A little more than 10 years ago, conditions around Kilauea Volcano’s summit were much different than today. The caldera floor was open to the public, and the air above it was normally clear. Halema‘uma‘u was an impressive sight, but peacefully in repose.
That quiet phase at Kilauea’s summit ended abruptly in 2008, ushering in a new era of lava lake activity that continues today.
Let’s review the past decade of this summit eruption.
After several months of increased seismic tremor and gas emissions, there was a small explosion in Halema‘uma‘u on March 19, 2008. The explosion marked the opening of a new crater, informally called the “Overlook crater.” During the remainder of 2008, several more explosions deposited spatter around Halema‘uma‘u, and the Overlook crater enlarged through collapses of its rim.
During 2009, small lava lakes were sometimes active deep within the Overlook crater. But since early 2010, the lava lake has been continuously present, steadily growing and rising higher.
The rise was interrupted March 5, 2011, when the lava lake briefly drained away because of the Kamoamoa eruption on Kilauea’s East Rift Zone.
The lava lake stabilized in 2012, rose to a higher level in 2013 and remained stable in 2014 and early 2015. In April 2015, the lava lake rose abruptly and briefly overflowed, spilling lava onto the floor of Halema‘uma‘u. High lake levels in 2016 allowed lava to be frequently observed from public viewing areas in Hawaii Volcanoes National Park, but a gradual drop in 2017 has made direct viewing of the lake less common during the past year.
The lava lake activity in 2018 is similar to that during the previous several years — relatively steady — and there are no signs that the summit eruption is slowing down.
Halema‘uma‘u now hosts one of the two largest lava lakes on Earth. It is likely the largest, but this cannot be said with complete certainty, as regular measurements are not available from the closest contender — Nyiragongo volcano in the Democratic Republic of the Congo.
Most persistent lava lakes are difficult to access, either because of geographic location (for example, Erebus in Antarctica) or political instability (for example, Nyiragongo). The size and accessibility of the Halema‘uma‘u lava lake, as well as the existing network of monitoring instruments, make it one of the premier locations to study lava lake behavior.
USGS Hawaiian Volcano Observatory scientists, along with collaborators from other institutions, are engaged in research to understand how the lava lake works and what it can tell us about the behavior and hazards of Kilauea.
For instance, we learned that the lake rises and falls in concert with changes in summit ground tilt. This tells us that the lake responds to the pressure of the magma chamber, so the lake level can be used like a pressure gauge.
The lake also fluctuates in concert with the lava pond at Pu‘u ‘O‘o on Kilauea’s East Rift Zone, illustrating the hydraulic connection between the two eruption sites. Lava chemistry at the two sites also is similar, adding further evidence of a close connection.
Another important finding deals with the nature of small explosions that occur at the lava lake from time to time.
HVO webcams revealed that the explosions are triggered by rockfalls from the Overlook crater rim impacting the lake surface. This observation is further evidence that the lava lake is very gassy, akin to lava foam. Rocks falling into this gas-rich, frothy lava triggers violent releases of gas that send spatter flying.
While the summit eruption has benefited science, it comes with many challenges, including persistent volcanic air pollution (vog) resulting from elevated sulfur dioxide gas emissions from the lava lake. Vog impacts the entire state at times, but the Ka‘u and Kona districts on the Island of Hawaii have been particularly hard hit.
Kilauea has a history of long-lasting summit eruptions, but it remains to be seen if the current eruption will go on for another decade. The past few years of stable activity suggest the summit lava lake is likely to continue into the near future.
However long it lasts, HVO will continue to study this awe-inspiring, unique feature to discover what more it can reveal about the volcano.
Volcano activity updates
This past week, Kilauea Volcano’s summit lava lake level fluctuated with summit inflation and deflation, ranging about 30.5-40.5 m (100-133 ft) below the vent rim. On the East Rift Zone, the 61g lava flow remained active downslope of Pu‘u ‘O‘o, with scattered breakouts on the upper part of the flow field and on Pulama pali, but no ocean entry. The 61g flows do not pose an immediate threat to nearby communities.
Mauna Loa is not erupting. Rates of deformation and seismicity have not changed significantly in the past week, persisting at above-long-term background levels. Sixteen microearthquakes (magnitudes less than 2) were located beneath the summit caldera, upper Southwest Rift Zone and western flank of the volcano at depths of 0-5 km (0-3 mi). GPS and InSAR measurements continue to show slow deformation related to inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone. No significant changes in volcanic gas emissions were measured.
No earthquakes were reported felt in the Hawaiian Islands this past week.
Visit HVO’s website (https://volcanoes.usgs.gov/hvo) for past Volcano Watch articles, Kilauea daily eruption updates, Mauna Loa weekly updates, volcano photos, maps, recent earthquake info, and more. Call for summary updates at 808-967-8862 (Kilauea) or 808-967-8866 (Mauna Loa). Email questions to askHVO@usgs.gov.
Volcano Watch (https://volcanoes.usgs.gov/hvo/hvo_volcano_watch.html) is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.
