Report on Kilauea (United States) — July 1986
Scientific Event Alert Network Bulletin, vol. 11, no. 7 (July 1986)
Managing Editor: Lindsay McClelland.
Kilauea (United States) Episode 48 from three new fissures
Please cite this report as:
Global Volcanism Program, 1986. Report on Kilauea (United States) (McClelland, L., ed.). Scientific Event Alert Network Bulletin, 11:7. Smithsonian Institution. https://doi.org/10.5479/si.GVP.SEAN198607-332010.
19.421°N, 155.287°W; summit elev. 1222 m
All times are local (unless otherwise noted)
Episode 48 (E-48). "After 22 days of repose, E-48 . . . began on 18 July with a local earthquake swarm and eruptions from new fissures on both the uprift and downrift sides of the Pu`u `O`o cone. At the time of the swarm, the magma column had reached the top of the conduit and was emitting spatter from a 15-m-high cone within Pu`u `O`o, but as fissures opened, the column subsided, the top of the spatter cone collapsed, and only burning gas issued from the small opening for the duration of the activity. After nearly 23 hours, activity ended temporarily on 19 July at around 0930. Mostly pahoehoe flows were produced. The longest flow moved rapidly SE for 7.5 km through a forested part of the Hawaii Volcanoes National Park to within 2.5 km of the sea. The Chain of Craters road was closed briefly until the flow stagnated, and ~4 km2 of forest were burned.
"On 20 July at about 0830, following 23 hours of inactivity, low fountains on the downrift fissure ("B" on figure 44) were first observed by a National Park Service overflight while the "A" fissure and the main Pu`u `O`o conduit remained quiet. By 0950, the "B" fissure had shut down and a new fissure ("C" on figure 44) had begun to erupt along a line parallel to, and ~150 m N of, the original January 1983 fissure. Low fountains, a few meters high, played intermittently along the 1100-m-long fissure, which eventually shortened to a pair of vents, < 50 m apart, that have continuously produced lava at a low rate. A pahoehoe shield, ~1.2 km2 in area and > 25 m high, has been built around the vents and a branching tube-fed pahoehoe and aa flow has moved ~4.5 km SE toward the sea. By the end of July, it had stagnated and remained ~6 km upslope from the nearest developed area. As of 8 August, lava was still welling out of one main vent without fountaining and was spreading over the summit of the growing shield. The new basalt flows have sparse small (<1 mm) olivine phenocrysts, similar to those of recent eruptions.
|Figure 44. Sketch map of eruptive fissures A-C and lava flows on Kilauea's East rift zone, July 1986. Courtesy of HVO.|
"The earthquake swarm . . . began on 18 July at 1046 and progressed downrift. It was recorded by seismometers just uprift of Pu`u `O`o and N of Kalalua. High tremor amplitudes on the uprift seismometer characterized the early phase of activity. From 20 July on, the tremor on the uprift instrument decreased to background levels, while very low-amplitude tremor has continued on the downrift instrument nearest the eruption vent. Above-normal levels of long-period seismicity occurred following the early activity of E-48 (figure 45).
"Deflationary summit tilt began on 18 July at about 1145, an hour after the onset of seismicity, and reached a record rate of nearly 3.1 µrad/hour between 1200 and 1300 (figure 45). The deflationary pattern reversed temporarily into an inflationary trend from about 0500 on 19 July, in concert with the short repose period. Since 20 July, tilt changes have been very small and no particular trend has been defined."
Geologic Background. 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.
Information Contacts: G. Ulrich, HVO.