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.
Images
Images related to natural hazards.
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.
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.
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.
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.
Map of Mount St. Helens Crater Glacier created from LiDAR data acquired September 2009.
Map of Mount St. Helens Crater Glacier created from LiDAR data acquired September 2009.
CalVO geologist Mae Marcaida examines thin layers of volcanic ash s...
CalVO geologist Mae Marcaida examines thin layers of volcanic ash s...CalVO geologist Mae Marcaida examines thin layers of volcanic ash sandwiched between thick beds of sediment deposited by ancestral Mono Lake in eastern California. Each ash layer is evidence of a past explosive eruption of the Mono Craters, which began erupting about 65,000 years ago just south of present-day Mono Lake.
CalVO geologist Mae Marcaida examines thin layers of volcanic ash s...
CalVO geologist Mae Marcaida examines thin layers of volcanic ash s...CalVO geologist Mae Marcaida examines thin layers of volcanic ash sandwiched between thick beds of sediment deposited by ancestral Mono Lake in eastern California. Each ash layer is evidence of a past explosive eruption of the Mono Craters, which began erupting about 65,000 years ago just south of present-day Mono Lake.
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.
Example of Yellowstone earthquake multiplets (families of repeating...
Example of Yellowstone earthquake multiplets (families of repeating...The seismic records or waveforms are from two seismic stations, and show the highly repetitive and similar nature of the seismic events.
Example of Yellowstone earthquake multiplets (families of repeating...
Example of Yellowstone earthquake multiplets (families of repeating...The seismic records or waveforms are from two seismic stations, and show the highly repetitive and similar nature of the seismic events.
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.
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.
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.
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
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.
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.
A sonar on a bottom platform while steaming to the deployment site in the Columbia River in 2013. The 3 platforms acquired data on currents and sediment transport at the river mouth over several months.
A sonar on a bottom platform while steaming to the deployment site in the Columbia River in 2013. The 3 platforms acquired data on currents and sediment transport at the river mouth over several months.
Photo of the seafloor in Block Island Sound, Rhode Island
Photo of the seafloor in Block Island Sound, Rhode IslandPhoto of the seafloor in Block Island Sound showing a rock crab and several shrimp on a boulder that is covered with bryozoans. The photo was collected in support of research and management activities (e.g., wind farms and fisheries) along the Rhode Island inner continental shelf.
Photo of the seafloor in Block Island Sound, Rhode Island
Photo of the seafloor in Block Island Sound, Rhode IslandPhoto of the seafloor in Block Island Sound showing a rock crab and several shrimp on a boulder that is covered with bryozoans. The photo was collected in support of research and management activities (e.g., wind farms and fisheries) along the Rhode Island inner continental shelf.
Tabernacle Hill tuff cone, part of the Black Rock Desert Volcanic Field in Utah
Tabernacle Hill tuff cone, part of the Black Rock Desert Volcanic Field in UtahTabernacle Hill tuff cone, part of the Black Rock Desert Volcanic Field in Utah, used to house a lava lake in the center of the crater.
Tabernacle Hill tuff cone, part of the Black Rock Desert Volcanic Field in Utah
Tabernacle Hill tuff cone, part of the Black Rock Desert Volcanic Field in UtahTabernacle Hill tuff cone, part of the Black Rock Desert Volcanic Field in Utah, used to house a lava lake in the center of the crater.