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Kīlauea images of eruptive activity, field work, and more.

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Scientist setting up an instrument
Kīlauea Volcano — GPS Measurements at Summit
Kīlauea Volcano — GPS Measurements at Summit
Kīlauea Volcano — GPS Measurements at Summit

USGS-HVO geophysicists installed additional continuous GPS stations around Halema‘uma‘u this morning. These stations will allow scientists to better monitor and measure the ongoing subsidence of Halema‘uma‘u and the adjacent caldera floor.

USGS-HVO geophysicists installed additional continuous GPS stations around Halema‘uma‘u this morning. These stations will allow scientists to better monitor and measure the ongoing subsidence of Halema‘uma‘u and the adjacent caldera floor.

Aerial view of ocean entry
Kīlauea Volcano — Kapoho Ocean Entry
Kīlauea Volcano — Kapoho Ocean Entry
Kīlauea Volcano — Kapoho Ocean Entry

An aerial view of the Kapoho ocean entry, as of 6:30 a.m. HST today, shows the extent of the lava delta, now about 200 acres in size, that has formed over the past six days (lava first entered the ocean on the night of June 3).

An aerial view of the Kapoho ocean entry, as of 6:30 a.m. HST today, shows the extent of the lava delta, now about 200 acres in size, that has formed over the past six days (lava first entered the ocean on the night of June 3).

Aerial of summit showing cracking and slumping
Kīlauea Volcano — Halema`uma`u Cracking and Slumping
Kīlauea Volcano — Halema`uma`u Cracking and Slumping
Kīlauea Volcano — Halema`uma`u Cracking and Slumping

Cracking and slumping of the Halema‘uma‘u crater walls are clearly evident in this aerial view captured during HVO's overflight of Kīlauea's summit this morning. Steam plumes have been rising from within the crater, as well as from cracks adjacent to the crater.

Cracking and slumping of the Halema‘uma‘u crater walls are clearly evident in this aerial view captured during HVO's overflight of Kīlauea's summit this morning. Steam plumes have been rising from within the crater, as well as from cracks adjacent to the crater.

A lava channel formed from a fissure eruption
Kīlauea Volcano — Fissure 8 Lava Channel
Kīlauea Volcano — Fissure 8 Lava Channel
Kīlauea Volcano — Fissure 8 Lava Channel

Fissure 8 and lava channel in the lower East Rift Zone of Kīlauea Volcano during this afternoon's overflight, with no apparent slowing in the eruption rate. The lava channel remained incandescent all the way around Kapoho Crater before entering the ocean.

Fissure 8 and lava channel in the lower East Rift Zone of Kīlauea Volcano during this afternoon's overflight, with no apparent slowing in the eruption rate. The lava channel remained incandescent all the way around Kapoho Crater before entering the ocean.

Kīlauea lower East Rift Zone lava flows and fissures, June 9, 10:00...
Kīlauea LERZ lava flows and fissures, June 9, 10:00 a.m.
Kīlauea LERZ lava flows and fissures, June 9, 10:00 a.m.
Kīlauea LERZ lava flows and fissures, June 9, 10:00 a.m.

Map as of 10:00 a.m. HST, June 9, 2018. The fissure 8 flow has created a lava delta approximately 200 acres in size, filling Kapoho Bay and shallow reefs along the nearby coastline.

Aerial photo of cracking
Kīlauea Volcano — Halema‘uma‘u Cracking
Kīlauea Volcano — Halema‘uma‘u Cracking
Kīlauea Volcano — Halema‘uma‘u Cracking

Another aerial view showing prominent cracking around Halema‘uma‘u from the ongoing subsidence at Kīlauea's summit. The steaming cracks in the background have been observed for several days.

Another aerial view showing prominent cracking around Halema‘uma‘u from the ongoing subsidence at Kīlauea's summit. The steaming cracks in the background have been observed for several days.

Plumes from ocean entry
Kīlauea Volcano — Kapoho Bay and Vacationland
Kīlauea Volcano — Kapoho Bay and Vacationland
Kīlauea Volcano — Kapoho Bay and Vacationland

HVO's early morning helicopter overflight of Kīlauea's lower East Rift Zone showed that lava continues to flow into the ocean in the vicinity of Kapoho Bay and Vacationland.

HVO's early morning helicopter overflight of Kīlauea's lower East Rift Zone showed that lava continues to flow into the ocean in the vicinity of Kapoho Bay and Vacationland.

Lava fountaining at night time
Kīlauea Volcano — Lava Fountaining (Fissure 8)
Kīlauea Volcano — Lava Fountaining (Fissure 8)
Kīlauea Volcano — Lava Fountaining (Fissure 8)

Around 3:00 a.m. HST today (June 8), lava fountains erupting from fissure 8 on Kīlauea Volcano's Lower East Rift Zone were reaching heights of 180–220 feet.

Kīlauea lower East Rift Zone lava flows and fissures, June 8, 12:00...
Kīlauea LERZ lava flows and fissures, June 8, 12:00 p.m.
Kīlauea LERZ lava flows and fissures, June 8, 12:00 p.m.
Kīlauea LERZ lava flows and fissures, June 8, 12:00 p.m.

Map as of 12:00 p.m. (noon) HST, June 8, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.

Map as of 12:00 p.m. (noon) HST, June 8, 2018. Given the dynamic nature of Kīlauea's lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.

Plume coming from a crater
Kīlauea Volcano — Summit Pluming
Kīlauea Volcano — Summit Pluming
Kīlauea Volcano — Summit Pluming

Dramatic changes at Halema‘uma‘u could be seen through gases rising from the crater during HVO's overflight of the summit this morning at 10 a.m. HST. The view here looks to the southwest, with the former overlook parking lot barely visible to the left of the gas plume.

Dramatic changes at Halema‘uma‘u could be seen through gases rising from the crater during HVO's overflight of the summit this morning at 10 a.m. HST. The view here looks to the southwest, with the former overlook parking lot barely visible to the left of the gas plume.

Outgassing rising from the summit
Kīlauea Volcano — Summit Outgassing
Kīlauea Volcano — Summit Outgassing
Kīlauea Volcano — Summit Outgassing

Outgassing from Halema‘uma‘u produced twin pillars that rose in the still morning air and merged into a towering cap above the summit of Kīlauea just after sunrise.

Outgassing from Halema‘uma‘u produced twin pillars that rose in the still morning air and merged into a towering cap above the summit of Kīlauea just after sunrise.

Ocean entry plume
Kīlauea Volcano — Laze Plume
Kīlauea Volcano — Laze Plume
Kīlauea Volcano — Laze Plume

Lava enters the ocean in the vicinity of Vacationland at 7 a.m. HST. The ocean entry produces a white plume called "laze," which drifts downwind. Laze is composed of steam, hydrochloric acid and tiny volcanic glass particles, which can irritate the lungs, eyes and skin.

Lava enters the ocean in the vicinity of Vacationland at 7 a.m. HST. The ocean entry produces a white plume called "laze," which drifts downwind. Laze is composed of steam, hydrochloric acid and tiny volcanic glass particles, which can irritate the lungs, eyes and skin.

lava fountain with lava flow
Kīlauea Volcano — Lava Fountain and Flow (Fissure 8)
Kīlauea Volcano — Lava Fountain and Flow (Fissure 8)
Kīlauea Volcano — Lava Fountain and Flow (Fissure 8)

View of the fissure 8 lava fountain and lava channel that travels to the ocean, a distance of about 12.5 km (7.8 mi). Photo taken during this morning's overflight at about 6:30 a.m. HST.

Crack in the ground
Kīlauea Volcano — Large Crack in Parking Lot
Kīlauea Volcano — Large Crack in Parking Lot
Kīlauea Volcano — Large Crack in Parking Lot

An even larger crack, shown here, arcs across the parking lot and bounds one of the large blocks mentioned above.

crack in parking lot
Kīlauea Volcano — Crack in Parking Lot
Kīlauea Volcano — Crack in Parking Lot
Kīlauea Volcano — Crack in Parking Lot

The median between two areas of the parking lot has been warped and broken by cracks. Ash accumulation in the parking area was generally not more than 4 cm (1.5 in) thick.

The median between two areas of the parking lot has been warped and broken by cracks. Ash accumulation in the parking area was generally not more than 4 cm (1.5 in) thick.

animated gif of crater
Kīlauea Volcano — Satellite Radar of Crater Slumping
Kīlauea Volcano — Satellite Radar of Crater Slumping
Kīlauea Volcano — Satellite Radar of Crater Slumping

This animated GIF shows a sequence of radar amplitude images that were acquired by the Italian Space Agency's Cosmo-SkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 6 at 6:00 a.m. HST.

This animated GIF shows a sequence of radar amplitude images that were acquired by the Italian Space Agency's Cosmo-SkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 6 at 6:00 a.m. HST.

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

Lava entering the ocean in the vicinity of Kapoho Bay is forming a lava delta, as seen from the air during this morning's overflight at about 7:00 a.m. HST.

Lava fountaining with lava flow
Kīlauea Volcano — Lava Fountain (Fissure 8)
Kīlauea Volcano — Lava Fountain (Fissure 8)
Kīlauea Volcano — Lava Fountain (Fissure 8)

 Fissure 8 lava fountain heights fluctuated between about 40 m (130 ft) and 70 m (230 ft) during this morning's overflight at about 6:30 a.m. HST.

Large rocks on the parking lot
Kīlauea Volcano — Large Rocks on Parking Lot
Kīlauea Volcano — Large Rocks on Parking Lot
Kīlauea Volcano — Large Rocks on Parking Lot

Many large blocks appeared to be in depressions in the ash, but upon closer examination, it was concluded that wind had winnowed ash from around the blocks, creating a false impression that the depressions were made by impact.

Many large blocks appeared to be in depressions in the ash, but upon closer examination, it was concluded that wind had winnowed ash from around the blocks, creating a false impression that the depressions were made by impact.

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