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staind epiphany mediafire staind instrumental staind chapter v mediafire staind 2011 flac staind album staind 2011 deluxe Rhyolite and dacite pyroclastic rocks and lava flows erupted near what is now the southeastern corner of Death Valley during the Miocene epoch (7-8 ma) (Wright, et al. 1991). The rocks are partly devitrified and have been faulted during the formation of the Basin and Range Province. The local region contains two sets of faults; one set trending approximately NS and the second trending approximately EW. In analogy with Basin and Range fault patterns, the faults are assumed to be normal faults. The outcrop distribution, although excellent, is not sufficient to determine whether one set of faults offsets the other. Consequently, the slip vector for the faults must approximate the line of intersection of the faults and plunge relatively steeply. |
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