New Zealand research could help track the path of searingly hot rock and gas flows that are the world’s most deadly volcanic hazard.
Te Whare Wānanga o Waitaha | University of Canterbury School of Mathematics and Statistics Lecturer Dr. Leighton Watson has for the first time shown that seismic signals—ground shaking recorded by seismometers—can be used to track pyroclastic flows, which can travel at up to 500 kmh (310 mph) during a volcanic eruption.
The catastrophic eruption at Whakaari White Island in 2019 caused a pyroclastic surge of gas and rock that killed 22 people, while an earlier eruption of Te Maari craters in 2012 on Mt. Tongariro also caused pyroclastic flows, resulting in the closure of the Tongariro Alpine Crossing. Around the world more than half of all volcano-related deaths are caused by pyroclastic flows.
Dr. Watson says these “terrifying” flows are challenging to study because they are sudden, fast-moving, and dangerous. “It’s hard to know what is going on inside a flow because the internal flow dynamics are hidden by an opaque gas cloud which is impossible to see through.”
However, he has used seismic data recorded by a permanent monitoring network at Mt. Etna, Italy, to track a pyroclastic flow that happened in February 2014. His findings have been published in the Journal of Geophysical Research: Solid Earth.
“We’ve shown that as the pyroclastic flow travels down the flanks of the volcano, it pushes on to Earth’s surface producing seismic waves. We can use these seismic signals to track the flow, potentially informing modeling of their flow paths in real time which could help with making hazard assessments for future eruptions.
“By considering how seismic signals get smaller further away from the pyroclastic flow, we can locate the source of these vibrations and track their location over time.”
He says because of the extreme hazard posed by pyroclastic flows there is an urgent need to improve monitoring capabilities. The findings could be applied at volcanoes in New Zealand such as Ruapehu, Tongariro and Taranaki.
“All of the New Zealand volcanoes are able to produce pyroclastic flows, so being able to monitor them better could help improve safety.”
Dr. Watson hopes to carry out further research in the New Zealand context using seismic signals to track lahars (mudflows composed of rock, debris, and water), as well as pyroclastic flows. A lahar from Ruapehu destroyed a bridge over the Whangaehu River causing a train derailment in the 1953 Tangiwai disaster that killed 151 people.
“The ultimate goal is to better understand and monitor volcanic hazards and to use these findings to save lives. This is especially useful as volcanoes are often shrouded in cloud and eruptions can happen during the night when cameras are not effective.”
Dr. Watson has already shown that sound waves can be used to detect mountain avalanches along the Milford Road and is currently working on monitoring avalanche activity in Mount Cook Aoraki National Park.
Leighton M. Watson et al, Tracking a Pyroclastic Density Current With Seismic Signals at Mt. Etna (Italy), Journal of Geophysical Research: Solid Earth (2023). DOI: 10.1029/2022JB026114
University of Canterbury
New tool could help track deadly path of searingly hot rock and gas flows during eruptions (2023, May 16)