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Volcano Hazard Program images.

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Colorful plumes - can we see volcanic gases?...
Colorful plumes - can we see volcanic gases?
Colorful plumes - can we see volcanic gases?
Colorful plumes - can we see volcanic gases?

LERZ Fissure 8 on June 5, 2018 - The sun is behind the observer taking this photo, making the plume appear bluish due to sunlight scattering by tiny sulfate aerosols. The gas plume is against a very dark cloud background, so that no backlighting is affecting the plume view. Photo credit: Allan Lerner, USGS Volunteer

LERZ Fissure 8 on June 5, 2018 - The sun is behind the observer taking this photo, making the plume appear bluish due to sunlight scattering by tiny sulfate aerosols. The gas plume is against a very dark cloud background, so that no backlighting is affecting the plume view. Photo credit: Allan Lerner, USGS Volunteer

Colorful plumes - can we see volcanic gases?...
Colorful plumes - can we see volcanic gases?
Colorful plumes - can we see volcanic gases?
Colorful plumes - can we see volcanic gases?

A volcanic gas cloud over the LERZ on May 19, 2018 - In this picture, the sun is illuminating the volcanic gas plume from behind. The plume appears orange in color, as the blue component of the sunlight has been preferentially removed by scattering on tiny sulfate aerosols.

A volcanic gas cloud over the LERZ on May 19, 2018 - In this picture, the sun is illuminating the volcanic gas plume from behind. The plume appears orange in color, as the blue component of the sunlight has been preferentially removed by scattering on tiny sulfate aerosols.

Aerial of ocean entry
Kīlauea Volcano — Vacationland Ocean Entry
Kīlauea Volcano — Vacationland Ocean Entry
Kīlauea Volcano — Vacationland Ocean Entry

View of the active ocean entry in the vicinity of Vacationland. The interaction of hot lava with the ocean creates "laze", a corrosive seawater plume laden with hydrochloric acid and fine volcanic particles that can irritate the skin, eyes, and lungs, but that dissipates quickly with distance.

View of the active ocean entry in the vicinity of Vacationland. The interaction of hot lava with the ocean creates "laze", a corrosive seawater plume laden with hydrochloric acid and fine volcanic particles that can irritate the skin, eyes, and lungs, but that dissipates quickly with distance.

View of fissure 8 cone
Kīlauea Volcano — Fissure 8
Kīlauea Volcano — Fissure 8
Kīlauea Volcano — Fissure 8

Fissure 8 produces a lava fountain that pulses to heights of 55 to 60 m (185 to 200 ft).

Kīlauea Volcano — Halema`uma`u Slumping
Kīlauea Volcano — Halema`uma`u Slumping
Kīlauea Volcano — Halema`uma`u Slumping

At Kīlauea Volcano's summit, inward slumping of the rim and walls of Halema‘uma‘u continues in response to ongoing subsidence. In this view to the southwest taken after this morning's event, a section of dark-colored wall rock (center left) has detached and dropped downward into the crater.

At Kīlauea Volcano's summit, inward slumping of the rim and walls of Halema‘uma‘u continues in response to ongoing subsidence. In this view to the southwest taken after this morning's event, a section of dark-colored wall rock (center left) has detached and dropped downward into the crater.

Aerial of ocean entries
Kīlauea Volcano — Kapoho Bay and Vacationland
Kīlauea Volcano — Kapoho Bay and Vacationland
Kīlauea Volcano — Kapoho Bay and Vacationland

Lava from fissure 8 travels about 13 km (8 mi) down a well established channel (visible in the center of the image) to an ocean entry at Kapoho. Lava is building a seaward delta that is approximately 320 acres in size. The view is to the southwest with the Kapoho area in the lower right.

Lava from fissure 8 travels about 13 km (8 mi) down a well established channel (visible in the center of the image) to an ocean entry at Kapoho. Lava is building a seaward delta that is approximately 320 acres in size. The view is to the southwest with the Kapoho area in the lower right.

Fissure activity and active ocean entry in Kīlauea Volcano's lower ...
Fissure activity and active ocean entry in Kīlauea's LERZ
Fissure activity and active ocean entry in Kīlauea's LERZ
Fissure activity and active ocean entry in Kīlauea's LERZ

Fissure 8 produces a lava fountain that pulses to heights of 55 to 60 m (185 to 200 ft). Spattering has built a cinder cone that partially encircles fissure 8, now 51 m (170 ft) tall at its highest point. The steam in the foreground is the result of heavy morning rain falling on warm (not hot) tephra (lava fragments).

Fissure 8 produces a lava fountain that pulses to heights of 55 to 60 m (185 to 200 ft). Spattering has built a cinder cone that partially encircles fissure 8, now 51 m (170 ft) tall at its highest point. The steam in the foreground is the result of heavy morning rain falling on warm (not hot) tephra (lava fragments).

Lava from fissure 8 travels about 13 km (8 mi) down a well establis...
Lava from fissure 8 travels about 13 km (8 mi) down a well establis...
Lava from fissure 8 travels about 13 km (8 mi) down a well establis...
Lava from fissure 8 travels about 13 km (8 mi) down a well establis...

Lava from fissure 8 travels about 13 km (8 mi) down a well established channel (visible in the center of the image) to an ocean entry at Kapoho. Lava is building a seaward delta that is approximately 320 acres in size. The view is to the southwest with the Kapoho area in the lower right. The white plume is the vigorous ocean entry at Vacationland.

Lava from fissure 8 travels about 13 km (8 mi) down a well established channel (visible in the center of the image) to an ocean entry at Kapoho. Lava is building a seaward delta that is approximately 320 acres in size. The view is to the southwest with the Kapoho area in the lower right. The white plume is the vigorous ocean entry at Vacationland.

View of the active ocean entry in the vicinity of Vacationland. The...
View of the active ocean entry in the vicinity of Vacationland. The...
View of the active ocean entry in the vicinity of Vacationland. The...
View of the active ocean entry in the vicinity of Vacationland. The...

View of the active ocean entry in the vicinity of Vacationland. The interaction of hot lava with the ocean creates "laze", a corrosive seawater plume laden with hydrochloric acid and fine volcanic particles that can irritate the skin, eyes, and lungs, but that dissipates quickly with distance.

View of the active ocean entry in the vicinity of Vacationland. The interaction of hot lava with the ocean creates "laze", a corrosive seawater plume laden with hydrochloric acid and fine volcanic particles that can irritate the skin, eyes, and lungs, but that dissipates quickly with distance.

Fissure 8 lava fountain
Kīlauea Volcano — Fissure 8 Lava Fountain
Kīlauea Volcano — Fissure 8 Lava Fountain
Kīlauea Volcano — Fissure 8 Lava Fountain

Photograph taken during helicopter overflight captures fissure 8 lava fountain.

Laze plumes from ocean entry of lava
Kīlauea Volcano — Ocean Entry
Kīlauea Volcano — Ocean Entry
Kīlauea Volcano — Ocean Entry

The ocean entry remains fairly broad with a white steam/laze plume blowing onshore. USGS image taken June 15, 2018.

The ocean entry remains fairly broad with a white steam/laze plume blowing onshore. USGS image taken June 15, 2018.

View of a spatter cone
Kīlauea Volcano — Spatter Cone Building
Kīlauea Volcano — Spatter Cone Building
Kīlauea Volcano — Spatter Cone Building

Lava fountains from Fissure 8 reach heights of 200 ft overnight. The cinder and spatter cone that is building around the fissure is now about 165 ft at its highest point.

Lava fountains from Fissure 8 reach heights of 200 ft overnight. The cinder and spatter cone that is building around the fissure is now about 165 ft at its highest point.

Kīlauea Volcano — Halema`uma`u Crater Enlargement
Kīlauea Volcano — Halema`uma`u Crater Enlargement
Kīlauea Volcano — Halema`uma`u Crater Enlargement

This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 14 at about 6:00 a.m. HST.

This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 14 at about 6:00 a.m. HST.

Thermal map of fissure system and lava flows...
Thermal map of fissure system and lava flows
Thermal map of fissure system and lava flows
Thermal map of fissure system and lava flows

This thermal map shows the fissure system and lava flows as of 6 am on Thursday June 14. The fountain at Fissure 8 remains active, with the lava flow entering the ocean at Kapoho. Very small, weak lava flows have been active recently near the Fissure 16/18 area. The black and white area is the extent of the thermal map.

This thermal map shows the fissure system and lava flows as of 6 am on Thursday June 14. The fountain at Fissure 8 remains active, with the lava flow entering the ocean at Kapoho. Very small, weak lava flows have been active recently near the Fissure 16/18 area. The black and white area is the extent of the thermal map.

Satellite radar shows continued inward slumping of Halema‘uma‘u cra...
Satellite radar shows continued inward slumping of Halema‘uma‘u
Satellite radar shows continued inward slumping of Halema‘uma‘u
Satellite radar shows continued inward slumping of Halema‘uma‘u

This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 14 at about 6:00 a.m. HST.

This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 14 at about 6:00 a.m. HST.

View of a fissure with lava and steam coming out
Kīlauea Volcano — Fissure 8 Cone Building
Kīlauea Volcano — Fissure 8 Cone Building
Kīlauea Volcano — Fissure 8 Cone Building

The Fissure 8 viewed from the north at 7:50 AM. The cone is roughly 50 m (165 ft) high at is peak, and a plume of sulfur dioxide and other volcanic gases rises as an orange tinge from the erupting lava fountains (hidden within the cone). Lava is still flowing out of the ventunabated as a full channel.

The Fissure 8 viewed from the north at 7:50 AM. The cone is roughly 50 m (165 ft) high at is peak, and a plume of sulfur dioxide and other volcanic gases rises as an orange tinge from the erupting lava fountains (hidden within the cone). Lava is still flowing out of the ventunabated as a full channel.

Aerial view of laze plumes at ocean entry point
Kīlauea Volcano — Laze Plumes
Kīlauea Volcano — Laze Plumes
Kīlauea Volcano — Laze Plumes

Several laze plumes rise along the ocean entry margin as break outs feed many small and large flows. The largest Pāhoehoe breakout area is on the northern margin of the flow.

Several laze plumes rise along the ocean entry margin as break outs feed many small and large flows. The largest Pāhoehoe breakout area is on the northern margin of the flow.

Aerial of lava breakouts along ocean entry.
Kīlauea Volcano — Pāhoehoe Breakouts
Kīlauea Volcano — Pāhoehoe Breakouts
Kīlauea Volcano — Pāhoehoe Breakouts

A close up view of the pāhoehoe breakouts along the northern ocean entry.

View of fissure 8
Kīlauea Volcano — Fissure 8
Kīlauea Volcano — Fissure 8
Kīlauea Volcano — Fissure 8

Fissure 8 lava fountains continue to reach heights of 40-45 m (130-150 ft) from within the growing cone of cinder and spatter, which

Fissure 8 lava fountains continue to reach heights of 40-45 m (130-150 ft) from within the growing cone of cinder and spatter, which

Aerial of lava entering ocean
Kīlauea Volcano — Ocean Entry
Kīlauea Volcano — Ocean Entry
Kīlauea Volcano — Ocean Entry

View of the ocean entry and the resulting laze plume where lava is entering the sea. As of June 12, lava entering the ocean had added about 100 ha (250 acres) of new land to the Island of Hawai‘i. 

View of the ocean entry and the resulting laze plume where lava is entering the sea. As of June 12, lava entering the ocean had added about 100 ha (250 acres) of new land to the Island of Hawai‘i.