Laserfiche WebLink
• Stover noted a rock fall near the northern boundary of the D9 panel. As illustrated in <br />figure 10, this event appear to be localized spalling of rocks from a fluvial sandstone <br />escarpment. Unlike this minor spalling event, regional spalling from the cliff-forming <br />Castlegate Sandstone has been subject to long-term studies by Utah operators and Forest <br />Service resource specialists (Maleki and others 2001). <br /> <br />• <br />Maleki Technologies, Inc. Page 22