HVO: Kīlauea Under Sea Impacts Explored

Nighttime scene from shipboard of lava entering the Pacific Ocean on July 12, 2018, captured from a scientific research vessel deploying submarine seismometers. Photograph courtesy of Jackie Caplan-Auerbach, Western Washington University. PC: USGS/HVO

The visible part of Kīlauea from the summit to the Lower East Rift Zone makes up only a small portion of the total volcano. Much of Kīlauea lies beneath the sea, including the Puna ridge to the east, and the south flank extending offshore beyond the southern coastline.

As the volcano grows, this underwater region of the south flank creeps slowly to the south, moving in fits and starts with earthquakes that last seconds (such the May 4, 2018, magnitude-6.9 event) and in slow slip events, which last for days or weeks. Many questions have been raised about the stability of the south flank, since other portions of Hawai`i Island’s coasts show evidence of past landslides.

Although Kīlauea’s submarine south flank is a major part of the volcano, its motion is much harder to monitor than is the part above sea level. While we can record earthquakes occurring beneath the flank, only the largest, and those closest to shore, are well-captured by the USGS Hawaiian Volcano Observatory seismic network. In general, only a few offshore earthquakes are recorded. However, following the M6.9 earthquake and Kīlauea’s LERZ eruption, a significant number of earthquakes took place beneath the south flank, some of which were in regions that have not typically been very seismically active.

University students assisted with deployment of ocean-bottom seismometers off the south coast of Kīlauea Volcano from the deck of the R/V Ka`imikai-o-Kanaloa, a 223-foot research vessel operated by the University of Hawai‘i, on July 10, 2018. Photograph courtesy of Jackie Caplan-Auerbach, Western Washington University. PC: USGS/HVO

To better understand what’s going on within Kīlauea’s south flank and help determine how it has been affected by the eruption, a group of scientists from Western Washington University, Rice University, and the University of Rhode Island deployed 12 ocean bottom seismometers (OBSs) on the submarine Kīlauea south flank in July.

The instruments were deployed from the R/V Ka`imikai-o-Kanaloa, a 223-foot research vessel operated by the University of Hawai‘i during a week-long cruise funded by the National Science Foundation.

Seismometers were positioned over the whole south flank so that earthquakes associated with the edges of the flank could be recorded to see if the offshore stress field has changed. They were also positioned on the M6.9 aftershock zone to try to better understand that earthquake, and near the LERZ eruption ocean entry to study how lava enters the water and progresses downslope.

These data should allow the scientific team to determine more precisely where the offshore earthquakes occurred and on what fault(s) the M6.9 earthquake took place. Recordings of the ocean entry activity may help us learn more about why some lava-water interactions are explosive, while others are relatively calm. In general, we hope that by collecting data offshore we will be able to better understand parts of Kīlauea that cannot be easily observed.

The OBSs record data internally, so we won’t know what they have recorded until they are recovered in September. A group of scientists on a related research cruise have volunteered their time to collect our instruments and download the data for us. At that point the data will be made available to any scientists interested in studying them, notably the seismologists at HVO.

While aboard the ship, we had a view of the eruption that was both spectacular and sobering. The power and volume of lava flowing from fissure 8 to the sea was striking, even from miles offshore. We saw dozens of ocean entries over miles of coastline, and changes in the color of the seawater, even miles offshore. But we were also witness to the pain of the eruption, watching black smoke as a structure burned, knowing that it was yet another loss among many in the vibrant community. Our thoughts continue to be with the people of Puna.

Volcano Activity Updates

Activity on Kīlauea’s lower East Rift Zone and at the summit of the volcano remained greatly diminished this past week. LERZ activity was limited to a small crusted-over pond of lava deep within the fissure 8 cone and a few scattered streams of lava entering the ocean. Summit earthquakes remained at low levels. The last summit collapse event occurred on August 2, and no significant subsidence has been observed since August 4. However, hazardous conditions remain in both areas. Residents in the lower Puna and Kīlauea summit areas on the Island of Hawaiʻi should stay informed and heed Hawai‘i County Civil Defense closures, warnings, and messages (http://www.hawaiicounty.gov/active-alerts). HVO daily status reports are posted at https://volcanoes.usgs.gov/volcanoes/kilauea/status.html.

Two earthquakes with three or more felt reports occurred in Hawaii this past week: a magnitude-2.6 earthquake 13 km (8 mi) southeast of Volcano at -1.0 km (-0.6 mi) depth on August 11, at 6:21 a.m. HST, and a magnitude-4.4 earthquake 15 km (9 mi) southwest of Leilani Estates at 8.0 km (5.0 mi) depth on August 9 at 6:50 a.m. HST.

At Mauna Loa, HVO geophysical monitoring networks indicate that earthquakes and deformation are near background levels, and the USGS Volcano Alert level for the volcano remains at NORMAL. HVO continues to monitor the volcano closely and will report any significant changes.

***Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates. This week’s article is by Jackie Caplan-Auerbach, Western Washington University; Julia Morgan, Rice University; and Yang Shen, the University of Rhode Island.***