Range, Dry Piney Basin
View into Green River Basin from Wyoming Range, Dry Piney BasinView into Green River Basin from Wyoming Range, Dry Piney Basin
Installing piezometer on the bank of the New Fork River
Installing piezometer on the bank of the New Fork RiverInstalling piezometer on the bank of the New Fork River
Installing piezometer on the bank of the New Fork River
Installing piezometer on the bank of the New Fork RiverInstalling piezometer on the bank of the New Fork River
Confluence of New Fork (foreground) and Green Rivers
Confluence of New Fork (foreground) and Green RiversConfluence of New Fork (foreground) and Green Rivers
Confluence of New Fork (foreground) and Green Rivers
Confluence of New Fork (foreground) and Green RiversConfluence of New Fork (foreground) and Green Rivers
Bull elk in Grand Teton National Park, Wyoming.
Bull elk in Grand Teton National Park, Wyoming.
Installing stream thermistor at New Fork Groundwater Streamgage
Installing stream thermistor at New Fork Groundwater StreamgageInstalling stream thermistor at New Fork Groundwater Streamgage
Installing stream thermistor at New Fork Groundwater Streamgage
Installing stream thermistor at New Fork Groundwater StreamgageInstalling stream thermistor at New Fork Groundwater Streamgage
Mud Pot within the Mud Volcano thermal area of Yellowstone National Park
Mud Pot within the Mud Volcano thermal area of Yellowstone National ParkA mud pot in the Obsidian Pool Thermal Area, near Mud Volcano. The large amounts of suspended sediment make the thermal water much more viscous than pure water. Photo by Shaul Hurwitz, September 2014.
Mud Pot within the Mud Volcano thermal area of Yellowstone National Park
Mud Pot within the Mud Volcano thermal area of Yellowstone National ParkA mud pot in the Obsidian Pool Thermal Area, near Mud Volcano. The large amounts of suspended sediment make the thermal water much more viscous than pure water. Photo by Shaul Hurwitz, September 2014.
Little Powder River above Dry Week, near Weston, Wyoming
Little Powder River above Dry Week, near Weston, WyomingLittle Powder River above Dry Week, near Weston, Wyoming
Little Powder River above Dry Week, near Weston, Wyoming
Little Powder River above Dry Week, near Weston, WyomingLittle Powder River above Dry Week, near Weston, Wyoming
Flowing well used for stock water, Green River Basin
Flowing well used for stock water, Green River BasinFlowing well used for stock water, Green River Basin
Flowing well used for stock water, Green River Basin
Flowing well used for stock water, Green River BasinFlowing well used for stock water, Green River Basin
Windmill and cattle near Big Piney
Wind turbines working in Wyoming.
Wind turbines working in Wyoming.
Blue pool of boiling water at Beryl Springs, Yellowstone National Park
Blue pool of boiling water at Beryl Springs, Yellowstone National ParkBeryl Spring's strongly boiling blue pool is about 8 m (25 ft) wide and contains high-chloride liquid water with a near-neutral pH. Immediately behind the pool is a loud, hissing fumarole producing a white cloud of steam. USGS Photo by Pat Shanks, 2002.
Blue pool of boiling water at Beryl Springs, Yellowstone National Park
Blue pool of boiling water at Beryl Springs, Yellowstone National ParkBeryl Spring's strongly boiling blue pool is about 8 m (25 ft) wide and contains high-chloride liquid water with a near-neutral pH. Immediately behind the pool is a loud, hissing fumarole producing a white cloud of steam. USGS Photo by Pat Shanks, 2002.
Looking upstream from bridge, Tongue river, Monarch
Looking upstream from bridge, Tongue river, MonarchLooking upstream from bridge, Tongue river, Monarch
Ice jam, Powder River near Arvada (06317000)
When looking for a place to set up a capture location, biologists look for existing bear sign such as scratches on trees and bear scat. Sometimes traps are set in areas that have no obvious bear sign to determine if indeed bears are present.
When looking for a place to set up a capture location, biologists look for existing bear sign such as scratches on trees and bear scat. Sometimes traps are set in areas that have no obvious bear sign to determine if indeed bears are present.
Photo of the Old Faithful Inn lobby, which features a six-story-tall fireplace and chimney made from rocks quarried form a rhyolite lava flow in Yellowstone. NPS photo by Jim Peaco, July 22, 2013.
Photo of the Old Faithful Inn lobby, which features a six-story-tall fireplace and chimney made from rocks quarried form a rhyolite lava flow in Yellowstone. NPS photo by Jim Peaco, July 22, 2013.
Image of Biscuit Basin (visible between the trees) captured by the YVO mobile webcam on June 17, 2012
Image of Biscuit Basin (visible between the trees) captured by the YVO mobile webcam on June 17, 2012Image of Biscuit Basin (visible between the trees) captured by the YVO mobile webcam on June 17, 2012, when it was positioned on a hill just east of the basin.
Image of Biscuit Basin (visible between the trees) captured by the YVO mobile webcam on June 17, 2012
Image of Biscuit Basin (visible between the trees) captured by the YVO mobile webcam on June 17, 2012Image of Biscuit Basin (visible between the trees) captured by the YVO mobile webcam on June 17, 2012, when it was positioned on a hill just east of the basin.
map of historic and current sage-grouse range in 2000
map of historic and current sage-grouse range in 2000Map of historic and current sage-grouse range in 2000, provided as a download from the old USGS Sagemap website.
map of historic and current sage-grouse range in 2000
map of historic and current sage-grouse range in 2000Map of historic and current sage-grouse range in 2000, provided as a download from the old USGS Sagemap website.
Sulfur “cinder” from Cinder Pool in Norris Geyser Basin, Yellowstone National Park
Sulfur “cinder” from Cinder Pool in Norris Geyser Basin, Yellowstone National ParkSulfur “cinder” attached to a sampling tube that was extracted from Cinder Pool in Norris Geyser Basin. The “cinder” is sulfur that existed as a molten layer at the bottom of the pool and was carried upward by gas and solidified. The black color is due to the presence of finely dispersed pyrite.
Sulfur “cinder” from Cinder Pool in Norris Geyser Basin, Yellowstone National Park
Sulfur “cinder” from Cinder Pool in Norris Geyser Basin, Yellowstone National ParkSulfur “cinder” attached to a sampling tube that was extracted from Cinder Pool in Norris Geyser Basin. The “cinder” is sulfur that existed as a molten layer at the bottom of the pool and was carried upward by gas and solidified. The black color is due to the presence of finely dispersed pyrite.