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<br /> <br /> <br />Phase I Environmental Site Assessment <br />Old Snelling Avenue & County Road E Improvements <br />WSB Project No. 015447-000 Page 11 <br /> <br />Based on the lack of contamination identified beyond the former fuel oil tank basin, Leak Site <br />LS0012785 is not considered a REC. <br /> <br />5.3 Physical Setting Information <br /> <br />ERIS provided a Physical Setting Report that details topographic, hydrologic, geologic, soil, wells <br />and radon information for the Project Corridor. A copy of the ERIS Physical Setting Report is <br />included as Appendix D. The following information was obtained through review of the report: <br /> <br />· The Project Corridor elevation ranges from approximately 920 feet at the north end to <br />885 feet at the south end. The Project Corridor slopes gradually to the south towards <br />Lakes Johanna and Josephine. <br /> <br />· No wetland features were depicted at the Project Corridor. Multiple wetland features <br />were illustrated adjacent to the Project corridor including freshwater ponds, freshwater <br />emergent wetlands, and freshwater forested/shrub wetlands. Lakes Josephine and <br />Johanna are located between approximately 615 feet and 1,230 feet west and 815 feet <br />southeast of the Project Corridor, respectively. <br /> <br />· Federal Emergency Management Agency (FEMA) flood zone data was available for the <br />Project Corridor. The south end of the Project Corridor, where Old Snelling Avenue <br />crosses over the creek connecting Lakes Johanna and Josephine, is classified as Flood <br />Zone AE-11. Zone AE-11 is considered an area that has a 1% probability of flooding <br />every year. The remainder of the Project Corridor is classified a Zone X-12, an area of <br />minimal flood hazard. <br /> <br />· The underlying bedrock geology at the Project Corridor consists of sandstone and <br />limestone. The bedrock geology is reported as Middle Ordovician rocks, undivided- <br />Decorah Shale; limestone of the Platteville Formation; shaly rocks of the Glenwood <br />Formation; and St. Peter Sandstone in the Hollandale embayment of southeastern <br />Minnesota. Based on information included in adjacent and surrounding well logs, the <br />estimated depth to bedrock is greater than 120 feet below grade. <br /> <br />· The surficial soil at the Project Corridor is primarily reported as urban land-Hayden- <br />Kingsley complex. The Hayden-Kingsley complex consists of fine sandy loam, clay loam, <br />and/or sandy loam. <br /> <br />· No water wells are depicted at the Project Corridor. Multiple domestic water wells are <br />depicted at adjacent sites. Based on information obtained from the well logs included in <br />the Physical Setting Report, the estimated depth of static groundwater level at the Project <br />Corridor ranges from 45 feet below grade at the south end to 95 feet below grade at the <br />north end. Shallow groundwater was encountered at 14 feet below grade at two boring <br />locations advanced during the 2019 Geotechnical Investigation (see Section 2.5). <br /> <br />· Based on information obtained from the Physical Setting Report and the Minnesota <br />Geologic Atlas for Ramsey County, groundwater is anticipated to flow southwest at the <br />Project Corridor. It should be noted that groundwater flow can be subject to localized <br />variation due to factors including geology, topography, soil type, drawdown from local <br />wells, etc. <br /> <br />· The Project Corridor is in Ramsey County which is classified as EPA Radon Zone 1. <br />Counites in Zone 1 have predicted average indoor radon screening values greater than 4 <br />picocuries per liter (pCi/L). <br />