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

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 small amounts of sulfur dioxide
small amounts of sulfur dioxide
small amounts of sulfur dioxide
small amounts of sulfur dioxide

Only small amounts of sulfur dioxide (SO2) and hydrogen sulfide (H2S) are currently being released from Kīlauea, but they chemically react with each other (oxidation-reduction reaction) to form the bright yellow sulfur deposits visible on the crater walls within Halema‘uma‘u.

Only small amounts of sulfur dioxide (SO2) and hydrogen sulfide (H2S) are currently being released from Kīlauea, but they chemically react with each other (oxidation-reduction reaction) to form the bright yellow sulfur deposits visible on the crater walls within Halema‘uma‘u.

Color photograph of sulfur deposits and steam on crater wall
Sulfur deposits forming in the new Halema‘uma‘u crater
Sulfur deposits forming in the new Halema‘uma‘u crater
Sulfur deposits forming in the new Halema‘uma‘u crater

Telephoto zoom of the largest sulfur deposit forming on the NE talus wall in Halema‘uma‘u. The view is from the
USGS Hawaiian Volcano Observatory's K3cam. Images can be viewed on HVO's website at https://volcanoes.usgs.gov/observatories/hvo/webcam.html?webcam=K3cam.

test flight of an unmanned aerial system
test flight of an unmanned aerial system
test flight of an unmanned aerial system
test flight of an unmanned aerial system

A USGS pilot and Hawaiian Volcano Observatory gas geochemist prepare to conduct a test flight of an unmanned aerial system (UAS) on Kīlauea Volcano in November 2018. This UAS was outfitted with a prototype miniaturized multi-gas sensor for the detection of volcanic gases emitted by Kīlauea, including sulfur dioxide and carbon dioxide.

A USGS pilot and Hawaiian Volcano Observatory gas geochemist prepare to conduct a test flight of an unmanned aerial system (UAS) on Kīlauea Volcano in November 2018. This UAS was outfitted with a prototype miniaturized multi-gas sensor for the detection of volcanic gases emitted by Kīlauea, including sulfur dioxide and carbon dioxide.

Hawaii that extend offshore
Hawaii that extend offshore
Hawaii that extend offshore
Hawaii that extend offshore

Many of the earthquakes in Hawaii that extend offshore and up the island chain are due to plate bending, or flexure. The upper panel shows magnitude-5 and greater earthquakes since 1861, with some notable events labeled.

Many of the earthquakes in Hawaii that extend offshore and up the island chain are due to plate bending, or flexure. The upper panel shows magnitude-5 and greater earthquakes since 1861, with some notable events labeled.

progression of the magmatic intrusion from Kīlauea
progression of the magmatic intrusion from Kīlauea
progression of the magmatic intrusion from Kīlauea
progression of the magmatic intrusion from Kīlauea

Earthquakes (red dots) track the progression of the magmatic intrusion from Kīlauea Volcano's middle East Rift Zone to the lower East Rift Zone between April 30 and May 3, 2018. Orange triangles show the locations of fissure 1 (right), which erupted on May 3, and Pu‘u ‘Ō‘ō (left).

Earthquakes (red dots) track the progression of the magmatic intrusion from Kīlauea Volcano's middle East Rift Zone to the lower East Rift Zone between April 30 and May 3, 2018. Orange triangles show the locations of fissure 1 (right), which erupted on May 3, and Pu‘u ‘Ō‘ō (left).

Color graphic showing earthquake locations and counts over time
Thumbnail image for an animation of earthquake production during the 2018 eruption and caldera collapse of Kīlauea volcano
Thumbnail image for an animation of earthquake production during the 2018 eruption and caldera collapse of Kīlauea volcano
Thumbnail image for an animation of earthquake production during the 2018 eruption and caldera collapse of Kīlauea volcano

Thumbnail image for an animation of earthquake production during the 2018 eruption and caldera collapse of Kīlauea volcano. Inset of the Hawaiian Islands shows the location of the main frame (red polygon).

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.

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.

Kīlauea Volcano’s 2018 summit collapse
Kīlauea Volcano’s 2018 summit collapse
Kīlauea Volcano’s 2018 summit collapse
Kīlauea Volcano’s 2018 summit collapse

Kīlauea Volcano’s 2018 summit collapse, shown here on July 28 (left), and the lower East Rift Zone fissure 8 lava flow, shown here on July 2 (right), will be the focus of “Volcano Awareness Month” talks offered in January 2019.

Kīlauea Volcano’s 2018 summit collapse, shown here on July 28 (left), and the lower East Rift Zone fissure 8 lava flow, shown here on July 2 (right), will be the focus of “Volcano Awareness Month” talks offered in January 2019.

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. 

Views of Mauna Loa Volcano during clear weather day (left) and on d...
Views of Mauna Loa Volcano during clear weather day and on day when...
Views of Mauna Loa Volcano during clear weather day and on day when...
Views of Mauna Loa Volcano during clear weather day and on day when...

These views of Mauna Loa are from near the Hawaiian Volcano Observatory looking toward the west. The view on left is typical during strong trade winds that blow the plume from Halema‘uma‘u Crater southwest of the summit area. The view on right is common during slack winds that allow vog conditions to develop in the summit area of Kīlauea.

These views of Mauna Loa are from near the Hawaiian Volcano Observatory looking toward the west. The view on left is typical during strong trade winds that blow the plume from Halema‘uma‘u Crater southwest of the summit area. The view on right is common during slack winds that allow vog conditions to develop in the summit area of Kīlauea.

 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

Map of selected earthquakes beneath a portion of southeast Hawaii
Map of selected earthquakes beneath a portion of southeast Hawaii
Map of selected earthquakes beneath a portion of southeast Hawaii
Map of selected earthquakes beneath a portion of southeast Hawaii

Map of selected earthquakes beneath a portion of southeast Hawai`i from May 4, 2018 to March 14, 2019, showing principally aftershocks following May 4, 2018 M6.9 earthquake. Black dots indicate epicenters of 13,083 earthquakes located during this time interval; yellow stars show locations of the M6.9 earthquake and the March 13, 2019 M5.5 earthquake.

Map of selected earthquakes beneath a portion of southeast Hawai`i from May 4, 2018 to March 14, 2019, showing principally aftershocks following May 4, 2018 M6.9 earthquake. Black dots indicate epicenters of 13,083 earthquakes located during this time interval; yellow stars show locations of the M6.9 earthquake and the March 13, 2019 M5.5 earthquake.

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.

Color plots and photographs showing Ambae eruption and impacts
Ambae Island, Ambae eruption sequence, and Ambae evacuations
Ambae Island, Ambae eruption sequence, and Ambae evacuations
Ambae Island, Ambae eruption sequence, and Ambae evacuations

Ambae Island is in the northern Vanuatu archipelago (Figure A, courtesy of NASA) and hosts a nested caldera at its summit. A temporary seismic-acoustic array was deployed beginning July 2018 (yellow squares). Local airports are marked by the red squares.

Ambae Island is in the northern Vanuatu archipelago (Figure A, courtesy of NASA) and hosts a nested caldera at its summit. A temporary seismic-acoustic array was deployed beginning July 2018 (yellow squares). Local airports are marked by the red squares.

Lava flow thickness 2018
Lava flow thickness 2018
Lava flow thickness 2018
Lava flow thickness 2018

This preliminary thickness map of Kīlauea Volcano's 2018 lower East Rift Zone lava flows was calculated by subtracting pre-eruption ground surface elevations from post-eruption ground surface elevations mapped with USGS Unmanned Aerial System (drone) flights.

This preliminary thickness map of Kīlauea Volcano's 2018 lower East Rift Zone lava flows was calculated by subtracting pre-eruption ground surface elevations from post-eruption ground surface elevations mapped with USGS Unmanned Aerial System (drone) flights.

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.

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