Megathrusts are found in areas where one tectonic plate dives beneath another, in this case the Pacific plate being pushed under the North American plate. This area is known for generating powerful tremors. In fact, the Queen Charlotte fault system represents the greatest seismic hazard in Canada, producing the country’s largest recorded earthquake in 1949 and a notable earthquake in 2012 that created a tsunami.
“This region is actively becoming a subduction zone, so understanding the fault structure here tells us about the early stages of subduction zone development,” says lead author Collin Brandl, a postdoctoral research scientist at the Lamont-Doherty Earth Observatory, part of the Columbia Climate School. “Our study provides the first direct observations of the Haida Gwaii thrust, the “megathrust” of this system, which can help improve hazard analysis in the region, better preparing residents for future earthquakes and tsunamis.”
Brandl’s co-authors are part of an international team, with scientists from the University of New Mexico, Western Washington University, the U.S. Naval Research Laboratory, Boise State University, Nova Scotia’s Dalhousie University, the University of British Columbia, the University of Victoria, the Geological Survey of Canada, and the Universidad de Chile.
Press interviews with Collin Brandl can be arranged by emailing [email protected].