By Frank R. Ettensohn, Nicholas Rast, Carlton Elliot Brett

ISBN-10: 0813723590

ISBN-13: 9780813723594

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9), which overstepped both L4 and sand ejected along the main fault, accumulated as a colluvial wedge adjacent to the secondary fault. The next younger loess deposit (L2, see Fig. 4, Fig. 9) accumulated as a colluvial wedge adjacent to the main fault and overstepped L3 and L4 between the main and secondary faults. The youngest loess deposit (L1, see Fig. 4, Fig. 9) accumulated as colluvial wedges adjacent to both the main and secondary faults. Additionally, the retro-deformation of the faults and strata in the trench log, combined with analysis of structural data from the trench and historic seismicity, allowed us to determine which stress field caused each of the six events.

Y. y. Reverse faulting perhaps reflects accommodation associated with major events on the nearby Centennial fault during northsouth extension associated with the Yellowstone hotspot. y. and a recurrence interval of more than 20 ka. ACKNOWLEDGMENTS Renee A. Greenwell and Elzbieta Covington provided hardware and software support. This study was partially supported by a Montana Tech Research Center grant to Bartholomew and Stickney. We thank Diane I. Doser, James W. Sears, and Edmond G. Deal for reviews that helped us to improve the paper.

2 and 3). A landslide that filled the incised channel of the Red Rock River near the modern dam (Fig. 2) probably created this ephemeral lake of latest Pleistocene age. Numerous landslides are found in this area (Fig. 2). Analogous examples include the landslide, which impounded Quake Lake in the incised gorge along the Madison River (Fig. 1B), associated with the 1959 Hebgen Lake earthquake Late Quaternary paleoseismites Figure 1. Index map of southwestern Montana showing study area (heavy-line box in A outlines area of Fig.

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Ancient Seismites (GSA Special Paper 359) by Frank R. Ettensohn, Nicholas Rast, Carlton Elliot Brett

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