(ABOVE VIDEO) During a press conference held on Saturday afternoon, Janet Babb with the U.S. Geological Survey’s Hawaiian Volcano Observatory answers questions from local and national media about how long this current lava flow – and eruption – is expected to continue.
This is a common discussion at media conferences these days. Residents who live on the island are familiar with the ways of the volcano, but for the visiting members of the national media, the question of “how long” is often asked. USGS HVO scientists usually provide the answer, as Babb does in this video. Even with the current stall at the flow front, there are no signs that the June 27 lava flow is about to end, or that the 31 year eruption of Pu’u O’o is nearing a finish.
This week’s Volcano Watch article – written by the scientists of the USGS Haawaiian Volcano Observatory – details the starts and stops of the current lava flow endangering Pahoa town.
Just over a week ago Kīlauea Volcano’s June 27th lava flow was barely moving forward, but then it surged into Pāhoa. With that in mind, the USGS Hawaiian Volcano Observatory (HVO) is using this Volcano Watch article to summarize how the lava went from being a somewhat distant threat to an immediate one in just a few days.
In mid-October, following weeks of relatively slow advance—less than 1.6 km (1 mi) in three weeks—the leading edge of the June 27th lava flow stalled. While there were no illusions that it had stopped for good (there were still plenty of lava outbreaks behind the flow front, indicating that it remained active), residents downslope of the lava flow were granted some extra time to prepare for its possible arrival. The threat may even have seemed a bit abstract, with lava still more than 1 km (0.6 mi) upslope of Apa‘a Street/Cemetery Road and almost 2 km (1.2 mi) from Pāhoa Village Road.
The situation began to change on October 13, when a narrow finger of lava broke out from behind the flow front and moved along the southeast margin of the existing flow, at times reaching rates over 150 m (165 yd) per day. On October 22, the narrow finger overtook the stalled flow front and became the leading edge of the flow. The following day it advanced 390 m (430 yd), due in part to a local gully, which narrowed and focused the lava flow.
On Saturday, October 25, at 3:20 a.m., HST, lava reached Apa‘a Street—a milestone with historical, geographical, and psychological implications. The June 27th flow had entered the community of Pāhoa and was impacting human infrastructure.
Pushing closer towards town, lava inundated the Pāhoa cemetery, just 0.8 km (0.5 mi) from Pāhoa Village Road, on the morning of October 26. By that afternoon, the flow was moving through a grassy field and adjacent forest, and burning vegetation resulted in frequent, and often loud, methane blasts. These blasts—common wherever lava encounters vegetation—are a significant, yet underappreciated, hazard to anyone nearby.
As lava moves through vegetated ground, plant materials covered by the flow, including roots, continue to burn. This burning produces methane, which can accumulate beneath the flow and, under certain circumstances, burst through the flow surface or along the flow margins. Occasionally, the methane bursts can be quite large—powerful enough to throw hot rock (and anyone standing on it) into the air.
Moving at 5-10 meters (yards) per hour, with the advance rate varying due to changes in the slope of the land, the lava flow reached a fence line marking private property on the morning of October 28. As it moved through the private land, the lava engulfed everything in its path, including a utility shed, trees in a small macadamia nut orchard, and a pile of tires. The burning tires produced a thick plume of black smoke that was visible for miles, causing both interest and concern among Pāhoa and nearby residents!
Over the subsequent days, the lava flow continued to advance through private property toward Pāhoa Village Road, although the advance rate of the flow front slowed to only a few meters (yards) per hour, and eventually stalled on October 30. Such slowdowns are common in pāhoehoe flows. Breakouts upslope of the flow front can divert supply away from the leading edge, and flow inflation can cause the flow to thicken instead of pushing forward.
Nevertheless, it is important to remain vigilant. Inflated flows can suddenly burst forth, releasing streams of lava that can move rapidly over small distances—behavior that was common in the days prior to the October 30 slowdown. In addition, we expect the flow to continue to widen as breakouts upslope fill in places that were initially bypassed by the leading edge. The process of inflating, surging, and widening is the pattern by which pāhoehoe lava flows grow.
HVO and Hawai‘i County Civil Defense are monitoring the ongoing lava flow activity around the clock to keep abreast of these and other developments. Maps, photos, and detailed updates are posted on the HVO and Civil Defense websites at http://hvo.wr.usgs.gov and http://www.hawaiicounty.gov/active-alerts/.USGS Hawaiian Volcano Observatory Volcano Watch on Oct. 30, 2014