A closer view of the ocean entry and plumes of hot, discolored water.
Images
Volcano Hazard Program images.
A closer view of the ocean entry and plumes of hot, discolored water.
lava firehose at the ocean entry. The lava stream roughly 1-2 mete...
lava firehose at the ocean entry. The lava stream roughly 1-2 mete...A closer view of the lava firehose at the ocean entry. The lava stream here is roughly 1-2 meters wide (3-6 ft), and plunges about 20 m (66 ft) into the water.
lava firehose at the ocean entry. The lava stream roughly 1-2 mete...
lava firehose at the ocean entry. The lava stream roughly 1-2 mete...A closer view of the lava firehose at the ocean entry. The lava stream here is roughly 1-2 meters wide (3-6 ft), and plunges about 20 m (66 ft) into the water.
Summit inflation over the past day has driven the lava lake to rise slightly. This morning, the surface of the lake was about 23.5 m (77 ft) below the Overlook crater rim. In this photo, spattering was occurring along the southern lake margin in two locations.
Summit inflation over the past day has driven the lava lake to rise slightly. This morning, the surface of the lake was about 23.5 m (77 ft) below the Overlook crater rim. In this photo, spattering was occurring along the southern lake margin in two locations.
Worldview-2 satellite image of Bogoslof volcano collected on Mar. 1...
Worldview-2 satellite image of Bogoslof volcano collected on Mar. 1...Eruptive activity on March 8 produced large changes in the shape and size of the island. The most active vent for the explosive activity is located under the water in the center of the island, and it was greatly enlarged by the March 8 event. The western coastline has grown, and a new vent was produced on the north shore of the island.
Worldview-2 satellite image of Bogoslof volcano collected on Mar. 1...
Worldview-2 satellite image of Bogoslof volcano collected on Mar. 1...Eruptive activity on March 8 produced large changes in the shape and size of the island. The most active vent for the explosive activity is located under the water in the center of the island, and it was greatly enlarged by the March 8 event. The western coastline has grown, and a new vent was produced on the north shore of the island.
Satellite image shows continued breakouts on flow field
Satellite image shows continued breakouts on flow fieldThis satellite image was captured on Wednesday, March 8, by the NASA/USGS Landsat 8 satellite. Although this is a false-color image, the color map has been chosen to mimic what the human eye would expect to see. Bright red pixels depict areas of very high temperatures and show active lava. White areas are clouds.
Satellite image shows continued breakouts on flow field
Satellite image shows continued breakouts on flow fieldThis satellite image was captured on Wednesday, March 8, by the NASA/USGS Landsat 8 satellite. Although this is a false-color image, the color map has been chosen to mimic what the human eye would expect to see. Bright red pixels depict areas of very high temperatures and show active lava. White areas are clouds.
Recent collapses at Kamokuna ocean entry underscore on-going hazard
Recent collapses at Kamokuna ocean entry underscore on-going hazardAs seen in late January, the interaction of molten lava and cold seawater at the Kamokuna ocean entry produces an explosion, sending hot fragments and steam high into the air. The sea cliff in this image is about 15 meters (50 feet) high. USGS photo.
Recent collapses at Kamokuna ocean entry underscore on-going hazard
Recent collapses at Kamokuna ocean entry underscore on-going hazardAs seen in late January, the interaction of molten lava and cold seawater at the Kamokuna ocean entry produces an explosion, sending hot fragments and steam high into the air. The sea cliff in this image is about 15 meters (50 feet) high. USGS photo.
Inundation zones shown on map sheets as numbered colored boxes.
Inundation zones shown on map sheets as numbered colored boxes.
The Anatahan eruption: what might happen down the road
The Anatahan eruption: what might happen down the roadEruption cloud, from the east crater of Anatahan Volcano. View from the NE side of the island, looking in a southwesterly direction.
The Anatahan eruption: what might happen down the road
The Anatahan eruption: what might happen down the roadEruption cloud, from the east crater of Anatahan Volcano. View from the NE side of the island, looking in a southwesterly direction.
Sluggish breakout on Kīlauea's coastal plain remains active
Sluggish breakout on Kīlauea's coastal plain remains activeThe surface breakout that started on February 10 remains active on the coastal plain just east of the main episode 61g lava flow field. The flow front, pictured here, advanced to about 300 m (0.2 miles) from the emergency access road in Hawai‘i Volcanoes National Park, but appeared to be stalled this afternoon.
Sluggish breakout on Kīlauea's coastal plain remains active
Sluggish breakout on Kīlauea's coastal plain remains activeThe surface breakout that started on February 10 remains active on the coastal plain just east of the main episode 61g lava flow field. The flow front, pictured here, advanced to about 300 m (0.2 miles) from the emergency access road in Hawai‘i Volcanoes National Park, but appeared to be stalled this afternoon.
A Valentine's Day 2017 view of Kīlauea Volcano's summit lava lake, here the surface of the lake is about 21 m (69 ft) below the vent rim. The lake diameter is about 255 m or 840 ft. Careful tracking of the amount of ash emitted by lake processes suggest an important new insight into the supply of magma to Kīlauea's summit. USGS Photo.
A Valentine's Day 2017 view of Kīlauea Volcano's summit lava lake, here the surface of the lake is about 21 m (69 ft) below the vent rim. The lake diameter is about 255 m or 840 ft. Careful tracking of the amount of ash emitted by lake processes suggest an important new insight into the supply of magma to Kīlauea's summit. USGS Photo.
Campout flow forms several benches at East Ka`ili`ili. August 5, 2006. View is toward the southwest along the coast of Kīlauea Volcano at the eastern edge of the new lava entry. Note multiple benches forming at base of seacliff, which is about 20 m tall.
Campout flow forms several benches at East Ka`ili`ili. August 5, 2006. View is toward the southwest along the coast of Kīlauea Volcano at the eastern edge of the new lava entry. Note multiple benches forming at base of seacliff, which is about 20 m tall.
HVO shares its research with the international scientific community
HVO shares its research with the international scientific communityThis is a helicorder seismogram displaying vertical ground velocities at the summit of Hualālai volcano south of the earthquake epicenters. Each line represents 10 minutes and time increases from left to right. Each line continues on the line below. The seismogram starts at 2 am and ends at 2 pm HST on October 15, 2006.
HVO shares its research with the international scientific community
HVO shares its research with the international scientific communityThis is a helicorder seismogram displaying vertical ground velocities at the summit of Hualālai volcano south of the earthquake epicenters. Each line represents 10 minutes and time increases from left to right. Each line continues on the line below. The seismogram starts at 2 am and ends at 2 pm HST on October 15, 2006.
Close view of lava spilling into the sea at nearest bench in left photo.
Close view of lava spilling into the sea at nearest bench in left photo.
Webcam view of the lava pond within Pu‘u ‘Ō‘ō crater on July 10, 2007, at 11:19 a.m. H.s.t. Note that the lava level has dropped so the inner edges of the levee on the far side can be seen more clearly.
Webcam view of the lava pond within Pu‘u ‘Ō‘ō crater on July 10, 2007, at 11:19 a.m. H.s.t. Note that the lava level has dropped so the inner edges of the levee on the far side can be seen more clearly.
Webcam view of the lava pond on July 12 at 10:43 a.m. The lava level is higher than on July 10 and completely fills the levees.
Webcam view of the lava pond on July 12 at 10:43 a.m. The lava level is higher than on July 10 and completely fills the levees.
This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of February 16 is shown in pink, while widening and advancement of the active flow as of February 24 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.
This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of February 16 is shown in pink, while widening and advancement of the active flow as of February 24 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.
Remotely measuring the temperature of Kīlauea lava
Remotely measuring the temperature of Kīlauea lavaA U.S. Geological Survey scientist used a custom-built, high-speed camera to remotely measure the temperature of spattering lava on the surface of Kīlauea Volcano's summit lava lake (background). This particular experiment, conducted from the Jaggar Museum overlook in Hawai‘i Volcanoes National Park on December 10, 2016, was part of a NASA-funded research project.
Remotely measuring the temperature of Kīlauea lava
Remotely measuring the temperature of Kīlauea lavaA U.S. Geological Survey scientist used a custom-built, high-speed camera to remotely measure the temperature of spattering lava on the surface of Kīlauea Volcano's summit lava lake (background). This particular experiment, conducted from the Jaggar Museum overlook in Hawai‘i Volcanoes National Park on December 10, 2016, was part of a NASA-funded research project.
Today (February 22, 2017), the breakout along the eastern edge of Kīlauea Volcano's episode 61g flow remains active and had advanced approximately 570 m (620 yards) since it was last mapped on February 14.
Today (February 22, 2017), the breakout along the eastern edge of Kīlauea Volcano's episode 61g flow remains active and had advanced approximately 570 m (620 yards) since it was last mapped on February 14.
February 19 Bogoslof eruption plume as seen from Unalaska Island, 53 miles ESE of Bogoslof volcano. Photo taken from helicopter during fieldwork by AVO geologists at 5:22PM, approximately 14 minutes after the start of the eruption.
February 19 Bogoslof eruption plume as seen from Unalaska Island, 53 miles ESE of Bogoslof volcano. Photo taken from helicopter during fieldwork by AVO geologists at 5:22PM, approximately 14 minutes after the start of the eruption.
This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of January 12 is shown in pink, while widening and advancement of the active flow as of February 16 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.
This map shows recent changes to Kīlauea's East Rift Zone lava flow field. The area of the active flow field as of January 12 is shown in pink, while widening and advancement of the active flow as of February 16 is shown in red. Older Pu‘u ‘Ō‘ō lava flows (1983-2016) are shown in gray.
Left: Astronauts James A. Lovell, Jr., and Fred W. Haise, Jr., members of NASA's third team of moon explorers, carried cameras, communications equipment, and an Apollo Lunar Hand Tools scoop during a simulation of a lunar traverse at Kīlauea Volcano in December 1969.
Left: Astronauts James A. Lovell, Jr., and Fred W. Haise, Jr., members of NASA's third team of moon explorers, carried cameras, communications equipment, and an Apollo Lunar Hand Tools scoop during a simulation of a lunar traverse at Kīlauea Volcano in December 1969.