On trade wind days, which prevail much of the year, visitors to Kilauea’s summit are greeted by the majestic sight of a towering eruption plume that drifts to the southwest. At night, the deep red glow of the lava lake’s overturning surface is reflected by the fume above the vent within Halemaumau Crater.
On trade wind days, which prevail much of the year, visitors to Kilauea’s summit are greeted by the majestic sight of a towering eruption plume that drifts to the southwest. At night, the deep red glow of the lava lake’s overturning surface is reflected by the fume above the vent within Halemaumau Crater.
The plume and nighttime glow wax and wane, but the sensory experience is normally visual (and perhaps spiritual). Until recently, that is.
For the past several months, lava within the summit vent has been slowly and fitfully rising. As of Oct. 5, lava reached a level that covered the previous high-lava “bathtub” ring within the vent. This is when the other human senses — sound, smell, taste and feel — became more engaged by the eruption, even as far away as the Jaggar Museum Overlook in Hawaii Volcanoes National Park.
The rising level put hot lava much closer to the cooler rock than it had been before, causing rapid heating, expansion and cracking of the vent walls. This caused bangs and booms that could easily be heard at Jaggar Museum because the trade winds, which usually steer sound away from the overlook, had ceased. In their place, gentle Kona breezes carried the rock-breaking sounds to the overlook, as well as the pungent smell and taste of sulfur dioxide gas in the plume and some fine strands of Pele’s hair.
The rise in lava level within the vent is associated with a modest uplift and expansion of Kilauea’s summit area. The root cause for this expansion isn’t clear. It’s not likely because of an increase in magma supply from depth, because a significant increase in carbon dioxide emissions, which would reasonably accompany increased magma supply, has not been observed. Another possible explanation for the uplift and expansion is a backup of magma caused by a constriction in the volcanic plumbing system between the summit magma reservoir and the active Puu Oo eruptive vent on Kilauea’s east rift zone.
There are some observations and data that support the possibility of a summit-rift constriction. For instance, when the lava lake level within the summit vent was previously as high as it is now, the lava in east rift zone vents was also at the same high level, minus about 260 feet of frictional “head loss.” The reason for this lava level similarity is that the summit and rift vents, while more than 11 miles apart, are hydraulically connected. This connection has been responsible for significant east rift eruptive changes that occur in response to variations in summit activity, particularly during the past several years.
On at least three occasions between March and September 2011, the level of the lava lake within the summit vent was unusually elevated. This condition caused increased pressure within the east rift plumbing system, resulting in notable eruptive outbreaks: the short-lived Kamoamoa fissure eruption just uprift of Puu Oo and two subsequent events in which Puu Oo was split open along its flanks.
For the last several months, lava within Kilauea’s summit vent has been at its highest level since the summit eruption began in 2008, and yet it appears the associated high summit pressure has not significantly transmitted down the volcano’s east rift. The lava level within Puu Oo crater, while elevated, is not extraordinarily so. And even though lava is flowing through a tube near the base of the Puu Oo cone, flows haven’t reached the ocean in nearly a year.
A steady decrease in Kilauea’s east rift zone gas emissions since August also suggests a decrease in magma flow between the summit and east rift zone.
One possible outcome of continued summit expansion and lava level rise could be an eventual outpouring of lava on the floor of Halemaumau Crater. Alternatively, the increased pressure might overcome the apparent constriction, resulting in an outbreak somewhere between the summit and Puu Oo, akin to the March 2011 Kamoamoa fissure eruption.
Time will tell what happens next. For now, visitors to Kilauea’s summit can continue to watch the show and listen to the symphony of bangs and booms.
Kilauea activity update
A lava lake within the Halemaumau Overlook vent produced nighttime glow that was visible from the Jaggar Museum overlook and by Hawaiian Volcano Observatory’s webcam during the past week. The lava lake level rose to a new high, about 165 feet below the floor of Halemaumau Crater, during a prolonged period of summit inflation that ended Tuesday. As of this writing on Thursday, the lava lake remains high, but the level could begin to fluctuate if back-to-back deflation-inflation events resume.
On Kilauea’s east rift zone, surface lava flows continued to accumulate at the base of the Pulama pali within the abandoned Royal Gardens subdivision. One branch extended seaward across the coastal plain, reaching about a mile from the shoreline on Wednesday, but was moving slowly. Within the Puu Oo crater, the lava pond in the northeastern pit continued to circulate and was visible in the webcam over the past week.
No earthquakes were reported felt in the last week below the island of Hawaii.
Visit the HVO Web site at hvo.wr.usgs.gov for detailed Kilauea, Mauna Loa and Hualalai activity updates, recent volcano photos, recent earthquakes and more; call 967-8862 for a Kilauea summary; email questions to askHVO@usgs.gov.
Volcano Watch is a weekly article and activity update written by scientists at the U.S. Geological Survey’s Hawaiian Volcano Observatory.