Lava from fissure 8 meets ocean at the Kapoho bay

Overflight photograph at approximately 6:13 a.m. HST shows the lava flow originating from Fissure 8 (not visible in photograph) entering Kapoho Bay. The ocean entry was reported to have occurred by 10:30 p.m. on the night of June 3, 2018.

The lava from fissure 8 entered the ocean at  Kapoho Bay at about 10:30 PM HST on June 3 generating a laze plume that is blowing inland but dissipating quickly. As of today morning, the lava is also constructing a delta in Kapoho Bay extending a few hundred yards into the bay.

The lava flow front is half a mile wide. A sluggish lava flow was observed in the vicinity of fissure 18 and rest of the fissures are all inactive.

Volcanic gas emissions remain very high from the fissure eruptions and also at the summit. Trade wind conditions are bringing vog to the south and west sides of the Island of Hawaii. Afternoon easterly winds may bring vog to communities in the Volcano area.

Inward slumping of the rim and walls of the walls of Halema`uma`u continues in response to persistent subsidence.

The USGS is predicting an increased earthquake activity in the coming days.

Some of the photos from USGS update today:

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.

What a difference four days makes! These thermal images of fissure 8 fountains erupting on Kīlauea's lower East Rift Zone show a few things: 1) The lava fountains have gained height—with the tallest one growing from 150 ft to over 250 ft. 2) A pu‘u (cone) has built up downwind. 3) The amount of material wafting downwind is greater. Scientifically, we know the fountain temperatures are reaching up to about 2040 degrees F (1115 C). The composition of the lava erupted has high MgO (magnesium oxide) values, which comes from olivine crystals that are being pulled from deep in the rift zone.