Logo link to homepage

Report on Kilauea (United States) — 22 October-28 October 2008


Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 22 October-28 October 2008
Managing Editor: Sally Sennert.

Please cite this report as:

Global Volcanism Program, 2008. Report on Kilauea (United States) (Sennert, S, ed.). Weekly Volcanic Activity Report, 22 October-28 October 2008. Smithsonian Institution and US Geological Survey.

Weekly Report (22 October-28 October 2008)


United States

19.421°N, 155.287°W; summit elev. 1222 m

All times are local (unless otherwise noted)

HVO reported that during 22-28 October lava flowed SE through a tube system from underneath Kilauea's Thanksgiving Eve Breakout (TEB) and rootless shield complex, reaching the Waikupanaha ocean entry. Lava flow production possibly paused during 26-27 October. Multiple surface lava flows on the pali were noted. On 23 October, a plume drifted above the County Viewing Area near the ocean entry and rained acid droplets, causing a closure. Explosions at the ocean entry were reported on 24 October. The sulfur dioxide emission rate at Pu'u 'O'o was 1,000 tonnes per day on 23 and 24 October, half of the background rate of the 2005-2007 average. Weak winds caused the viewing area to close again on 25 October.

During the reporting period, Kilauea earthquakes were variously located beneath and to the S of the caldera, along the S-flank faults, and along the SW rift zone. Beneath Halema'uma'u crater earthquakes ranged from less than 30 per day to 70 (background is about 40), but were too small to be located more precisely. The vent in Halema'uma'u crater continued to produce a predominantly white plume that drifted mainly SW. Night-time incandescence was intermittently seen at the base of the plume, and sounds resembling distant surf, rock clattering, and rock impacts were heard in the vicinity of the crater. Weak winds resulted in poor air quality at the summit during 21 and 25-28 October. During an overflight on 24 October, HVO geologists used a FLIR (Forward Looking InfraRed) camera to view the vent. The vent (about 80 m by 60 m) was wider than a lower orifice (about 30 m by 15 m), but narrower than a chamber above the orifice, resulting in an over-hanging vent rim prone to collapse. The sulfur dioxide emission rate was 500-900 tonnes per day during 22-24 October. The 2003-2007 rate average was 140 tonnes per day.

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)