Scientists conduct a stream channel cross-section survey of the Toutle River on the north side of Mount St. Helens (view to the southwest).
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Images related to natural hazards.
Scientists conduct a stream channel cross-section survey of the Toutle River on the north side of Mount St. Helens (view to the southwest).
Assembling Hawai‘i Island's volcanoes: Does size really matter?
Assembling Hawai‘i Island's volcanoes: Does size really matter?Colors ranging from red to purple indicate the water depth around the Island of Hawai‘i, while shades of gray show land topography above sea level. Red shows lava flows erupted over the past 200 years. The Puna Ridge represents the submarine extension of Kīlauea's east rift zone.
Assembling Hawai‘i Island's volcanoes: Does size really matter?
Assembling Hawai‘i Island's volcanoes: Does size really matter?Colors ranging from red to purple indicate the water depth around the Island of Hawai‘i, while shades of gray show land topography above sea level. Red shows lava flows erupted over the past 200 years. The Puna Ridge represents the submarine extension of Kīlauea's east rift zone.
View of Pu‘u ‘Ō‘ō, looking SW. The vent for the Kahauale‘a 2 flow ...
View of Pu‘u ‘Ō‘ō, looking SW. The vent for the Kahauale‘a 2 flow ...View of Pu‘u ‘Ō‘ō, looking southwest. The vent for the Kahauale‘a 2 flow is on the near side of the crater, close to the center of the photograph (but obscured by white fume).
View of Pu‘u ‘Ō‘ō, looking SW. The vent for the Kahauale‘a 2 flow ...
View of Pu‘u ‘Ō‘ō, looking SW. The vent for the Kahauale‘a 2 flow ...View of Pu‘u ‘Ō‘ō, looking southwest. The vent for the Kahauale‘a 2 flow is on the near side of the crater, close to the center of the photograph (but obscured by white fume).
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ō
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ōThe Kahauale‘a 2 flow remains active northeast of Pu‘u ‘Ō‘ō, with the flow front this week consisting of a narrow finger that has reached 7.5 km (4.7 miles) northeast of the vent on Pu‘u ‘Ō‘ō. The flow front has cut a narrow swath through the forest, and is igniting numerous small fires.
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ō
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ōThe Kahauale‘a 2 flow remains active northeast of Pu‘u ‘Ō‘ō, with the flow front this week consisting of a narrow finger that has reached 7.5 km (4.7 miles) northeast of the vent on Pu‘u ‘Ō‘ō. The flow front has cut a narrow swath through the forest, and is igniting numerous small fires.
Map showing the submarine shape of the Hawaiian hotspot track, which extends from the Hawaiian Islands, through a prominent bend in the middle of the Pacific Ocean, to Alaska's Aleutian Islands. The inset shows the volcanoes in the main Hawaiian Islands.
Map showing the submarine shape of the Hawaiian hotspot track, which extends from the Hawaiian Islands, through a prominent bend in the middle of the Pacific Ocean, to Alaska's Aleutian Islands. The inset shows the volcanoes in the main Hawaiian Islands.
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ō
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ōThe Kahauale‘a 2 flow remains active northeast of Pu‘u ‘Ō‘ō, with the flow front this week consisting of a narrow finger that has reached 7.5 km (4.7 miles) northeast of the vent on Pu‘u ‘Ō‘ō. The flow front has cut a narrow swath through the forest, and is igniting numerous small fires.
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ō
Kahauale‘a 2 flow advancing through forest NE of Pu‘u ‘Ō‘ōThe Kahauale‘a 2 flow remains active northeast of Pu‘u ‘Ō‘ō, with the flow front this week consisting of a narrow finger that has reached 7.5 km (4.7 miles) northeast of the vent on Pu‘u ‘Ō‘ō. The flow front has cut a narrow swath through the forest, and is igniting numerous small fires.
During the first few hours of the Kamoamoa fissure eruption in March 2011, lava bubbled to the surface through a ground crack that propagated along Kīlauea Volcano's East Rift Zone. How it and other Hawaiian fissure eruptions work will be the topic of a talk at UH-Hilo on January 16, 2014.
During the first few hours of the Kamoamoa fissure eruption in March 2011, lava bubbled to the surface through a ground crack that propagated along Kīlauea Volcano's East Rift Zone. How it and other Hawaiian fissure eruptions work will be the topic of a talk at UH-Hilo on January 16, 2014.
Mauna Loa: How well do you know the volcano in your backyard?
Mauna Loa: How well do you know the volcano in your backyard?Erupting vents on Mauna Loa's Northeast Rift Zone near Pu‘u‘Ula‘ula (Red Hill) on Mar. 25, 1984—just hours after the eruption began—sent massive ‘A‘ā lava flows moving toward Hilo at 4 miles per hour. By the time the eruption ended on April 15, lava flows had reached to within four miles of Hilo city limits. USGS photo.
Mauna Loa: How well do you know the volcano in your backyard?
Mauna Loa: How well do you know the volcano in your backyard?Erupting vents on Mauna Loa's Northeast Rift Zone near Pu‘u‘Ula‘ula (Red Hill) on Mar. 25, 1984—just hours after the eruption began—sent massive ‘A‘ā lava flows moving toward Hilo at 4 miles per hour. By the time the eruption ended on April 15, lava flows had reached to within four miles of Hilo city limits. USGS photo.
Hawaii's history of destructive earthquakes the focus of two talks
Hawaii's history of destructive earthquakes the focus of two talksHawaiian Volcano Observatory seismologists will talk about Hawaii's history of destructive earthquakes in two public presentations. Paul Okubo (right) will speak at the University of Hawai‘i at Hilo on November 20, and Wes Thelen (left) will speak in Hawai‘i Volcanoes National Park on November 26.
Hawaii's history of destructive earthquakes the focus of two talks
Hawaii's history of destructive earthquakes the focus of two talksHawaiian Volcano Observatory seismologists will talk about Hawaii's history of destructive earthquakes in two public presentations. Paul Okubo (right) will speak at the University of Hawai‘i at Hilo on November 20, and Wes Thelen (left) will speak in Hawai‘i Volcanoes National Park on November 26.
Seismogram signal examples from volcanic earthquakes
Seismogram signal examples from volcanic earthquakesSeismogram signal examples from volcanic earthquakes: volcano tectonic (VT) Low Frequency (LF)/Deep Long-Period (DLP), hybrid (mix of VT and LF), very low frequency (VLF), and Tremor.
Seismogram signal examples from volcanic earthquakes
Seismogram signal examples from volcanic earthquakesSeismogram signal examples from volcanic earthquakes: volcano tectonic (VT) Low Frequency (LF)/Deep Long-Period (DLP), hybrid (mix of VT and LF), very low frequency (VLF), and Tremor.
Trout Lake lowland view from the south, downslope from Mount Adams,...
Trout Lake lowland view from the south, downslope from Mount Adams,...Trout Lake lowland view from the south, downslope from Mount Adams, Washington. The lowland area along the White Salmon River (trees) is underlain by lahar deposits 300 and 6000 years old.
Trout Lake lowland view from the south, downslope from Mount Adams,...
Trout Lake lowland view from the south, downslope from Mount Adams,...Trout Lake lowland view from the south, downslope from Mount Adams, Washington. The lowland area along the White Salmon River (trees) is underlain by lahar deposits 300 and 6000 years old.
Northern Lights over the World Heritage site. The aurora is more active when there are solar flares on the sun.
Northern Lights over the World Heritage site. The aurora is more active when there are solar flares on the sun.
Southeastward view across saddle between North and Middle Sisters. ...
Southeastward view across saddle between North and Middle Sisters. ...In left foreground, ice-ravaged mafic edifice Little Brother is separated from North Sister by Little Ice Age trough of Collier Glacier. Both North Sister and Little Brother expose numerous oxidized scoria falls, whereas smooth black Middle Sister cone is cloaked by mafic lava flows.
Southeastward view across saddle between North and Middle Sisters. ...
Southeastward view across saddle between North and Middle Sisters. ...In left foreground, ice-ravaged mafic edifice Little Brother is separated from North Sister by Little Ice Age trough of Collier Glacier. Both North Sister and Little Brother expose numerous oxidized scoria falls, whereas smooth black Middle Sister cone is cloaked by mafic lava flows.
Photo of Crater Lake with oblique bathymetric image of the caldera ...
Photo of Crater Lake with oblique bathymetric image of the caldera ...Photo of Crater Lake with oblique bathymetric image of the caldera floor beneath the lake's surface. Oregon
Photo of Crater Lake with oblique bathymetric image of the caldera ...
Photo of Crater Lake with oblique bathymetric image of the caldera ...Photo of Crater Lake with oblique bathymetric image of the caldera floor beneath the lake's surface. Oregon
Time history of Yellowstone caldera uplift and subsidence patterns ...
Time history of Yellowstone caldera uplift and subsidence patterns ...Time history of Yellowstone Caldera uplift (black line) and subsidence patterns along with quarterly catalog earthquake counts (blue bars). Note that large swarms in 1985 and 2010 accompany uplift to subsidence of caldera. The vertical deformation on the right axis was measured at the Sour Creek (SC) dome in the eastern part of the Yellowstone Caldera.
Time history of Yellowstone caldera uplift and subsidence patterns ...
Time history of Yellowstone caldera uplift and subsidence patterns ...Time history of Yellowstone Caldera uplift (black line) and subsidence patterns along with quarterly catalog earthquake counts (blue bars). Note that large swarms in 1985 and 2010 accompany uplift to subsidence of caldera. The vertical deformation on the right axis was measured at the Sour Creek (SC) dome in the eastern part of the Yellowstone Caldera.
Shaded relief image of Vineyard Sound, MA Shoals
Shaded relief image of Vineyard Sound, MA Shoals
USGS technicians prepare a sediment trap to sample the sea floor off Cape Hatteras.
USGS technicians prepare a sediment trap to sample the sea floor off Cape Hatteras.
Digital Elevation Map of Mount St. Helens with annotation of pre-19...
Digital Elevation Map of Mount St. Helens with annotation of pre-19...This shaded relief image was produced from LIDAR data. LIDAR is an acronym for Light Detection and Ranging, a modern remote sensing technique used to map topography very accurately—more so than is possible with older techniques. The crater is 1.2 miles (1.9 km) wide east-west. Elsewhere the scale varies owing to the oblique viewing angle.
Digital Elevation Map of Mount St. Helens with annotation of pre-19...
Digital Elevation Map of Mount St. Helens with annotation of pre-19...This shaded relief image was produced from LIDAR data. LIDAR is an acronym for Light Detection and Ranging, a modern remote sensing technique used to map topography very accurately—more so than is possible with older techniques. The crater is 1.2 miles (1.9 km) wide east-west. Elsewhere the scale varies owing to the oblique viewing angle.
Wes Hildreth is an expert when it comes to studying the Long Valley Caldera. Here, he is standing on Tertiary basalt lava flows on the north rim of the caldera, view to the southeast with Lake Crowley visible in the center of the caldera, and McGee Mountain above the lake on the skyline.
Wes Hildreth is an expert when it comes to studying the Long Valley Caldera. Here, he is standing on Tertiary basalt lava flows on the north rim of the caldera, view to the southeast with Lake Crowley visible in the center of the caldera, and McGee Mountain above the lake on the skyline.
Eric Moore, Wayne Baldwin, and Tommy O’Brien are deploying multichannel seismic streamer onboard R/V Pelican during a 2013 seismic cruise in the Gulf of Mexico as part of the gas hydrates program.
Eric Moore, Wayne Baldwin, and Tommy O’Brien are deploying multichannel seismic streamer onboard R/V Pelican during a 2013 seismic cruise in the Gulf of Mexico as part of the gas hydrates program.
Variations of repeating earthquake activity through time
Variations of repeating earthquake activity through timeTop: Map of repeating earthquake areas corresponding to the deformation episodes, below. Bottom: Left 1996-1998 Yellowstone caldera uplift episode. Middle: 1998-2004 subsidence episode. Right: 2004-2010 uplift episode. Bottom: vertical ground deformation from GPS observations at station, WLWY, on the Sour Creek resurgent dome.
Variations of repeating earthquake activity through time
Variations of repeating earthquake activity through timeTop: Map of repeating earthquake areas corresponding to the deformation episodes, below. Bottom: Left 1996-1998 Yellowstone caldera uplift episode. Middle: 1998-2004 subsidence episode. Right: 2004-2010 uplift episode. Bottom: vertical ground deformation from GPS observations at station, WLWY, on the Sour Creek resurgent dome.