HVO reported that lava from a vent on the inner NW wall of Kilauea’s Halema`uma`u Crater streamed down the cone into a perched lava lake during 3-9 February. The western half of the lake dropped from 213 m on 3 February to 211 m on 4 February and stayed at that level during 5-6 February; the drop in lake level was likely the result of summit deflation that was detected by tiltmeters. The lake level had risen to 214 m by the morning of 7 February coincident with the onset of summit inflation. A small dome fountain was visible at the entry point of lava into the lake on 8 February. The stagnant E half of the lake, separated by a series of surface cracks, was about 5 m lowed than the W half.

Geological Summary. Kilauea overlaps the E flank of the massive Mauna Loa shield volcano in the island of Hawaii. 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 Halemaumau 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.

Source: US Geological Survey Hawaiian Volcano Observatory (HVO)