U.S. Geological Survey - Hawaiian Volcano Observatory
Kilauea - Eruption Summary - Hazards - History
This update current as of June 5, 1998. Eruption updates are posted monthly; more frequent updates will accompany drastic changes in activity or increased threat to residential areas.
[Previous eruption updates may be accessed through our archive index.]
Episode 55 of Kilauea's east rift zone eruption continues. On most days lava issues quietly from vents on the SW flank of Pu`u `O`o and travels about 12 km through lava tubes to the coast. Several vents within Pu`u `O`o crater are intermittently active. For example, over a several-hour period, lava will emerge from one or more of these vents, sometimes reaching to within 10-30 m of the crater rim, then suddenly drain back into one or more of the vents (activity occurring within Pu`u `O`o is documented by the remote video-telemetry system; see images below recorded on June 4). Such lava fill and drain cycles occur irregularly. This activity, however, does not appear to affect the steady flow of lava through the tube system into the ocean. Between 300,000 to 600,000 m3 of lava continues to enter the ocean at two entry points -- Waha`ula and Kamokuna.
Pu`u `O`o crater has a major vent at its west end, a feature we call the crater vent. Several smaller pits have formed elsewhere across the crater floor; a new one developed at the base of the east crater wall on May 7. Such pits form by undermining as magma beneath the crater floor erodes parts of the solidified crust. Where the crust becomes thin, the floor collapses to form a pit, which may become a new vent or a place where lava can drain back into the main magma conduit system beneath the cone. These pits periodically overflow and spill small lava flows across the crater floor. All these flows remain contained within the crater of Pu`u `O`o. The most recent crater overflow occurred in January 18, 1998.
A temporary pause in the supply of magma to Pu`u `O`o on May 19-20 permitted lava within the tube system to drain completely so that lava ceased flowing into the ocean at the Waha`ula and Kamokuna entry points. After lava began re-entering the tube system during the evening of May 20, several breakouts occurred along the length of the tube. The most voluminous breakouts began early in the morning of May 21 on the steep slope of the pali between 2,000 and 1,100 feet.
During a pause, the roof and walls of the drained tubes are prone to collapse. When lava reoccupies the tube system, blockages or irregularities in the tube cause the lava to back up and escape through skylights or other weak points. A prolonged period of surface flow activity inevitably results in lateral expansion of the lava-flow field, because the middle of the field is usually higher than the sides and new surface flows are diverted to the edges. During this most recent pause, however, the tube system quickly accommodated nearly all of the lava. The Kamokuna entry point resumed abruptly at about 1240 on May 21. Sixteen similar pauses have occurred since episode 55 began in March 1997.
May 21, 1998. Aerial view SW across one of the lava breakouts that occurred when magma was resupplied to Pu`u `O`o and the tube system. The lava channel spreading from the tube's skylight is feeding an `a`a flow that is moving down the pali (left) out of view.
May 21, 1998. Aerial view to SW above a breakout from the lava tube on the steep pali about 6 km from Pu`u `O`o. The breakout is feeding an `a`a lava flow that reached the base of the pali. This breakout ceased within a few hours after this image was taken as the tube system accomodated more of the erupting lava./i>
May 21, 1998. Lava breakout moves through a forested kipuka.
May 21, 1998. Close view of lava cascading down a steep slope within a lava tube as lava re-occupies the tube system. The cascade is about 2 m high, but the entire cascade is hidden from view by the roof of the tube, which is estimated to be about 6 m high.
June 4, 1998. Aerial view to NW shows the underground path of the lava tube that leads from Pu`u `O`o (6 km in distance) over the steep pali (foreground) and to the sea. The tube's path is marked by the blue-colored fume that rises from skylights and other weak points in the roof of the tube.
At the coast, the tube system continues to discharge lava into the ocean at two sites, Waha`ula and Kamokuna. Most of the lava enters the ocean at the Kamokuna entry point, where new land collapses into the ocean without warning and various types of littoral explosions occur frequently. Following a collapse of the Kamokuna bench sometime between May 1 and 4, a new bench about 90 m wide was built by June 2. Numerous breakouts have been occurring along the entire bench area, and prominent cracks have formed immediately behind a new littoral cone that is forming on the seaward edge of the new bench. This bench is susceptible to collapse, which is likely to trigger vigorous explosions and scalding waves that can endanger people who venture too close to the entry point.
June 4, 1998. Aerial view to SW shows the Waha`ula (bottom) and Kamokuna (upper) lava entry points on the south coastline of Kilauea Volcano. The three small but distinct plumes rising from the Waha`ula entry point indicate that lava is entering the sea at three different points. In the past few weeks, most lava poured into the sea at the Kamokuna entry.
May 7, 1998. View is SW across the Kamokuna entry a few days after new land (lava bench) seaward of the littoral cone collapsed into the ocean. The cone is about 10 m tall. By June 2, a new bench about 90 m wide had formed.
May 25, 1998. View is SW across a new bench forming at the Waha`ula entry point. Following the brief pause on May 19-20, many small breakouts from the lava tube feeding this entry point poured over the 3-to 4-m-tall cliff onto the bench. The cliff was created when an older bench collapsed into the ocean.
As the lava enters the sea it builds new land along the ocean edge. This land proves unstable, owing to the steep submarine slope along the south coast of the Big Island. The lava builds a low shelf known as a bench, but periodically the bench and its underpinnings slide seaward, a process called bench collapse. These collapses are life endangering; the land itself is destroyed and numerous explosions ensue as the hot lava reacts violently with the ocean water. For more information about this activity and the associated hazards, see:
Eruption-viewing opportunities change constantly, so those readers planning a visit to the volcano should contact Hawai`i Volcanoes National Park for the most current eruption information (ph. 808-985-6000). Additional photographs and descriptions of east rift eruptive activity may be found on the University of Hawai`i's web site.
Flow-field map showing lava emplaced during the Pu`u `O`o - Kupaianaha eruption since 1983. Note the new lava flows that were emplaced on the Pulama pali and at the Kamokuna and Waha`ula entry points following the brief pause May 19-20. This map was compiled on June 5, 1998.