Âé¶¹´«Ã½

Skip to content
Reading time: < 1 minute
A Hawaiian Volcano Observatory geologist documents the fissure 8 flow southeast of Four Corners (the intersection of Highways 132 and 137). Credit: U.S. Geological Survey.

Volcanologists at the (SOEST) will receive a $119,821 grant from the U.S. National Science Foundation to study the ongoing volcanic activity on Âé¶¹´«Ã½ Island. The project, Rapid: Tracking magmatic and volcanic changes in the May 2018 K¨©lauea Eruption, seeks to inform why the current volcanic activity is occurring and will help to predict future eruption activity.

“Scientific data has been critical to tracking the volcanic activity on Âé¶¹´«Ã½ Island to minimize the threat to Puna families,” Hirono said. “This federal funding is timely and will increase the resources available to study K¨©lauea’s east rift zone and gain insight into future eruptions.”

“We are extremely grateful to the U.S. National Science Foundation, and the (United States Geological Survey) Hawaiian Volcano Observatory for funding and supporting this research into the current eruption at K¨©lauea, using a range of rapid-response tools,” said , principal investigator on the grant and chair of the at SOEST.

The project was funded through the National Science Foundation’s Rapid Research Response program, which is available for research on natural disasters and other unanticipated events.

Rubin, along with three other SOEST volcanologists, , and , will lead the assessment of the location and movement of magma beneath the lower east rift zone of K¨©lauea to provide information on the processes leading up to the fissures and eruption activity. This study will incorporate aerial imagery and samples of lava collected throughout the event by UH Hilo and the USGS Hawaiian Volcano Observatory to inform knowledge on volcanic processes and activities in volcanic rift zones.

Additionally, the project also includes application of very short half-life natural radioactivity to look at volcanic conditions such as magma ascent rate and degassing. These need to be measured in lavas shortly after being erupted or the signal decays away.

“This eruption represents an amazing opportunity to look, really for the first time, at variations of the isotopes with eruption condition in space and time, and would simply not be possible without the sample collections in real time by USGS,” said Rubin. “Very few labs in the world can do this sort of analysis and we are lucky to be able to take advantage of this opportunity.”

Back To Top