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Trade winds blow gas plume from Halema‘uma‘u to the southwest, Kīla...
Trade winds blow gas plume from Halema‘uma‘u to SW, Kīlauea
Trade winds blow gas plume from Halema‘uma‘u to SW, Kīlauea
Trade winds blow gas plume from Halema‘uma‘u to SW, Kīlauea

Gas plume rising from the new Overlook Vent in Halema‘uma‘u Crater, Kīlauea Volcano, Hawai‘i. Trade winds blow the plume to the southwest.

Advisory to drivers during high concentrations of sulfur dioxide ga...
Advisory to drivers during high concentrations of sulfur dioxide ga...
Advisory to drivers during high concentrations of sulfur dioxide ga...
Advisory to drivers during high concentrations of sulfur dioxide ga...

Road sign on Highway 11 advises drivers to roll up windows to protect themselves from high sulfur dioxide gas concentrations Kīlauea volcano on April 9, 2008. The temporary sign was put in place by Hawai‘i County Civil Defense, the agency responsible for public safety.

Road sign on Highway 11 advises drivers to roll up windows to protect themselves from high sulfur dioxide gas concentrations Kīlauea volcano on April 9, 2008. The temporary sign was put in place by Hawai‘i County Civil Defense, the agency responsible for public safety.

Volcanic-gas plume rises from Halema‘uma‘u Crater, Kīlauea Volcano,...
Volcanic-gas plume rises from Halema‘uma‘u, Kīlauea
Volcanic-gas plume rises from Halema‘uma‘u, Kīlauea
Volcanic-gas plume rises from Halema‘uma‘u, Kīlauea

A plume of volcanic gases (chiefly water vapor, carbon dioxide, and sulfur dioxide), tiny lava and rock particles, and droplets drifts southwest in the tradewinds from Halema‘uma‘u Crater.

A plume of volcanic gases (chiefly water vapor, carbon dioxide, and sulfur dioxide), tiny lava and rock particles, and droplets drifts southwest in the tradewinds from Halema‘uma‘u Crater.

Image: Prescribed Burn
Prescribed Burn
Prescribed Burn
Prescribed Burn

Iowa State Grad students Devan McGranahan and Torre Hovick, along with DNR private land specialist Josh Rusk and ISU Research Technician Shannon Rusk ignite a prescribed fire on a patch-burn grazing research pasture in southern Iowa.

Iowa State Grad students Devan McGranahan and Torre Hovick, along with DNR private land specialist Josh Rusk and ISU Research Technician Shannon Rusk ignite a prescribed fire on a patch-burn grazing research pasture in southern Iowa.

Ash-rich plume rising from Halema‘uma‘u Crater, Kīlauea Volcano 5 d...
Ash-rich plume rising from Halema‘uma‘u, Kīlauea 5 days after the f...
Ash-rich plume rising from Halema‘uma‘u, Kīlauea 5 days after the f...
Ash-rich plume rising from Halema‘uma‘u, Kīlauea 5 days after the f...

View of ash-rich plume rising from a new vent in Halema‘uma‘u Crater in Kīlauea Caldera 5 days after the first explosion from the vent occurred on March 19, 2008. The ash is turning the formerly white steam and gas plume a dusty-brown color. Note the ash fallout down-wind of the plume.

View of ash-rich plume rising from a new vent in Halema‘uma‘u Crater in Kīlauea Caldera 5 days after the first explosion from the vent occurred on March 19, 2008. The ash is turning the formerly white steam and gas plume a dusty-brown color. Note the ash fallout down-wind of the plume.

Flood of March 19, 2008, Buffalo River near St. Joe, Ark.
Flood of March 19, 2008 at Buffalo River, Ark.
Flood of March 19, 2008 at Buffalo River, Ark.
Flood of March 19, 2008 at Buffalo River, Ark.

B.K. Martin, hydrologic technician in the Little Rock office of the USGS Lower Mississippi-Gulf Water Science Center, measuring streamflow with an acoustic doppler current profiler during flood of March 19, 2008, at USGS streamflow-gaging station 07056000, Buffalo River near St. Joe, Arkansas. Photograph by W.E.

B.K. Martin, hydrologic technician in the Little Rock office of the USGS Lower Mississippi-Gulf Water Science Center, measuring streamflow with an acoustic doppler current profiler during flood of March 19, 2008, at USGS streamflow-gaging station 07056000, Buffalo River near St. Joe, Arkansas. Photograph by W.E.

Wooden fence on edge of Halema‘uma‘u Overlook area damaged by explo...
Wooden fence on edge of Halema‘uma‘u Overlook area damaged by explo...
Wooden fence on edge of Halema‘uma‘u Overlook area damaged by explo...
Wooden fence on edge of Halema‘uma‘u Overlook area damaged by explo...

The explosion occurred at 2:58 a.m. HST on March 19, 2008. The explosion scattered rock debris over an area of about 30 hectares (75 acres), covering a portion of Crater Rim Drive and damaging Halema‘uma‘u Overlook. The wooden fence of the overlook was bombarded by rocks hurled onto the rim of Halema‘uma‘u crater from the fumarolic area.

The explosion occurred at 2:58 a.m. HST on March 19, 2008. The explosion scattered rock debris over an area of about 30 hectares (75 acres), covering a portion of Crater Rim Drive and damaging Halema‘uma‘u Overlook. The wooden fence of the overlook was bombarded by rocks hurled onto the rim of Halema‘uma‘u crater from the fumarolic area.

Early morning view of fumarolic area at the base of eastern wall of...
Early morning view of fumarolic area at the base of eastern wall of...
Early morning view of fumarolic area at the base of eastern wall of...
Early morning view of fumarolic area at the base of eastern wall of...

This fumarolic area appeared on March 12, 2008. Gas is being emitted through rubble the Halema‘uma‘u Crater wall. The white fume is a mixture of condensed water vapor, sulfur trioxide, and invisible sulfur dioxide. The fume takes a pale bluish color if it contains very tiny sulfur particles (in center of fuming area).

This fumarolic area appeared on March 12, 2008. Gas is being emitted through rubble the Halema‘uma‘u Crater wall. The white fume is a mixture of condensed water vapor, sulfur trioxide, and invisible sulfur dioxide. The fume takes a pale bluish color if it contains very tiny sulfur particles (in center of fuming area).

Glass Mountain obsidian flow at Medicine Lake volcano, California....
Glass Mountain obsidian flow at Medicine Lake volcano, CA.
Glass Mountain obsidian flow at Medicine Lake volcano, CA.
Glass Mountain obsidian flow at Medicine Lake volcano, CA.

Glass Mountain obsidian flow at Medicine Lake volcano, California. Glass Mountain is a spectacular, nearly treeless, steep-sided rhyolite and dacite obsidian flow that erupted just outside the eastern caldera rim and flowed down the steep eastern flank of Medicine Lake volcano.

Glass Mountain obsidian flow at Medicine Lake volcano, California. Glass Mountain is a spectacular, nearly treeless, steep-sided rhyolite and dacite obsidian flow that erupted just outside the eastern caldera rim and flowed down the steep eastern flank of Medicine Lake volcano.

Image: Bee Specimen
Bee Specimen
Bee Specimen
Bee Specimen

Scientists at Lake Michigan Ecological Research Station are examining how habitat structure, fire history, nesting resources, and plant community composition affect bee community composition.

Scientists at Lake Michigan Ecological Research Station are examining how habitat structure, fire history, nesting resources, and plant community composition affect bee community composition.

Stream of lava from Pu‘u ‘Ō‘ō flowing through the forest in the Roy...
Stream of lava from Pu‘u ‘Ō‘ō flowing through the forest in the Roy...
Stream of lava from Pu‘u ‘Ō‘ō flowing through the forest in the Roy...
Stream of lava from Pu‘u ‘Ō‘ō flowing through the forest in the Roy...

Stream of lava from Pu‘u ‘Ō‘ō flowing through the forest in the Royal Gardens subdivision, February 28, 2008. The lava stream is about 3 m (10 ft) wide. Kīlauea Volcano, Hawai‘i.

HVO technicians working on seismic station at summit of Kīlauea Vol...
HVO technicians working seismic station at summit of Kīlauea
HVO technicians working seismic station at summit of Kīlauea
HVO technicians working seismic station at summit of Kīlauea

HVO technicians install a solar-powered seismic station near the summit of Kīlauea Volcano to monitor earthquake activity. The seismic data is transmitted via radio signal directly to the observatory, where the data is initially analyzed by automatic computer programs and then examined in greater detail by a seismologist. Mauna Loa Volcano in background.

HVO technicians install a solar-powered seismic station near the summit of Kīlauea Volcano to monitor earthquake activity. The seismic data is transmitted via radio signal directly to the observatory, where the data is initially analyzed by automatic computer programs and then examined in greater detail by a seismologist. Mauna Loa Volcano in background.

Underwater view of tropical fish swimming in shallow water above a coral reef which reflects upward to the water surface.
Fish and coral in Tumon Bay Marine Reserve, Guam
Fish and coral in Tumon Bay Marine Reserve, Guam
Image: Mud Volcano
Mud Volcano
Mud Volcano
Mud Volcano

A surface expression of geothermal activity.

A surface expression of geothermal activity.

Image: Mud Volcano
Mud Volcano
Mud Volcano
Mud Volcano

A surface expression of geothermal activity.

A surface expression of geothermal activity.

Image: Mud Volcano
Mud Volcano
Mud Volcano
Mud Volcano

A surface expression of geothermal activity.

A surface expression of geothermal activity.

North Sister volcano's east face (750 m, 2460 ft high) consists of ...
North Sister volcano's east face (750 m, 2460 ft high) consists of ...
North Sister volcano's east face (750 m, 2460 ft high) consists of ...
North Sister volcano's east face (750 m, 2460 ft high) consists of ...

East face of North Sister, 750 m high. Consists of about 100 thin mafic lava flows and intercalated layers of red scoria, capped by thick summit lava flows. Remnant of Thayer Glacier feeds cirque lake. Pervasively altered yellow-orange buttress on right, 250 m thick, consists of east-dipping, palagonitized, ash-rich fragmental flow deposits.

East face of North Sister, 750 m high. Consists of about 100 thin mafic lava flows and intercalated layers of red scoria, capped by thick summit lava flows. Remnant of Thayer Glacier feeds cirque lake. Pervasively altered yellow-orange buttress on right, 250 m thick, consists of east-dipping, palagonitized, ash-rich fragmental flow deposits.

A large poster has photos, maps, and text on it to show what research was done in Pleasure Point, Santa Cruz, California.
Does Pleasure Point Need a Seawall?
Does Pleasure Point Need a Seawall?
Does Pleasure Point Need a Seawall?

The USGS, in cooperation with Santa Cruz County and the California Department of Boating and Waterways, studied the seacliffs, ocean floor, and waves of Pleasure Point, California.   We created detailed maps of the seacliffs and ocean floor using LIDAR laser scanners and sonar.

The USGS, in cooperation with Santa Cruz County and the California Department of Boating and Waterways, studied the seacliffs, ocean floor, and waves of Pleasure Point, California.   We created detailed maps of the seacliffs and ocean floor using LIDAR laser scanners and sonar.

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