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Introduction <br />The following report presents the results of a slope stability analysis for a proposed open <br />cut gravel extraction operations at the Varra Coulson pit operations near Greeley, <br />Colorado. This analysis was performed at the request of Varra Companies, Inc., ( Varra). <br />It is our understanding the Colorado Division of Reclamation and Mine Safety (DRMS) <br />requires this analysis as part of Varra's mine permit submittal. <br />Background Information <br />The proposed Coulson gravel quarry is located in the NE1 /4, S10, TSN, R65W of the 6th <br />Principal Meridian. The surrounding land use consists of agricultural, rural residential, <br />commercial and open -cut gravel quarry operations. The proposed mine area occupies an <br />estimated 62 acres. The water table at the site is located in unconsolidated alluvial <br />deposits associated with the Poudre River with the depth to water between 5 and 10 feet <br />below grade. Soil conditions generally consist of varying thicknesses of top soil underlain <br />by sand and gravel deposits, which in turn are underlain by Pierre Shale. Over the entire <br />area the average saturated thickness of the sand and gravel deposits (prior to mining) is <br />estimated at 45 feet. It is our understanding that the sand and gravel will be dewatered <br />during aggregate extraction. The site location is presented on Figure 1. <br />Previous Investigations <br />In August 2000, 17 soil borings were drilled from ground surface to bedrock to determine <br />the potential aggregate mass within the proposed mine boundary. The depth to bedrock <br />over the site varied between 29 and 65 feet below ground surface. In general the site <br />consists of three to five feet of top soil underlain by 24 to 60 feet of sand and gravel with <br />occasional clay and sand lenses. Geotechnical studies conducted by Terracon 2011, and <br />CTL Thompson, 2006 document soil strength properties at two adjacent mines (Great <br />Western & Durham). The results of these investigations are presented in Attachment A. <br />Conservative soil strength properties presented by DRMS are presented in Attachment B. <br />