Volcano Watch: The past is the key to the future at Kilauea

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For 15 years, we’ve been on a journey of discovery through Kilauea’s volcanic past. Today, we review what’s been learned on that journey and how new findings are shaping our thoughts about the future at Kilauea.

For 15 years, we’ve been on a journey of discovery through Kilauea’s volcanic past. Today, we review what’s been learned on that journey and how new findings are shaping our thoughts about the future at Kilauea.

Geologists from the Smithsonian, the University of Hawaii and Hawaiian Volcano Observatory began their journey in the late 20th century, when it was thought Kilauea was almost always effusive (erupting lava flows) and the opposite kind of eruption, violently explosive, was anomalous and rare. Now, 15 years into the 21st century, we know explosive eruptions are far more common than previously thought and the kind of eruptive activity, whether explosive or effusive, alternates during periods of centuries.

How did this startling change in thinking take place, and why is it important?

Boots on the ground was the method, coupled with the ability to measure the age (to the nearest few decades) of tiny bits of charcoal found in volcanic deposits. Thousands of field observations of explosive deposits discovered more than 100 sites with charcoal resulting from fires started by eruption. Field work pieced together the sequence in which deposits were laid — younger deposits overlie older like papers on a cluttered desk — and determined how far they were dispersed away from the summit of Kilauea. More sophisticated analysis indicates some volcanic ash reached upward well into the jet stream, a hazard to air travel were it to happen again.

As our journey progressed, we dated charcoal in the deposits using advanced carbon-14 techniques. The ages confirmed field interpretations that the explosive deposits spanned a considerable time and were not products of rare, solitary eruptions. The most recent explosive period lasted from about 1500-1800 CE, and an earlier period from about 200 BCE-1000 CE. Still-older explosive deposits await more study.

We then assembled all previously determined carbon-14 ages for Kilauea lava flows on the volcano and found something remarkable. Most lava flows were erupted between explosive periods, not during them.

Wow! Suddenly it dawned on us that Kilauea erupts in cycles. Periods dominated by explosive eruptions alternate with periods dominated by effusive eruptions. Kilauea mostly has erupted lava flows for the past 200 years, and we were misled into thinking the volcano was always like that. Now, we know better.

We then calculated that the volumes of lava flows surpass the volumes of explosive deposits by nearly 100 times. This was another wow! Apparently, the rate at which magma is supplied to the volcano from deep within the earth is almost 100 times faster during effusive periods than during explosive periods. Why this happens is not yet obvious.

The physical characteristics of the explosive deposits indicate most eruptions were powered by steam from heated groundwater. This happens when the summit caldera is deep and intersects the water table, which today is about 615 meters (2,000 feet) below the rim of the caldera.

Putting all this together, we get a picture of explosive eruptions during periods of low magma supply and a deep caldera, and of effusive eruptions during periods of high magma supply and a shallow or filled caldera, such as today.

The future probably will resemble the past. Eventually, the magma supply rate will drop drastically from its currently high level. The caldera will collapse because there is insufficient magma to fill the reservoirs supporting the summit, and explosive eruptions will resume. That would create a hazardous situation at the summit that could last for centuries, until the magma supply rate picks up and effusive eruptions again take command.

What an exhilarating journey of discovery … and it continues.

Kilauea activity update

Kilauea’s summit lava lake level fluctuated this past week between about 48 and 51 m (157–167 ft) below the vent rim.

The June 27 lava flow continues to feed widespread breakouts northeast of Pu‘u ‘O‘o. All active lava remains within about 8 km (5 mi) of Pu‘u ‘O‘o.

One earthquake was reported felt on the Big Island in the past week. At 12:38 a.m. Aug. 3, a magnitude-2.9 earthquake occurred 19.6 km (12.2 mi) northwest of Kawaihae at a depth of 17.5 km (10.9 mi).

Visit the HVO website (http://hvo.wr.usgs.gov) for past Volcano Watch articles, Kilauea daily eruption updates and other volcano status reports, current volcano photos, recent earthquakes, and more; call (808) 967-8862 for a Kilauea summary update; email questions to askHVO@usgs.gov.

Volcano Watch (http://hvo.wr.usgs.gov/volcanowatch/) is a weekly article and activity update written by scientists at the U.S. Geological Survey`s Hawaiian Volcano Observatory.