1972
DOI: 10.3133/ofr72240
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Geologic map of the Rapid City NW Quadrangle, Meade and Pennington counties, South Dakota

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“…Subsurface lithology can affect the movement of contaminants in groundwater in the study area. The geology around EAFB consists of about 260 m (860 ft) of Cretaceousage Pierre Shale (bedrock) overlain by surficial deposits that are predominately alluvium (McGregor and Cattermole, 1973;Rahn and Glick, 2000). The alluvium consists of sand, silt, clay, and gravel that range in depth from about 3 to 12 m (10 to 40 ft; Tetra Tech Incorporated, 2008).…”
Section: Methodsmentioning
confidence: 99%
“…Subsurface lithology can affect the movement of contaminants in groundwater in the study area. The geology around EAFB consists of about 260 m (860 ft) of Cretaceousage Pierre Shale (bedrock) overlain by surficial deposits that are predominately alluvium (McGregor and Cattermole, 1973;Rahn and Glick, 2000). The alluvium consists of sand, silt, clay, and gravel that range in depth from about 3 to 12 m (10 to 40 ft; Tetra Tech Incorporated, 2008).…”
Section: Methodsmentioning
confidence: 99%