National Science Foundation (NSF)’s Post

Between 70 and 100 miles off the coasts of southern British Columbia, Washington, Oregon and northern California lies the Cascadia subduction zone: a 600-mile-long strip hosting a “megathrust” fault capable of generating 9.0+ magnitude earthquakes and tsunamis 100 feet high. To bring this hazardous fault into sharper focus, a team of NSF-funded researchers led by Lamont-Doherty Earth Observatory used seismic instruments to “peer” under the seafloor, characterizing the geometry of the overlying sediments of the subducting Juan de Fuca plate, as well as the structure of the overriding North American plate. The team discovered that the megathrust fault is not one continuous structure but rather four segments, each potentially unaffected by movements from the others. This means that movement on one of the segments could be buffered from movement on another. Insights like this can help scientists forecast probabilities of multiple earthquake scenarios, which in turn helps authorities who design building codes and warning systems minimize natural hazard damage and ultimately save lives. To learn more, visit: https://bit.ly/3RWGAwI 📸: Courtesy of the U.S. Geological Survey

  • An illustration of the Cascadia Subduction Zone, located in the U.S. Pacific Northwest and southwestern British Columbia
Eden Ohr

Marketing Assistant at Eagle Point Funding | Helping your tech startup secure US Government grants

1w

This study's revelation that the Cascadia megathrust fault comprises four distinct segments underscores the complex nature of seismic hazards in the region. Such detailed understanding is crucial for refining earthquake preparedness strategies, enhancing building codes, and developing more effective warning systems to mitigate potential damage and save lives.

Like
Reply

To view or add a comment, sign in

Explore topics