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Geotechnical Engineering Report lrerracon <br /> Carr Aggregate Pit ■ Carr, Colorado <br /> April 23, 2020 ■ Terracon Project No. 20195087 GeORepOrt. <br /> PROJECT DESCRIPTION <br /> Our final understanding of the project conditions is as follows: <br /> Item Description <br /> Information Provided The following project information was provided to us in a notice of intent(NOI) <br /> to the State by Kiewit and through conversation with the client. <br /> We understand the project includes an investigation for a new aggregate pit <br /> Project Description in Carr, Colorado. We understand the gravel pit will cover an approximately <br /> 640-acre area; however, the current scope of services includes only 160- <br /> acres. <br /> If project information or assumptions vary from what is described above or if location of proposed <br /> mining changes, we should be contacted as soon as possible to confirm and/or modify our <br /> recommendations accordingly. <br /> GEOTECHNICAL CHARACTERIZATION <br /> Geology <br /> The project area is located within the Colorado Piedmont section of the Great Plains <br /> physiographic province. The Colorado Piedmont, formed during Late Tertiary and Early <br /> Quaternary time (approximately 2,000,000 years ago), is a broad, erosional trench which <br /> separates the Southern Rocky Mountains from the High Plains. Structurally, the site lies along <br /> the western flank of the Denver Basin. During the Late Mesozoic and Early Cenozoic Periods <br /> (approximately 70,000,000 years ago), intense tectonic activity occurred, causing the uplifting of <br /> the Front Range and associated down-warping of the Denver Basin to the east. Relatively flat <br /> uplands and broad valleys characterize the present-day topography of the Colorado Piedmont in <br /> this region. <br /> Surficial geologic conditions mapped in the vicinity of the site ('Hershey and Schneider, 1978), <br /> (2Tweto, 1979), include Quaternary Gravels (Qgo) and Valley Fill terrace deposits (Qvf and Qt) <br /> which has been described as arkosic sand and gravel, which may be locally cemented. Bedrock <br /> units mapped in the vicinity of the site include the Laramie Formation (KI). Bedrock was <br /> encountered in our borings and test pits at depths ranging from about 3'/z to 13'/2 feet below <br /> existing ground surface. The bedrock formations in the area have been reported to include mostly <br /> 'Hershey, L.A., and Schneider, P.A., 1972,Geologic map of the lower Cache La Poudre River basin,north-central <br /> Colorado: U.S. Geological Survey, Miscellaneous Geologic Investigations Map 1-687, scale 1:62,500. <br /> 2 Tweto, Ogden, 1979 Geologic Map of Colorado, United States Geological Survey. <br /> Responsive■ Resourceful ■ Reliable 2 <br />