| Comments |
| Kelsey and Bockheim (1994) calculated a vertical slip rate of about 0.5 mm/yr across the Whaleshead fault zone since 125 ka, and a left-lateral strike-slip rate of approximately 2.5 mm/yr since roughly 200 ka. The assigned slip rate represents the oblique rate from the published vertical and horizontal slip rates. |
| Selected References |
Kelsey, H.M., and Bockheim, J.G., 1994, Coastal landscape evolution as a function of eustasy and surface uplift rate, Cascadia margin, southern Oregon: Geological Society of America Bulletin, v. 106, p. 840-854.
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