Videos

Aerial views of the ocean entry on Kīlauea Volcano's lower East Rift Zone on June 12, 2018, around 6:30 a.m. HST, show multiple small lavastreams spilling into the ocean along the southern portion of the lava delta in Kapoho Bay.

Three closely spaced lava fountains at fissure 8 continue to feed a channelized flow trending north and then east to the ocean entry at Kapoho Bay. This video is from an HVO helicopter overflight of the braided lava channel this morning around 6:30 a.m. HST.

USGS Hawaiian Volcano Observatory, Status of Kīlauea Volcano, June 11, 2018, Jessica Ball, USGS Volcanologist

The interaction of molten lava flowing into cool seawater causes pulsating "littoral explosions" that throw spatter (fragments of molten lava) and pieces of solidified glassy lava (black sand, Pele's hair, limu o Pele) high into the air.

Video of the lava fountain and flow (left) from fissure 8. Only the tallest waves of the channelized flow can be seen in the video.

Video of the lava ocean entry during today's late afternoon overflight of the lower East Rift Zone.

USGS Hawaiian Volcano Observatory, Status of Kīlauea Volcano, June 7, 2018. Jessica Ball, USGS Volcanologist.

Clear conditions at Pu‘u ‘Ō‘ō provided good views into the crater. The crater floor collapsed, and the lava lake drained, a little more than a month ago. The crater now has a funnel-shape geometry with a deeper cylindrical shaft. Rubble fills the base of the shaft.

This 3D thermal map shows the new geometry of Halema‘uma‘u Crater. Magma in the summit magma chamber has drained over the past month due to Kīlauea's lower East Rift Zone eruption, causing much of t

This is a video compilation from a helicopter overflight of Kīlauea Volcano's lower East Rift Zone on June 6, 2018, around 6:30 AM. The video shows the fissure 8 lava fountain feeding a channelized lava flow that travels northeast around the Kapoho cone, and then flows toward the south to enter the ocean at Kapoho Bay and Vacationland.

Unmanned Aircraft Systems (UAS) conducted a mission on Kīlauea Volcano's lower East Rift Zone to collect video of flowing lava in the upper lava channel of fissure 8. Scientists use the video to assess lava flow velocities, which are measured by tracking surface features in the stationary video view.

USGS Hawaiian Volcano Observatory, Status of Kīlauea Volcano, 9:30am HST, June 6, 2018, Jessica Ball, USGS Volcanologist
 

This is a video compilation from a helicopter overflight of Kīlauea Volcano's lower East Rift Zone on June 6, 2018, around 6:30 AM.

HVO's mid-day overflight on June 5 shows ongoing partial collapse of Halema‘uma‘u at the summit of Kīlauea Volcano. To the north of the former visitor Overlook parking area (closed in 2008) is the site of the former lava lake—now a deep hole piled with wall-rock rubble.

The fissure 8 lava fountain height has diminished. Previously, fountain heights reached a sustained 260 ft. During the overnight hours of June 4-5, fluctuating heights were measured at about 100 to 160 ft.

U.S. Geological survey scientists use fly-overs to track active lava flows. 

U.S. Geological survey scientists use fly-overs to track active lava flows. 

USGS Hawaiian Volcano Observatory Update of Kīlauea Volcano for June 4, 2018. On Camera: Jessica Ball, USGS Volcanologist.
 

Video from helicopter overflight of Kīlauea Volcano's lower East Rift Zone on June 4, 2018, shows lava from fissure 8 entering the ocean at Kapoho Bay. View to the north.

This short video compilation shows conditions at Kapoho Bay during a helicopter overflight on June 4, 2018, around 6:15 a.m. HST and again around 1:38 p.m. HST.

Beginning on June 3, lava from fissure 8 entered the ocean at Kapoho Bay. By June 6, lava had completely filled Kapoho Bay and built a delta that now extends over a mile from shore.