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Fault Name | State |
---|---|
Likely | California |
GEOMETRY | |
Dip (degrees) | 90 |
Dip direction | V |
Sense of slip | strike slip |
Rupture top (km) | 0 |
Rupture bottom (km) | 11 |
Rake (degrees) | 180 |
Length (km) | 64 |
MODEL VALUES | ||
---|---|---|
Slip Rate | 0.3 | |
Probability of activity | 1 | |
ELLSWORTH | HANKS | |
Minimum magnitude | 6.5 | 6.5 |
Maximum magnitude | 7.00 | 6.90 |
b-value | 0.8 | 0.8 |
Fault Model | Deformation Model |
Char Rate1 | GR-a-value1 | Weight |
---|---|---|---|---|
Stitched | 2.1 | 1.61e-04 / 2.27e-04 | 1.271 / 1.407 | 0.50 |
UnStitched | 2.1 | 1.61e-04 / 2.27e-04 | 1.271 / 1.407 | 0.50 |
Stitched | 2.4 | 1.61e-04 / 2.27e-04 | 1.271 / 1.407 | 0.50 |
UnStitched | 2.4 | 1.61e-04 / 2.27e-04 | 1.271 / 1.407 | 0.50 |
1 1st Value is based on Ellsworth relation and 2nd value is based on Hanks and Bakun relation |
Comments |
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Unconstrained slip rate based on assumption by authors that up to 5 m of dextral offset of latest Pleistocene shorelines at northern Madeline Plains (Bryant, 1991) may go unobserved and also overall geomorphic expression of fault zone. |