Science, Hazards and Planning in Subduction Zone Regions II
Date: 4/25/2019
Time: 8:30 AM to 12:00 PM
Room: Cascade II
Subduction zones host the Earth’s largest faults and many of its active volcanoes. Subduction systems also play a central role in the formation and accretion of continental crust and are responsible for recycling oceanic crust and volatiles into the mantle. This session explores the latest multidisciplinary scientific advances in subduction zones around the world, including their mechanics, structure, evolution and dynamics from the trench to the backarc. We welcome studies that explore such topics as seismicity, tremor and deformation transients, including the slip behavior of faults and tsunami genesis, as well as studies that explore the geologic signatures of these processes. Below the arc, studies may explore volatile and magma migration, mantle wedge dynamics and melt production in the lower crust.
The dynamic processes inherent to subduction zones also challenge society’s prosperity given the potential for natural disasters with broad regional impacts. These natural disasters are often compound events, as in the case where large earthquakes can trigger both landslides and tsunamis. The successful mitigation of these natural hazards requires a thorough scientific understanding of the underlying processes. Therefore, we also welcome studies that explore the recurrence, probability, potential impacts and mitigation strategies of these natural hazards.
Conveners
David Schmidt, University of Washington (dasc@uw.edu)
Lori Dengler, Humboldt State University (lori.dengler@humboldt.edu)
Will Levandowski, TetraTech (will.levandowski@tetratech.com)
Kathy Davenport, Oregon State University (davenpka@oregonstate.edu)
Jamey Turner, TetraTech (jamey.turner@tetratech.com)
Rick Wilson, California Geological Survey (rick.wilson@conservation.ca.gov)
Brendan W. Crowell, University of Washington (crowellb@uw.edu)
Oral Presentations
Participant Role | Details | Start Time | Minutes | Action |
---|---|---|---|---|
Submission | Sediments From Lower Squaw Lake, OR, Contain Evidence of the 1700 AD Cascadia and 1873 AD Intraplate Earthquakes and Suggest a New Method for the Precise Dating of Earthquake Deposits | 08:30 AM | 15 | View |
Submission | Calibrating Cascadia Paleoearthquake Magnitudes and Ground Motions From the Paleoseismic Record | 08:45 AM | 15 | View |
Submission | Complicated Kinematics in the Southern Cascadia Subduction Zone | 09:00 AM | 15 | View |
Submission | Repeating Earthquakes in the Cascadia Subduction Zone and Their Ties to Seismogenic Zone Heterogeneities | 09:15 AM | 15 | View |
Submission | What Is the Potential for Large Deep Intraslab Earthquakes Beneath Northern California | 09:30 AM | 15 | View |
Other Time | Posters and Break | 09:45 AM | 60 | |
Submission | Probabilistic Tsunami Hazard Maps for Application Through the California Seismic Hazard Mapping Act | 10:45 AM | 15 | View |
Submission | Efficient Methods for Site-Specific Probabilistic Tsunami Hazard Analysis | 11:00 AM | 15 | View |
Submission | Building a Geologic Record of Earthquakes and Tsunamis of the Guerrero Seismic Gap, Mexican Subduction | 11:15 AM | 15 | View |
Submission | Ground Motions From Tsunami Earthquakes: An Example From Indonesia and Implications for Hazard and Warning | 11:30 AM | 15 | View |
Total: | 195 Minute(s) |
Science, Hazards and Planning in Subduction Zone Regions II
Description