Hawai'i Volcanoes National Park's Kīlauea Volcano vented its fury during 2018/USGS
Editor's note: Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.
Five years ago, volcanic activity at Kīlauea dramatically changed when magma intruded into the lower East Rift Zone (LERZ). What happened at Kīlauea in 2018? What have been the resulting learning opportunities?
An aerial view looking downrift from Leilani Estates at erupting fissures 5, 6, 19, and 22. Ponded lava from these fissures fed lava channels moving downslope, right side of the image, including the channels that fed the ocean entries just north of MacKenzie State Park. USGS photo taken on May 22, 2018, by S. Isgett.
An image taken from the visitor viewing area in front of the Jaggar Muesum, at the summit of Kīlauea, at 7:45 a.m. HST on May 16, 2018. Explosive episodes from the previous night created ash falls which blanketed the surrounding landscape.
The sequence of events began on April 30, 2018, when Pu‘u‘ō‘ō crater floor collapsed as magma began intruding downrift. Over the next several days seismic and deformation data tracked the dike as it migrated underground farther down the East Rift Zone.
The first LERZ eruption in 58 years began on the evening of May 3 when a fissure opened in Leilani Estates Subdivision. By the end of May 4, six fissures had opened in the LERZ and a magnitude-6.9 earthquake struck the south coast of the Island of Hawai‘i.
The summit lava lake level began to drop as magma moved into the LERZ, and sections of the unsupported crater walls fell into the lake, triggering small explosive events. Hawai‘i Volcanoes National Park closed to the public on May 11, and Hawaiian Volcano Observatory (HVO) staff vacated the office on Uēkahuna bluff on May 16 due to increased ash explosions, seismic activity, and building damage.
From early-May to late-August, HVO staff, with help from the USGS Volcano Science Center, the University of Hawai‘i, and other Department of the Interior offices, maintained a 24-hour field presence and data watch to monitor the eruption and communicate any changes to the public and emergency managers. These collaborations were essential for continuous monitoring and data analysis, but they also introduced new monitoring techniques like using Unoccupied Aircraft Systems (UAS). UAS flights are now included as part of HVO’s routine eruption monitoring tasks.
The 2018 eruption was the most destructive over the last 200 years in Hawai‘i, with 24 fissures covering an area of over 8,700 acres (35.5 square km) including the addition of 875 acres of new land beyond the old coastline. Over 700 structures and 30 miles (48 km) of roads were covered, displacing many residents. Gas emissions were at the highest levels ever recorded at Kīlauea and impacted much of the State of Hawaii and areas as far away as Guam.
The summit region experienced 62 total collapse events during the eruption. These near-daily occurrences each released energy roughly equivalent to a magnitude-5.3 earthquake. Shaking from these events caused damage to nearby homes and businesses, along with Hawai‘i Volcanoes National Park roads and infrastructure and the former HVO building. Volcanic ashfall from explosions in May, and gas emissions, also impacted downwind communities in the District of Ka‘ū.
Recovery efforts are still underway for Island of Hawai‘i communities impacted by the 2018 eruption, and for HVO.
Some of HVO’s new monitoring capabilities include cutting edge field equipment for tracking seismicity, ground deformation, gas, gravity, lava lake level, and surface changes. Lab equipment that can analyze physical and chemical characteristics of ash and cinder and lava samples, providing insights on eruptive processes, has also been acquired thanks to the Supplemental funding.
Exciting new research has also been taking place at Kīlauea to help improve our understanding of the volcano’s magma plumbing system and structure, eruptive past, and hazards. This includes the ongoing Kīlauea Seismic Imaging Project.
In the years since 2018, HVO has had the opportunity to apply lessons learned during 2018 to several Kīlauea summit eruptions and the first Mauna Loa eruption in 38 years. Research and monitoring upgrades funded through the Supplemental Funding have advanced our understanding of Hawaiian volcanoes, helping us to learn more about their hazards and potential future eruption impacts.
Kīlauea is not erupting. Its USGS Volcano Alert level is ADVISORY.
Webcams show no signs of active lava in Halemaʻumaʻu crater, at the summit of Kīlauea in Hawai‘i Volcanoes National Park. Over the past week, summit tiltmeters showed inflation and seismicity has been variable. The summit sulfur dioxide (SO2) emission rate was most recently measured on May 3, when it totaled 135 tonnes per day.
Mauna Loa is not erupting. Its USGS Volcano Alert Level is at NORMAL.
Webcams show no signs of activity on Mauna Loa. Seismicity remains low. Summit ground deformation rates show inflation above background levels, but this is not uncommon following eruptions. SO2 emission rates are at background levels.
There were two earthquakes with 3 or more felt reports in the Hawaiian Islands during the past week: a M3.0 earthquake 4 km (2 mi) SSE of Pāhala at 31 km (19 mi) depth on April 29 at 6:34 p.m. HST and a M0.5 earthquake 4 km (2 mi) SW of Volcano at 1 km (0 mi) depth on April 27 at 7:59 a.m. HST.
HVO continues to closely monitor Kīlauea and Mauna Loa.
Please visit HVO’s website for past Volcano Watch articles, Kīlauea and Mauna Loa updates, volcano photos, maps, recent earthquake information, and more. Email questions to [email protected].
