By Frank R. Ettensohn, Nicholas Rast, Carlton Elliot Brett
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Additional resources for Ancient Seismites (GSA Special Paper 359)
The wall strata of both dikes are deformed consistent with forceful upward injection of the dikes. Ejected sand was deposited on the former ground surface up to 2 m away from clastic dike 3, indicating forceful ejection. The orientations of these dikes are consistent with nearby historic focal mechanism solutions. The lag-gravel deposit unconformably overlies the vents and ejected sand of clastic dikes 2 and 3. The lag gravel appears conformable within the stream channel deposit where it and the lower part of the channel (C2, see Fig.
9). Such a 42 Mervin J. Bartholomew et al. Figure 8. Lower-hemisphere equal-area stereographic projections and rose diagrams. A: Slip vectors on minor faults associated with normal displacement on main fault. B: Faults with slip vectors associated with reverse and strike-slip displacements along Lima Reservoir fault zone and rose diagram of clastic dikes 2 and 3 (CD2 and CD3 in Fig. 4). C: Rose diagram of three clastic dikes (CD1, main fault, and secondary fault in Fig. 4). D; Taxis directions for recorded earthquakes (Fig.
5 km east of the trench site at a large stream valley (Figs. 2 and 3). Additionally a northwest trending, 5-km-long, linear feature extends across the lacustrine deposits about 1 km southwest of the trench site (Figs. 2 and 3B). This feature may be another fault scarp of the zone or it may be the frontal fold of the landslide that is northwest of the trench site. In the vicinity of the trench site (Fig. 3B) the main scarp trends about N60°W across the exhumed older Pinedale alluvial fan. 5 m (Fig.