During May of 1984, two snaIl debris flows occurred in Johnson's HollCM of Emigration Canyon (Figure 1 - Location Map, and Figure 2 - Vicinity Map). These flows passed through Standel Cove subdivision and into Emigration Canyon stream without any significant danage to the homes or drainage structures. Shortly after these events, an investigation revealed three large landslides located in JOhnson's Hollow approximately 3/4 mile above the Standel Cove subdivision. The landslides have the potential of becoming large debris flCMs in the event precipitation produces sufficient saturation in the unstable masses. Because of potential risk from the landslides, residents of Standel Cove SUbdivision have claimed that their property has been devalued and have requested a reduction in county property taxes. In order to provide da ta to evaluate these claims, 'Ule Utah Geological and Mineral Survey was requested to assess the potential danage to the homes and property in Standel Cove subdivision. The assessment was specifically limited to potential danage to real property and therefore excludes risk to personal property and life.