08/05/2022
The ongoing eruption at the summit of Kīlauea hasn’t made the news recently, but that doesn’t mean the recent eruptive activity hasn’t been noteworthy.
The first thing to appreciate is that we are witnessing a pattern that has typified Kīlauea’s summit behavior for centuries—the cycle of collapse and refilling. The caldera floor collapses and/or subsides—often due to an eruption on the rift zone—and subsequent summit eruptions fill the depression with new lava. Destruction and reconstruction, set on repeat.
Numerous cycles of collapse and refilling occurred during the 1800s and early 1900s. These ranged from large to small, some spanning much of the caldera floor, with others limited to just the Halemaʻumaʻu area. In each instance, lava eventually returned to the summit and filled much or all of the depression.
The collapse of the crater floor in 2018 was one of the largest such events in the past 200 years. Over the past year and a half, lava has been erupting in Halemaʻumaʻu crater and slowly refilling the new depression. Since returning to Halemaʻumaʻu in December 2020, lava has refilled about 17% of the volume of the 2018 collapse.
The second thing that is interesting about the current activity is the manner in which the lava is refilling the crater. In the simplest scenario, we might imagine the lava in Halemaʻumaʻu simply pouring in over earlier flows, stacking up and filling the crater.
While a portion of the refilling is being done in this manner, a major amount of the refilling is “endogenous.” In other words, lava from the vent is supplied beneath the solidified surface crust, out of view, lifting the crater floor. It’s akin to inflating a giant air mattress.
We can track this growth with unprecedented detail using modern tools. A continuous laser rangefinder measures the lava surface every second, with centimeter precision. Webcams operating on the rim of Halemaʻumaʻu show the nature of uplift clearly.
The process of endogenous growth is particularly well illustrated with the we**am on the east rim of Halemaʻumaʻu (the B1cam). Timelapse images from this we**am show the central portion of the crater floor is being lifted like a piston, intact and largely without fracturing.
The active lava lake—forming a relatively small portion of the crater floor—has essentially been lifted up gradually with the remainder of the crater floor.
At the same time, this zone along the margins of the crater floor is often resurfaced due to ooze-outs—basically lava that is squeezed out from beneath the crater floor, onto the surface.
This type of endogenous growth, or “bodily uplift,” was also observed in the 1800s and early 1900s. But it hasn’t been observed so much in the past hundred years on Kīlauea. And it certainly hasn’t been observed this clearly before, given our modern tools such as laser rangefinders and we**ams.
You can bear witness to this important phase in the lifecycle of Kīlauea, and a fascinating period in Hawaiian volcanism. Volcano watchers on the Island of Hawaiʻi can see the summit lava lake filling Halemaʻumaʻu crater by visiting the public viewing areas in Hawaiʻi Volcanoes National Park.
Visit go.nps.gov/new-eruption for viewing tips and how to prepare for your visit and a link to the USGS we**ams.
(This post is excerpted from Volcano Watch, a weekly activity update article written by USGS Volcanoes scientists and affiliates.)
USGS Photo/M.Patrick
