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Photograph and sketch of a set of northwest trending near vertical breccia zones associated with an OWL-trend fault (location 21 on Map 3) viewed facing in the direction N50oE. The apparent slope of the breccia zones results from their cutting the outcrop face at less than 90o. A stereo plot of the dominantly sub-horizontal slickensides from this location is given in Figure 18.
Copyright © 1995-1997 Stephen C. Kuehn