During 31 August-6 September HVO reported that the lava lake continued to rise and fall, circulate, and spatter in Kīlauea's Overlook vent. Incandescence was evident in webcam images from several long-established vents on Puʻu ʻŌʻō Crater's floor. A collapse at the W vent increased the size of the vent and a 40-m-diameter lava pond that was 23 m below the vent's rim. The 61G lava flow, originating from a vent on Puʻu ʻŌʻō Crater's E flank, continued to enter the ocean at multiple areas near Kamokuna and spanning about 1 km of coastline and increasing the size of the lava delta at the base of the sea cliff. Scattered breakouts were active on the coastal plain and the pali.

Source: US Geological Survey Hawaiian Volcano Observatory (HVO)

Geological Summary. Kīlauea overlaps the E flank of the massive Mauna Loa shield volcano in the Island of Hawaiʻi. Eruptions are prominent in Polynesian legends; written documentation since 1820 records frequent summit and flank lava flow eruptions interspersed with periods of long-term lava lake activity at Halemaʻumaʻu crater in the summit caldera until 1924. The 3 x 5 km caldera was formed in several stages about 1,500 years ago and during the 18th century; eruptions have also originated from the lengthy East and Southwest rift zones, which extend to the ocean in both directions. About 90% of the surface of the basaltic shield volcano is formed of lava flows less than about 1,100 years old; 70% of the surface is younger than 600 years. The long-term eruption from the East Rift Zone between 1983 and 2018 produced lava flows covering more than 100 km², destroyed hundreds of houses, and added new coastline.