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Images

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

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Black and white annotated photograph of collapse pit
View of the walls of Halemaʻumaʻu during the crater collapse of June 5, 1916, looking northeast from the south side of the crater
View of the walls of Halemaʻumaʻu during the crater collapse of June 5, 1916, looking northeast from the south side of the crater
View of the walls of Halemaʻumaʻu during the crater collapse of June 5, 1916, looking northeast from the south side of the crater

View of the walls of Halemaʻumaʻu during the crater collapse of June 5, 1916, looking northeast from the south side of the crater. The lava lake is visible at the lower left, and the outer crater walls are at the top. The crater rim is just out of frame to the top.

Black and white photograph of eruption plume
May 19, 1916 — Mauna Loa Southwest Rift Zone eruption
May 19, 1916 — Mauna Loa Southwest Rift Zone eruption
May 19, 1916 — Mauna Loa Southwest Rift Zone eruption

Image of the steam plume that accompanied the start of Mauna Loa’s 1916 eruption on the Southwest Rift Zone. View is from within Hawai‘i Volcanoes National Park, with Kīlauea caldera wall visible in the middle of the photo. Photograph by H. Wood and courtesy of University of Hawai‘i at Mānoa Hamilton Library. 

Image of the steam plume that accompanied the start of Mauna Loa’s 1916 eruption on the Southwest Rift Zone. View is from within Hawai‘i Volcanoes National Park, with Kīlauea caldera wall visible in the middle of the photo. Photograph by H. Wood and courtesy of University of Hawai‘i at Mānoa Hamilton Library. 

Black and white photograph of building on rim of crater
Hawaiian Volcano Observatory “Technology Station”
Hawaiian Volcano Observatory “Technology Station”
Hawaiian Volcano Observatory “Technology Station”

The Hawaiian Volcano Observatory (HVO), founded in 1912 by Thomas A. Jaggar, was the first of five volcano observatories supported by USGS today. The “Technology Station” (circled) on the eastern rim of Halema‘uma‘u crater—at the summit of Kīlauea—was the first, though temporary, of several buildings that HVO has occupied since its founding.

The Hawaiian Volcano Observatory (HVO), founded in 1912 by Thomas A. Jaggar, was the first of five volcano observatories supported by USGS today. The “Technology Station” (circled) on the eastern rim of Halema‘uma‘u crater—at the summit of Kīlauea—was the first, though temporary, of several buildings that HVO has occupied since its founding.

Children pose with 8 ton ballistic block at Kīlauea volcano, Hawai‘...
Children pose with 8 ton ballistic block at Kīlauea, Hawai‘i.
Children pose with 8 ton ballistic block at Kīlauea, Hawai‘i.
Children pose with 8 ton ballistic block at Kīlauea, Hawai‘i.

Some of the large ballistic blocks from the Kīlauea eruption of 1924 later became visitor attractions. Many of these blocks remain in place today as evidence of the forces unleashed at Kīlauea during the eruption of 1924.

Some of the large ballistic blocks from the Kīlauea eruption of 1924 later became visitor attractions. Many of these blocks remain in place today as evidence of the forces unleashed at Kīlauea during the eruption of 1924.

Map of post-1823 lava flows erupted from Mauna Loa (gray) and numbe...
Map of post-1823 lava flows erupted from Mauna Loa (gray) and numbe...
Map of post-1823 lava flows erupted from Mauna Loa (gray) and numbe...
Map of post-1823 lava flows erupted from Mauna Loa (gray) and numbe...

Slope map of Mauna Loa, including lava flows erupted since 1823 (gray), showing the approximate number of hours or days it took for a flow to advance from the vent location to the ocean or maximum reach of a flow. One flow that moved down the steep slopes on west flank of Mauna Loa reached the ocean in as little as 3 hours after the vent started erupting in 1950.

Slope map of Mauna Loa, including lava flows erupted since 1823 (gray), showing the approximate number of hours or days it took for a flow to advance from the vent location to the ocean or maximum reach of a flow. One flow that moved down the steep slopes on west flank of Mauna Loa reached the ocean in as little as 3 hours after the vent started erupting in 1950.

Coconut grove and campground on the southern shoreline of Kīlauea V...
Coconut grove and campground on the southern shoreline of Kīlauea a...
Coconut grove and campground on the southern shoreline of Kīlauea a...
Coconut grove and campground on the southern shoreline of Kīlauea a...

Coconut grove and campground on the southern shoreline of Kīlauea Volcano at Halapē before 1975 magnitude 7.7 earthquake. Halapē was a popular hiking destination in Hawai‘i Volcanoes National Park.

chart showing overlaid cross-sections of volcanic crater
1892 and 1894 cross-sections of Halemaʻumaʻu crater
1892 and 1894 cross-sections of Halemaʻumaʻu crater
1892 and 1894 cross-sections of Halemaʻumaʻu crater

Surveyor Frank Dodge's 1894 cross-section of Halema‘uma‘u overlaid on his 1892 cross-section. The 1892 lava lake was measured at 73 m (240 ft) below the rim of Halema‘uma‘u pit and by early-1894, the lava lake had filled the pit and frequently overflowed onto the caldera floor.

Surveyor Frank Dodge's 1894 cross-section of Halema‘uma‘u overlaid on his 1892 cross-section. The 1892 lava lake was measured at 73 m (240 ft) below the rim of Halema‘uma‘u pit and by early-1894, the lava lake had filled the pit and frequently overflowed onto the caldera floor.

black-and-white photograph of volcanic terrain
1894 view of lava flows in Kaluapele
1894 view of lava flows in Kaluapele
1894 view of lava flows in Kaluapele

Photograph taken on March 20, 1894 looking up at the Halemaʻumaʻu lava lake perched atop a low dome on the floor of Kaluapele (Kīlauea caldera).

Photograph taken on March 20, 1894 looking up at the Halemaʻumaʻu lava lake perched atop a low dome on the floor of Kaluapele (Kīlauea caldera).

Annotated photograph of active and inactive lava flows
May 14, 2026 — Kīlauea episode 47 lava flows
May 14, 2026 — Kīlauea episode 47 lava flows
May 14, 2026 — Kīlauea episode 47 lava flows

This annotated photo was taken at 6:24 p.m. HST on May 14, 2026, from the south rim of Halema‘uma‘u crater and looks north during episode 47 of lava fountaining at the summit of Kīlauea on May 14, 2026. Only north vent produced a lava fountain, and associated lava flows traversed east across the crater floor.

This annotated photo was taken at 6:24 p.m. HST on May 14, 2026, from the south rim of Halema‘uma‘u crater and looks north during episode 47 of lava fountaining at the summit of Kīlauea on May 14, 2026. Only north vent produced a lava fountain, and associated lava flows traversed east across the crater floor.

Image: Halema'uma'u Vent Gas Plume
Halema'uma'u Vent Gas Plume
Halema'uma'u Vent Gas Plume
Halema'uma'u Vent Gas Plume

Over the past several days, the lava surface within the vent in Halema'uma'u has occasionally, and temporarily, reached to within about 115 m (375 ft) below the floor of Halema'uma'u Crater, as seen in this photo. During these high-lava stands, the gas plume is generally fairly wispy, providing the rare naked-eye view of the lava surface.

Over the past several days, the lava surface within the vent in Halema'uma'u has occasionally, and temporarily, reached to within about 115 m (375 ft) below the floor of Halema'uma'u Crater, as seen in this photo. During these high-lava stands, the gas plume is generally fairly wispy, providing the rare naked-eye view of the lava surface.

Image: Panorama of Pu'u 'O 'o Crater
Panorama of Pu'u 'O 'o Crater
Panorama of Pu'u 'O 'o Crater
Panorama of Pu'u 'O 'o Crater

Panorama of Pu'u 'O 'o crater from the south rim of Pu'u 'O 'o cone. Active lava flows (light gray) cover much of the crater floor and are erupting from the degassing vent at the far left.

Panorama of Pu'u 'O 'o crater from the south rim of Pu'u 'O 'o cone. Active lava flows (light gray) cover much of the crater floor and are erupting from the degassing vent at the far left.

Image: Erupting Vent in Pu'u 'O 'o Crater
Erupting Vent in Pu'u 'O 'o Crater
Erupting Vent in Pu'u 'O 'o Crater
Erupting Vent in Pu'u 'O 'o Crater

Close-up view of the erupting vent in Pu'u 'O 'o crater. Lava is not visible because it is going directly into tubes beneath the crusted surface to the right and feeding small lava flows near the flow front.

Close-up view of the erupting vent in Pu'u 'O 'o crater. Lava is not visible because it is going directly into tubes beneath the crusted surface to the right and feeding small lava flows near the flow front.

Image: Lava Entry near Kalapana
Lava Entry near Kalapana
Lava Entry near Kalapana
Lava Entry near Kalapana

View of the western edge of the western ocean entry delta near Kalapana.

Image: Pahoehoe Toe Advancing on Beach
Pahoehoe Toe Advancing on Beach
Pahoehoe Toe Advancing on Beach
Pahoehoe Toe Advancing on Beach

The Puhiokalaikini entry continues to expand eastward, as small pahoehoe toes advanced on the new black sand beach below the seacliff.

The Puhiokalaikini entry continues to expand eastward, as small pahoehoe toes advanced on the new black sand beach below the seacliff.

Image: Distant Fume from Lava Entry
Distant Fume from Lava Entry
Distant Fume from Lava Entry
Distant Fume from Lava Entry

View looking toward the ocean entries in the distance. The 'Ili'ili entry is marked by the tiny plume to the left. The very broad Puhiokalaikini entry comprises the rest of the plumes along the shoreline. The tube system feeding the ocean entries is delineated by the fume in the foreground.

View looking toward the ocean entries in the distance. The 'Ili'ili entry is marked by the tiny plume to the left. The very broad Puhiokalaikini entry comprises the rest of the plumes along the shoreline. The tube system feeding the ocean entries is delineated by the fume in the foreground.

Image: Lava Consuming Piece of Shrubbery
Lava Consuming Piece of Shrubbery
Lava Consuming Piece of Shrubbery
Lava Consuming Piece of Shrubbery

Lava was only slowly oozing from the edge of the flow adjacent to the road. In this photo, a piece of shrubbery is slowly consumed by the lava.

Lava was only slowly oozing from the edge of the flow adjacent to the road. In this photo, a piece of shrubbery is slowly consumed by the lava.

Image: Puhi-o-Kalaikini Entry Plume
Puhi-o-Kalaikini Entry Plume
Puhi-o-Kalaikini Entry Plume
Puhi-o-Kalaikini Entry Plume

The Puhi-o-Kalaikini entry continues to put up a large plume just west of Kalapana Gardens. No active lava flows have been reported on coastal flats in nearly 2 weeks.

The Puhi-o-Kalaikini entry continues to put up a large plume just west of Kalapana Gardens. No active lava flows have been reported on coastal flats in nearly 2 weeks.

Image: Halema'uma'u Vent Gas Plume
Halema'uma'u Vent Gas Plume
Halema'uma'u Vent Gas Plume
Halema'uma'u Vent Gas Plume

Kilauea's active summit vent is on the southeast side of Halema'uma'u Crater. In this photo, the floor of Halema'uma'u stretches out beyond the vent, and the summit of Kilauea Volcano is at upper right. The observation tower at the Hawaiian Volcano Observatory is the highest bump in the photo at Kilauea's summit.

Kilauea's active summit vent is on the southeast side of Halema'uma'u Crater. In this photo, the floor of Halema'uma'u stretches out beyond the vent, and the summit of Kilauea Volcano is at upper right. The observation tower at the Hawaiian Volcano Observatory is the highest bump in the photo at Kilauea's summit.

Image: Halema'uma'u Maintains Basic Geometry
Halema'uma'u Maintains Basic Geometry
Halema'uma'u Maintains Basic Geometry
Halema'uma'u Maintains Basic Geometry

The lava lake at Halema'uma'u has maintained the same basic geometry since February of this year. This thermal image was taken during a helicopter overflight, and shows the lava surface deep within the vent cavity. The lava surface is kidney-shaped and approximately 60 x 90 meters in size, and situated about 170 meters below the rim of the vent cavity.

The lava lake at Halema'uma'u has maintained the same basic geometry since February of this year. This thermal image was taken during a helicopter overflight, and shows the lava surface deep within the vent cavity. The lava surface is kidney-shaped and approximately 60 x 90 meters in size, and situated about 170 meters below the rim of the vent cavity.

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