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Hawaiian Volcano Observatory images of eruptive activity, field work, and more.

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Explosive eruption columns of ash rising
Explosive eruption columns of ash rising
Explosive eruption columns of ash rising
Explosive eruption columns of ash rising

Explosive eruption columns of ash rising from Halema‘uma‘u at 11:15 a.m. on May 18, 1924 (top) and at 11:05 a.m. on May 15, 2018 (bottom) look similar.

Explosive eruption columns of ash rising from Halema‘uma‘u at 11:15 a.m. on May 18, 1924 (top) and at 11:05 a.m. on May 15, 2018 (bottom) look similar.

earthquakes that occurred beneath the island
earthquakes that occurred beneath the island
earthquakes that occurred beneath the island
earthquakes that occurred beneath the island

The USGS Hawaiian Volcano Observatory continues to closely monitor volcanoes and earthquakes on the Island of Hawai‘i. On this map, which shows earthquakes that occurred beneath the island between August 6, 2018, and November 14, 2018, the size of each circle depicts earthquake magnitude and color indicates earthquake depth, relative to mean sea level.

The USGS Hawaiian Volcano Observatory continues to closely monitor volcanoes and earthquakes on the Island of Hawai‘i. On this map, which shows earthquakes that occurred beneath the island between August 6, 2018, and November 14, 2018, the size of each circle depicts earthquake magnitude and color indicates earthquake depth, relative to mean sea level.

a tiltmeter is ready for installation
a tiltmeter is ready for installation
a tiltmeter is ready for installation
a tiltmeter is ready for installation

On the right, a tiltmeter is ready for installation in a shallow borehole. On the left, the tiltmeter is located at the bottom of a 3 to 4 m (10 to 15 ft) borehole lined with a metal casing. The tiltmeter is surrounded by sand to secure it within the borehole so that it does not touch the casing.

On the right, a tiltmeter is ready for installation in a shallow borehole. On the left, the tiltmeter is located at the bottom of a 3 to 4 m (10 to 15 ft) borehole lined with a metal casing. The tiltmeter is surrounded by sand to secure it within the borehole so that it does not touch the casing.

 Department of Interior UAS pilots
UAS pilots at Kilauea
UAS pilots at Kilauea
UAS pilots at Kilauea

Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb

Department of Interior UAS pilots from left to right – Elizabeth Pendleton (USGS, Woods Hole, MA), Colin Milone (Office of Aviation Services, AK), John Vogel (USGS; Flagstaff, AZ), Sandy Brosnahan (USGS, Woods Hole, MA), Brandon Forbes (USGS; Tucson, AZ), Chris Holmquist-Johnson (USGS; Fort Collins, CO),&nb

Continued degassing from fumaroles at fissures
Continued degassing from fumaroles at fissures
Continued degassing from fumaroles at fissures
Continued degassing from fumaroles at fissures

Continued degassing from fumaroles at fissures on Kīlauea Volcano's lower East Rift Zone produce native sulfur crystals when sulfur dioxide and hydrogen sulfide gases react and cool upon reaching the surface. The delicate sulfur crystals are 5–15 mm (0.2–0.6 in) long.

Continued degassing from fumaroles at fissures on Kīlauea Volcano's lower East Rift Zone produce native sulfur crystals when sulfur dioxide and hydrogen sulfide gases react and cool upon reaching the surface. The delicate sulfur crystals are 5–15 mm (0.2–0.6 in) long.

pockets of natural gas from the burning plant material can ignite
pockets of natural gas from the burning plant material can ignite
pockets of natural gas from the burning plant material can ignite
pockets of natural gas from the burning plant material can ignite

When molten lava encroaches on grassland, forests, or other vegetated land, subsurface pockets of natural gas from the burning plant material can ignite, causing a blast known as a "methane explosion." To avoid this hazard, keep a safe distance—at least tens of yards—from the margin of an active lava flow in vegetated areas.

When molten lava encroaches on grassland, forests, or other vegetated land, subsurface pockets of natural gas from the burning plant material can ignite, causing a blast known as a "methane explosion." To avoid this hazard, keep a safe distance—at least tens of yards—from the margin of an active lava flow in vegetated areas.

Color photograph of volcanic cinder and spatter cone
Mauna Loa summit 1940 cinder-and-spatter cone
Mauna Loa summit 1940 cinder-and-spatter cone
Mauna Loa summit 1940 cinder-and-spatter cone

An aerial view of the prominent 1940 cinder-and-spatter cone on the floor of Mauna Loa's summit caldera. The cone, about 100 m (330 ft) high, was built during a 134-day-long eruption that began on April 7, 1940. Most of the caldera floor around the cone is covered by lava flows erupted in 1984.

An aerial view of the prominent 1940 cinder-and-spatter cone on the floor of Mauna Loa's summit caldera. The cone, about 100 m (330 ft) high, was built during a 134-day-long eruption that began on April 7, 1940. Most of the caldera floor around the cone is covered by lava flows erupted in 1984.

Color photograph of man and woman in front of stratovolcano
New HVO Deputy Scientist-in-Charge David Phillips
New HVO Deputy Scientist-in-Charge David Phillips
New HVO Deputy Scientist-in-Charge David Phillips

New Hawaiian Volcano Observatory Deputy Scientist-in-Charge David Phillips and his wife Francine Coloma with Japan's iconic Mt. Fuji in the background. 

New Hawaiian Volcano Observatory Deputy Scientist-in-Charge David Phillips and his wife Francine Coloma with Japan's iconic Mt. Fuji in the background. 

midwinter dawn at Halema‘uma‘u
midwinter dawn at Halema‘uma‘u
midwinter dawn at Halema‘uma‘u
midwinter dawn at Halema‘uma‘u

A midwinter dawn at Halema‘uma‘u on Kīlauea. Steaming cracks tell of water and heat interacting beneath the summit caldera of the volcano. In the background, the first rays of sunlight illuminate Uēkahuna Bluff.

A midwinter dawn at Halema‘uma‘u on Kīlauea. Steaming cracks tell of water and heat interacting beneath the summit caldera of the volcano. In the background, the first rays of sunlight illuminate Uēkahuna Bluff.

HVO geologist Matthew Patrick being interviewed on the Kīlauea lava...
Geologist Matthew Patrick being interviewed on the Kīlauea lava-flo...
Geologist Matthew Patrick being interviewed on the Kīlauea lava-flo...
Geologist Matthew Patrick being interviewed on the Kīlauea lava-flo...

HVO geologist Matthew Patrick being interviewed on the Kīlauea lava-flow field for a documentary about Hawaiian volcanism. Growing lava delta (left background) steaming at the point of ocean entry.

Kīlauea Volcano showing the main collapse area
Kīlauea Volcano showing the main collapse area
Kīlauea Volcano showing the main collapse area
Kīlauea Volcano showing the main collapse area

September 19, 2018 USGS photo of the south caldera of Kīlauea Volcano showing the main collapse area. The south Sulphur Bank is in the left side of the photo. Uēkahuna Bluff, from where this photo was taken, cuts across the bottom and lower right corner of the photo. After the collapse of 1868, the caldera floor may have looked something like this.

September 19, 2018 USGS photo of the south caldera of Kīlauea Volcano showing the main collapse area. The south Sulphur Bank is in the left side of the photo. Uēkahuna Bluff, from where this photo was taken, cuts across the bottom and lower right corner of the photo. After the collapse of 1868, the caldera floor may have looked something like this.

Sulfur dioxide and hydrogen sulfide gases
Sulfur dioxide and hydrogen sulfide gases
Sulfur dioxide and hydrogen sulfide gases
Sulfur dioxide and hydrogen sulfide gases

Sulfur dioxide and hydrogen sulfide gases themselves are not visible, but dramatic plumes are sometimes visible at Kīlauea Volcano's summit (shown here) and Pu‘u ‘Ō‘ō.

Sulfur dioxide and hydrogen sulfide gases themselves are not visible, but dramatic plumes are sometimes visible at Kīlauea Volcano's summit (shown here) and Pu‘u ‘Ō‘ō.

View into fissure 8
View into fissure 8 cone in Kīlauea Volcano's lower East Rift Zone
View into fissure 8 cone in Kīlauea Volcano's lower East Rift Zone
What is next for Kīlauea Volcano
What is next for Kīlauea Volcano
What is next for Kīlauea Volcano
What is next for Kīlauea Volcano

What is next for Kīlauea Volcano? This is a view of the summit area from the southwest, showing the collapsed area of Halema‘uma‘u and the adjacent caldera floor. A section of Crater Rim Drive preserved on a down-dropped block is visible at the far right.

What is next for Kīlauea Volcano? This is a view of the summit area from the southwest, showing the collapsed area of Halema‘uma‘u and the adjacent caldera floor. A section of Crater Rim Drive preserved on a down-dropped block is visible at the far right.

panoramic view, Hawai‘i Volcanoes National Park's Crater Rim Drive
panoramic view, Hawai‘i Volcanoes National Park's Crater Rim Drive
panoramic view, Hawai‘i Volcanoes National Park's Crater Rim Drive
panoramic view, Hawai‘i Volcanoes National Park's Crater Rim Drive

In this panoramic view, Hawai‘i Volcanoes National Park's Crater Rim Drive (left foreground) disappears into the enormous void created by the collapse of Halema‘uma‘u and portions of the Kīlauea caldera floor during the dramatic events at the summit of the volcano in May-August 2018.

In this panoramic view, Hawai‘i Volcanoes National Park's Crater Rim Drive (left foreground) disappears into the enormous void created by the collapse of Halema‘uma‘u and portions of the Kīlauea caldera floor during the dramatic events at the summit of the volcano in May-August 2018.

50,000 tons of sulfur dioxide gas per day
50,000 tons of sulfur dioxide gas per day
50,000 tons of sulfur dioxide gas per day
50,000 tons of sulfur dioxide gas per day

In mid-July 2018, fissure 8 (shown here) on Kīlauea Volcano's lower East Rift Zone was emitting more than 50,000 tons of sulfur dioxide gas per day, creating high levels of vog on the island. Since early August, lower East Rift Zone SO2 emissions have dropped to less than 100 tons per day, resulting in better air quality for Hawaii.

In mid-July 2018, fissure 8 (shown here) on Kīlauea Volcano's lower East Rift Zone was emitting more than 50,000 tons of sulfur dioxide gas per day, creating high levels of vog on the island. Since early August, lower East Rift Zone SO2 emissions have dropped to less than 100 tons per day, resulting in better air quality for Hawaii.

Color photograph of caldera
Kīlauea summit
Kīlauea summit
Kīlauea summit

At Kīlauea's summit today, a clear morning gave way to heavy rain, which re-mobilized the ash cover between HVO and the Southwest Rift Zone, concentrating the ash in washes.

At Kīlauea's summit today, a clear morning gave way to heavy rain, which re-mobilized the ash cover between HVO and the Southwest Rift Zone, concentrating the ash in washes.

color photograph of summit of volcano
Kīlauea summit
Kīlauea summit
Kīlauea summit

Kīlauea Volcano’s summit, seen here from the northeast rim of the caldera, has remained quiet, with no collapse events since August 2. It remains too soon to tell if this diminished activity represents a temporary lull or the end of summit collapses.

Kīlauea Volcano’s summit, seen here from the northeast rim of the caldera, has remained quiet, with no collapse events since August 2. It remains too soon to tell if this diminished activity represents a temporary lull or the end of summit collapses.

color photograph of sand bar and boat ramp
Pohoiki boat ramp and sand bar
Pohoiki boat ramp and sand bar
Pohoiki boat ramp and sand bar

Close view of the Pohoiki boat ramp during this morning's overflight. The southern-most flow margin has not advanced significantly toward the Pohoiki boat ramp, but black sand and larger fragments from the entry areas have washed ashore to create a sand bar and beach at this site.

Close view of the Pohoiki boat ramp during this morning's overflight. The southern-most flow margin has not advanced significantly toward the Pohoiki boat ramp, but black sand and larger fragments from the entry areas have washed ashore to create a sand bar and beach at this site.

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