Slip-rate category unknown; probably 0.2-1.0 mm/yr Comments: Data as presented by Ostenaa and Wood (1990 #318), based on trenching of Stickney and Bartholomew, indicate that slip during the most recent event was about 2.5 m, and the recurrence interval between the past two events was 5-15 k.y., which yields a slip rate that would fall within the assigned slip-rate category. Length End to end (km) 14.8 Cumulative trace (km) 15.2 Average strike (azimuth) 316°R eferences #294 Bartholomew, M.J., 1989, The Red Rock fault and complexly deformed structures in the Tendoy and Four Eyes Canyon thrust sheets-Examples of late Cenozoic and late Mesozoic deformation in