Northern California Earthquake Hazards Workshop - Day 2
- It's swarmy outside: Developing swarm earthquake forecasting methods
- Andrea Llenos
- CC
- Why do swarms happen? A brief review of what we know about swarm physics
- Alicia Hotovec-Ellis
- CC
- Moment tensors, state of stress, finite-source scaling and pseudo fracture network from micro earthquakes at the Geysers, CA
- Doug Dreger
- CC
- Research challenges from the coast to the Delta: Understanding hazard from partially creeping and "secondary" faults
- Steve DeLong
- CC
- Holocene slip rates in the Santa Cruz Mountains reveal temporal and spatial consistency along the Northern San Andreas Fault, CA
- Kim Blisniuk
- CC
- Aseismic Deformation Along the Central San Andreas and Calaveras Faults From Differencing Repeat Airborne LiDAR
- Chelsea Scott
- CC
- Geological slip rate and earthquake potential of the West Napa fault
- Mike Oskin
- CC
- The Northern San Andreas Fault - A Coastal and Marine Perspective
- Sam Johnson
- CC
- The 1906 earthquake on California's North Coast
- Lori Dengler
- CC
- Quantifying rates of interseismic deformation on faults near Humboldt Bay, Southern Cascadia
- Kathryn Materna
- CC
- Where Broken Plates Meet: The MTJ
- Bob McPherson
- CC
Multiple speakers
- Andrea Llenos
- Alicia Hotovec-Ellis
- Doug Dreger
- Steve DeLong
- Kim Blisniuk
- Chelsea Scott
- Mike Oskin
- Sam Johnson
- Lori Dengler
- Kathryn Materna
- Bob McPherson