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during the mountain building process, Some of these faults (which are identifiable at the <br />surface), dip are as much as 45 degrees to the east on the Hayden Baldy to 32 degrees to <br />the east on Fleming Mountain. Simply, there is a danger to the structural integrity or our <br />homes every time that they blast. The contact is not consolidated very strongly, and it is <br />sitting on such a steep slope, that it may move with the blasting. "Not consolidated" is <br />the professional term essentially for a pile of dirt and debris. There are faults mapped in <br />the valley below and on the hills above us, (USGS map studies). Our properties are sited <br />near the surface contact of these unconsolidated sediments as well as the fault pattern <br />mapped for the USGS. <br />We never would have agreed to buy the property if Ken Chlo (the Domtar, quarry <br />superintendent, and now Holcim's quarry superintendent) had not assured me that the <br />mine would never re-open. <br />Sincerely, <br />Bet~e`iley <br />Ro ers J. Bail y <br />