Comments |
The assigned slip rate was calculated by dePolo (1998) based on field data from Yount (1997, written comm., as reported in dePolo, 1998). The slip rate is derived from offset across a 3.2-m-high scarp (presumably a multiple-event scarp) on a latest Pleistocene (15 to 30 ka) fluvial terrace along the fault west of Lone Mountain. DePolo (1998) and dePolo and Anderson (2000) calculated a preferred vertical slip rate of 0.13 mm/yr (using a preferred vertical offset of 2.9 m from Yount's original data) and preferred age of the deposit of 22.5 k.y. |