... Valley, an ∼2000-m-thick package of Late Cenozoic strata has been uplifted and tilted to the northeast. We name this succession the formation of Pilot Knob Valley and provide new chronologic, stratigraphic, and provenance data for these rocks. The unit is divided into five members that record different...

... present-day rates inferred from geodetic velocity fields are indistinguishable from zero. We evaluate the possibility of non-steady slip over millennial timescales using displaced Late Holocene alluvium along the central Garlock fault in Pilot Knob Valley. Truncation of a Late Holocene alluvial fan...

... (Pilot Knob Valley syncline) and northwest (Teagle Wash syncline) lie at about the same elevations as they did when part of the originally active fan, implying that the synclines are passive results of the anticline development. If so, the original slope of the middle Pleistocene alluvial sediment sheet...

..., in the southwest corner of the Great Basin, the north-northwest–trending Slate Range anticline and Argus–Slate Range syncline appear to be active where bench-mark lines cross them. South of the fault, the east-northeast–trending Dome Mountain anticline and Pilot Knob Valley syncline appear active. Maximum rates...

...Figure 7. Simplified geologic map of the Pilot Knob Valley formation. (A) Detailed geologic map of the Pilot Knob Valley formation (location shown in Fig. 1 ) using data from Dunne and Walker (2004) , Andrew et al. (2014) , and Rittase et al. (2020) overlain on a shaded relief map. This map...