A west-east cross section shows that the mainshock is located at the northern end of the Saline Range where it becomes covered under the alluvium of Eureka Valley. The deepest extent of aftershocks makes an angle of 40-50 degrees and when projected to the surface, would outcrop along the western edge of the Last Chance Range. Eight west to east vertical cross sectional views arranged in panels from north to south. Map of Univ. See Figure 8 for hypocenter location.
Solid traces are observations and dashed traces are synthetics.
The focal mechanisms from Figure 5 and 6 are plotted over the seismicity from 1993 to 1998.