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City of Ramsey <br /> Project B1700969 <br /> March XX,2017 <br /> Page 3 <br /> DRAFT <br /> 13.3. Published Geologic Information <br /> B.3.a. Topography <br /> According to the United States Geological Survey(U.S.G.S)7.5-minute topographic map series, <br /> Anoka, Minnesota quadrangle,the Site is located at an elevation of approximately 865 feet above mean <br /> sea level.The topography of the Site is relatively level with a slight downward slope to the south. <br /> 13.3.1b. Geology <br /> The unconsolidated sediments in the Site vicinity are Quaternary Wisconsin Episode Langdon Terrace <br /> deposits,which consist of sand and gravelly sand (Meyer,2012). <br /> The uppermost bedrock unit in the Site vicinity is the Upper Cambrian St. Lawrence Formation (Mossler, <br /> 2012).The St. Lawrence Formation is described as light gray to yellowish-gray and pale yellowish-green, <br /> dolomitic,feldspathic siltstone with interbedded very fine-grained sandstone and shale. <br /> The depth to bedrock in the Site vicinity is approximately 150 feet to 200 feet below land surface <br /> (Mossler,2012). <br /> B.3.c. Hydrogeology <br /> Based on the findings of this Phase II ESA,groundwater is present under the Site at depths of <br /> approximately 20 to 28 feet below land surface. <br /> According to published geologic information,the regional groundwater flow direction within the <br /> unconsolidated deposits in the Site vicinity is generally south-southwest,towards the Mississippi River <br /> (Palen et al., 1993).The Site-specific groundwater flow direction was not determined through direct <br /> measurement during this Phase II ESA. <br /> C. Scope of Services <br /> The following tasks were conducted at the Site as part of this Phase II ESA: <br /> ■ Cleared public utilities through Gopher State One Call and private utilities through a private <br /> contractor for the investigation locations. <br /> ■ Advanced 9 environmental soil borings(S-1 through S-9)and collected soil samples. <br /> BRAUN <br /> INTERTEC <br />