Proceedings of the 12th International INQUA meeting on paleoseismology, active tectonic and archaeoseismology

tectonic geomorphology including well-developed triangular facets and over-steepened basal slopes along the range front, as well as a broad zone of several parallel traces that progressively displace various Quaternary alluvial fan deposits (Figs. 2 and 3). Fig. 1: Fault map of central Nevada showing physiographic features and location of study area (black box). 1954, M6.8 Dixie Valley rupture; 1915, M7.6 Pleasant Valley rupture. Faults from U.S. Geological Survey fault and fold database.