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Volcano Hazard Program images.
At Mount Baker, Washington, observers noted continuing landslide activity in the upper Middle Fork Nooksack drainage that resulted in small debris flows and muddy floods. Scientists from multiple agencies and institutions coordinated observations, surveying, and sampling to gain an understanding of the situation.
At Mount Baker, Washington, observers noted continuing landslide activity in the upper Middle Fork Nooksack drainage that resulted in small debris flows and muddy floods. Scientists from multiple agencies and institutions coordinated observations, surveying, and sampling to gain an understanding of the situation.
On Kīlauea's East Rift Zone, the Kahauale'a 2 flow advances slowly into the Puna Forest Reserve. The Kahauale`a 2 flow began in early May, 2013, on the north side of the rift.
On Kīlauea's East Rift Zone, the Kahauale'a 2 flow advances slowly into the Puna Forest Reserve. The Kahauale`a 2 flow began in early May, 2013, on the north side of the rift.
The Kahauale‘a 2 flow, which is active north of Pu‘u ‘Ō‘ō, is fed from a vent at this cone on the northeast rim of Pu‘u ‘Ō‘ō crater. Small openings at the top of the cone contain sloshing lava, and two skylights at the very start of the Kahauale‘a 2 lava tube provided views of a swiftly moving lava stream rushing downslope.
The Kahauale‘a 2 flow, which is active north of Pu‘u ‘Ō‘ō, is fed from a vent at this cone on the northeast rim of Pu‘u ‘Ō‘ō crater. Small openings at the top of the cone contain sloshing lava, and two skylights at the very start of the Kahauale‘a 2 lava tube provided views of a swiftly moving lava stream rushing downslope.
A wider view of a portion of the Kahauale‘a 2 flow margin at the forest boundary.
A wider view of a portion of the Kahauale‘a 2 flow margin at the forest boundary.
This thermal image shows the eastern ocean entry at Kupapa‘u Point. Just inland from the entry point a patch of slightly warmer temperatures indicates an area of recent small breakouts.
This thermal image shows the eastern ocean entry at Kupapa‘u Point. Just inland from the entry point a patch of slightly warmer temperatures indicates an area of recent small breakouts.
Carbon dioxide gas detection instrument installed at Horseshoe Lake, Mammoth Mountain, California.
Carbon dioxide gas detection instrument installed at Horseshoe Lake, Mammoth Mountain, California.
Teachers take a guided walk on the Hummocks Trail, learning about the depositional features of the May 18, 1980 eruption.
Teachers take a guided walk on the Hummocks Trail, learning about the depositional features of the May 18, 1980 eruption.
Todd Cullings, with the Mount St. Helens National Volcanic Monument, leads teachers in activities they can do with students before hiking the Hummocks Trail.
Todd Cullings, with the Mount St. Helens National Volcanic Monument, leads teachers in activities they can do with students before hiking the Hummocks Trail.
This geologic map of Mauna Loa shows surface flows that have been mapped as of 2013. The flows are color-coded to reflect age. Warm colors indicate younger flows, with red indicating flows erupted since 1832. Cooler colors indicate older flows, such as at South Point, which is covered by flows ranging from 7,000 to more than 21,000 years old (blues and purple).
This geologic map of Mauna Loa shows surface flows that have been mapped as of 2013. The flows are color-coded to reflect age. Warm colors indicate younger flows, with red indicating flows erupted since 1832. Cooler colors indicate older flows, such as at South Point, which is covered by flows ranging from 7,000 to more than 21,000 years old (blues and purple).
To better understand the physics of debris flows and to make more accurate hazards forecasts in the natural environment, scientists perform controlled experiments at the large-scale USGS debris flow flume facility.
To better understand the physics of debris flows and to make more accurate hazards forecasts in the natural environment, scientists perform controlled experiments at the large-scale USGS debris flow flume facility.
A close-up of the Kahauale‘a II flow burning vegetation at the forest line, just north of Pu‘u ‘Ō‘ō. The flow consists of numerous slow-moving pāhoehoe lobes.
A close-up of the Kahauale‘a II flow burning vegetation at the forest line, just north of Pu‘u ‘Ō‘ō. The flow consists of numerous slow-moving pāhoehoe lobes.
This photo looks south towards Pu‘u ‘Ō‘ō, where a vent is supplying lava to the Kahauale‘a II flow, north of the cone. This slow-moving flow has reached the forest line, producing small scattered brush fires.
This photo looks south towards Pu‘u ‘Ō‘ō, where a vent is supplying lava to the Kahauale‘a II flow, north of the cone. This slow-moving flow has reached the forest line, producing small scattered brush fires.
This photo looks south towards Pu‘u ‘Ō‘ō, where a vent is supplying lava to the Kahauale‘a II flow, north of the cone. This slow-moving flow has reached the forest line, producing small scattered brush fires.
This photo looks south towards Pu‘u ‘Ō‘ō, where a vent is supplying lava to the Kahauale‘a II flow, north of the cone. This slow-moving flow has reached the forest line, producing small scattered brush fires.
The summit eruption in Halema‘uma‘u crater remains active. The lava lake is within the Overlook crater (the source of the gas plume), which is in the southeast portion of Halema‘uma‘u Crater.
The summit eruption in Halema‘uma‘u crater remains active. The lava lake is within the Overlook crater (the source of the gas plume), which is in the southeast portion of Halema‘uma‘u Crater.
Two ocean entry points remain active near Kupapa‘u Point, near the boundary of Hawai‘i Volcanoes National Park. The eastern entry has produced a larger plume than that at the western entry, which tends to be weak and wispy.
Two ocean entry points remain active near Kupapa‘u Point, near the boundary of Hawai‘i Volcanoes National Park. The eastern entry has produced a larger plume than that at the western entry, which tends to be weak and wispy.
Pagan Volcano is the largest and one of the most active volcanoes in the Northern Mariana Islands. Prior to 2013, the volcano was not monitored with any ground-based instruments, so activity was observed only by satellite or by the few island inhabitants. Although geographically remote, eruptions from Pagan can threaten international air traffic.
Pagan Volcano is the largest and one of the most active volcanoes in the Northern Mariana Islands. Prior to 2013, the volcano was not monitored with any ground-based instruments, so activity was observed only by satellite or by the few island inhabitants. Although geographically remote, eruptions from Pagan can threaten international air traffic.
Camera captures SO2 released from Kīlauea's summit vent. HVO scientist tests the network link between the instrument and the Hawaiian Volcano Observatory.
Camera captures SO2 released from Kīlauea's summit vent. HVO scientist tests the network link between the instrument and the Hawaiian Volcano Observatory.
Pu‘u ‘Ō‘ō was still close to its maximum height of 255 m (835 ft) in 1992 (top), although its western flank had been partly buried by a lava shield. Since then, the cone has lost a third of its former height due to collapses, and lava has continued to bury its flanks (bottom). USGS photos.
Pu‘u ‘Ō‘ō was still close to its maximum height of 255 m (835 ft) in 1992 (top), although its western flank had been partly buried by a lava shield. Since then, the cone has lost a third of its former height due to collapses, and lava has continued to bury its flanks (bottom). USGS photos.
Why did the lava tube cross the road? This image shows the Peace Day lava tube coming down the pali in Royal Gardens subdivision. The lava tube parallels Ali`i avenue, shown by the straight line of warm temperatures that represent asphalt heated in the sun.
Why did the lava tube cross the road? This image shows the Peace Day lava tube coming down the pali in Royal Gardens subdivision. The lava tube parallels Ali`i avenue, shown by the straight line of warm temperatures that represent asphalt heated in the sun.
The spatter cone near the north rim of Pu‘u ‘Ō‘ō crater continues to produce pulsating gas jetting sounds. Compare this photo to one taken of the same cone on May 2 to see how much taller the cone has grown.
The spatter cone near the north rim of Pu‘u ‘Ō‘ō crater continues to produce pulsating gas jetting sounds. Compare this photo to one taken of the same cone on May 2 to see how much taller the cone has grown.
The spatter cone near the north rim of Pu‘u ‘Ō‘ō crater continues to produce pulsating gas jetting sounds. Compare this photo to one taken of the same cone on May 2 to see how much taller the cone has grown.
The spatter cone near the north rim of Pu‘u ‘Ō‘ō crater continues to produce pulsating gas jetting sounds. Compare this photo to one taken of the same cone on May 2 to see how much taller the cone has grown.