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Report on Kilauea (United States) — 4 September-10 September 2002


Kilauea

Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
4 September-10 September 2002
Managing Editor: Gari Mayberry

Please cite this report as:

Global Volcanism Program, 2002. Report on Kilauea (United States). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 4 September-10 September 2002. Smithsonian Institution and US Geological Survey.

Weekly Report (4 September-10 September 2002)

Kilauea

United States

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

All times are local (unless otherwise noted)


During 3-9 September, lava continued to flow SE down Paliuli and Pulama pali, and many surface lava flows were visible on the coastal flat. Lava began to enter the ocean on 3 September. Seismicity was generally at normal levels. The swarm of long-period earthquakes and tremor that had been occurring since early June returned to moderate-to-low levels. There were small episodes of inflation and deflation at Uwekahuna and Pu`u `O`o for several days.

Geological Summary. Kilauea, which overlaps the E flank of the massive Mauna Loa shield volcano, has been Hawaii's most active volcano during historical time. Eruptions are prominent in Polynesian legends; written documentation extending back to only 1820 records frequent summit and flank lava flow eruptions that were interspersed with periods of long-term lava lake activity that lasted until 1924 at Halemaumau crater, within the summit caldera. The 3 x 5 km caldera was formed in several stages about 1500 years ago and during the 18th century; eruptions have also originated from the lengthy East and SW rift zones, which extend to the sea on both sides of the volcano. About 90% of the surface of the basaltic shield volcano is formed of lava flows less than about 1100 years old; 70% of the volcano's surface is younger than 600 years. A long-term eruption from the East rift zone that began in 1983 has produced lava flows covering more than 100 km2, destroying nearly 200 houses and adding new coastline to the island.

Source: US Geological Survey Hawaiian Volcano Observatory (HVO)