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Structure and properties of the Cascadia plate interface: evidence from an exhumed paleomegathrust in the Olympic Subduction Complex

Structure and properties of the Cascadia plate interface: evidence from an exhumed paleomegathrust in the Olympic Subduction Complex is a funding opportunity from NSF, closing July 31, 2028.

Funder
NSF
Funding
Grant / contract
Deadline
Jul 31, 2028
(732d left)

Overview

Subduction zone faults produce the largest earthquakes on the planet and most of the devastating tsunamis. This project will study the Cascadia subduction zone, located off the Pacific Northwest coast, which represents a major earthquake and tsunami hazard to the USA and Canada. Researchers will study rocks from the…

Structure and properties of the Cascadia plate interface: evidence from an exhumed paleomegathrust in the Olympic Subduction Complex | Go Fund It Now