T022
The Cascadia Megathrust and Beyond: From Fundamental Scientific Processes to Societal Resilience
The Cascadia Megathrust and Beyond: From Fundamental Scientific Processes to Societal Resilience
Session ID#: 252292
Session Description:
The Cascadia Subduction Zone has the potential to rupture in great (M>8) megathrust earthquakes, but with the near absence of interseismic interplate seismicity, the Cascadia megathrust earthquake cycle must be examined through a range of observational tools and modeling approaches. Developing an understanding of the many processes, associated hazards, and cascading consequences of this unique system requires the integration of different disciplines at a variety of spatial and temporal scales, including both novel observations and models. Greater fundamental knowledge of Cascadia geohazards and their impacts on communities are critical for future hazard mitigation, adaptation, and resiliency efforts. In this session, we welcome contributions from all areas of Cascadia and comparative subduction zone science. Topics may include, but are not limited to: earthquake seismology, geophysical imaging, geodesy, rock mechanics, paleoseismology, structural geology, petrology and geochemistry, cascading hazards, novel offshore instrumentation, community engagement, and geoscience education.
Co-Sponsor(s):
- S - Seismology
Index Terms:
7230 Seismicity and tectonics [SEISMOLOGY]
7240 Subduction zones [SEISMOLOGY]
8150 Plate boundary: general [TECTONOPHYSICS]
8170 Subduction zone processes [TECTONOPHYSICS]
Primary Convener: Brian Boston, Auburn University, Auburn, United States
Conveners: Audrey Dunham, U.S Geological Survey, Seattle, United States, Harold J Tobin, University of Washington Seattle, Earth and Space Sciences, Seattle, WA, United States and Jianhua Gong, Indiana University Bloomington, Bloomington, IN, United States
Student/Early Career Convener: Zoe Krauss, University of Washington, Department of Earth and Space Sciences, Seattle, United States
See more of: Tectonophysics