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<br />C:IWINDOWSITEMPIBreach IJPG (local) <br /> <br />Page I of I <br /> <br /> <br />Breach': Looking upstream through the breach, A remnant of the slide can be seen on the left <br />The head scarp is visible at the crest This scarp was measured to be about 13 feet vertical in <br />height The remnant of the slide extends for about 150' from the breach, The rock at the right is <br />bedrock, a weakly cemented, course sandstone (Le, crumbles easily), The scarp in center of <br />photo is the remnant of an over-consolidated clay, suspected to be native overlying the <br />sandstone, Note the steep dip of the bedrock formation, A near vertical joint in the sandstone <br />can be traced form the bottom center of the photo up to the clay remnant (Gray colored line) The <br />joint was filled with a course, sandy clay, but no iron staining, <br /> <br />f <br /> <br />file:C:1 WINDOWSITEMPIBreach IJPG <br /> <br />5/5/98 <br />