U.S. Geological Survey scientists at the Hawaiian Volcano Observatory (HVO), scanning HVO’s Kilauea East Rift Zone webcam images, noted a new breakout of lava on Saturday, Nov. 15. It occurred in the vicinity of Pu‘u Kahauale‘a, a forested cone completely surrounded by Pu‘u ‘O‘o lava flows. This cone lies in the uppermost part of the June 27th lava flow, about 1.6 kilometers (1 miles) northeast of Pu‘u ‘O‘o. Throughout the day, helicopter pilots corroborated HVO’s observations.
U.S. Geological Survey scientists at the Hawaiian Volcano Observatory (HVO), scanning HVO’s Kilauea East Rift Zone webcam images, noted a new breakout of lava on Saturday, Nov. 15. It occurred in the vicinity of Pu‘u Kahauale‘a, a forested cone completely surrounded by Pu‘u ‘O‘o lava flows. This cone lies in the uppermost part of the June 27th lava flow, about 1.6 kilometers (1 miles) northeast of Pu‘u ‘O‘o. Throughout the day, helicopter pilots corroborated HVO’s observations.
HVO geologists continued to carefully monitor the flow field closer to Pahoa in the days following Saturday’s breakout. They found that the surface flows at the lower end of the flow field, including those near Apa‘a Street, the Pahoa Transfer Station, and the Pahoa Buddhist cemetery, gradually became less active. By Monday morning, Nov. 17, there was no surface activity on the flows near Pahoa — only glowing cracks in the hardened lava. This suggested that new lava was no longer reaching the lower section of the flow field.
Upslope, however, lava continued to break out of the tube near Pu‘u Kahauale‘a. Observers on Hawaii County Civil Defense (HCCD) and HVO helicopter overflights on Monday found that a series of new breakouts had also begun occurring progressively farther downslope along the tube system. It is reasonable to think that these upslope breakouts had, at least temporarily, diverted lava from the tube leading toward Pahoa.
The progression of these breakouts over time indicates that lava has been slowly reoccupying the lava tube downslope from Pu‘u Kahauale‘a. As of Thursday, Nov. 20, the breakout farthest downslope was about 2.5 kilometers (1.5 miles) southwest of Kaohe Homesteads.
Without lava flows posing immediate threats to the community, these recent changes have afforded us an opportunity to catch our collective breaths. The changes, however, have also ushered in a new phase of uncertainty about where these renewed surface flows will head.
Lava is currently breaking out of the tube at several locations, as well as milesgrating down the lava tube system. How far the lava will travel through the existing lava tube is not yet known, but based on flow activity in previous years, it is unlikely that lava will reoccupy the tube to the lowest part of the flow near Pahoa.
The farthest point at which lava breaks out of the tube and forms a surface flow could become the new flow front in the coming days. On the other hand, any of the existing upslope breakouts, such as the one near Pu‘u Kahauale‘a, could eventually capture much or all of the lava supply and become the new active front. In either case, the new active flow front will chart its own path downslope, which may or may not follow the route that the earlier part of the June 27th lava flow followed.
New breakouts from the tube are often forced to flow along the margin of the existing flow due to that flow’s inflated and elevated surface, thereby widening the overall flow field.
In some cases, this can cause the breakout of lava to head in a new direction and enter a different steepest-descent path (commonly shown by blue lines on HVO maps of the flow).
The recent upslope breakouts and subsequent interruption in lava supply to the flow front are typical aspects of pahoehoe lava flow behavior, and the sequence is similar to events repeatedly observed for earlier flows from Pu‘u ‘O‘o. Major interruptions can happen multiple times during the lifespan of an individual pahoehoe flow.
The recent stalling of flows near Pahoa is good news in the short term, but the ongoing breakouts from the June 27th lava tube clearly indicate that the flow is still active and remains a potential hazard to downslope communities. While it is unclear how far lava will be able to reoccupy the tube or where renewed surface flows milesght head, HVO and HCCD continue to monitor the flow closely with helicopter overflights, field work, satellite imagery, and other techniques.
Daily eruption updates, status reports, maps, photos, webcam images, and other information about KilaueaVolcano and the June 27th flow are available at http://hvo.wr.usgs.gov. A daily eruption update summary is also available by telephone at 967-8862.
Kilauea activity update
The June 27th lava flow from Pu‘u ‘O‘o remained active on Kilauea Volcano’s East Rift Zone. Breakouts were active along the milesddle to upper part of the flow field, between about 1.6 kilometers (1 mile) and 12 kilometers (7.5 miles) northeast of Pu‘u ‘O‘o. No surface flows were active north of Kaohe Homesteads or near Apa‘a Street and Pahoa. There was no significant change in activity at Pu‘u ‘O‘o.
The summit lava lake within Halema‘uma‘u Crater produced nighttime glow that was visible via HVO’s webcam over the past week. The lava level was relatively steady but began to drop on Wednesday, Nov. 19, with the onset of rapid DI deflation. As of this writing (Thursday, Nov. 20), the lava lake was about 45 meters (150 feet) below the rim of the Overlook crater.
One earthquake was reported felt in Hawaii during the past week. On Friday, Nov. 14, at 9:06 p.m., HST, a magnitude-3.6 earthquake occurred 9.7 kilometers (6.0 miles) northwest of Ka‘ena Point on the Island of Hawaii at a depth of 8 kilometers (5 miles).
Visit the HVO website (http://hvo.wr.usgs.gov) for past Volcano Watch articles and current 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.