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4.0 RECORDS REVIEW <br />The purpose of the records review was to obtain and review records that may assist in identifying <br />RECs in connection with the Property.Some of the records reviewed pertain to the Property as well <br />as to properties within an additional ASTM specified search distance.These records were reviewed <br />in an effort to evaluate the potential for migrating hazardous substances or petroleum products to <br />impact the Property.Unless otherwise stated, the approximate minimum search distances used were <br />specified in ASTM Standard E 1527-21. <br />4.1 Physical Setting Source(s) <br />4.1.1 Regional Geologic and Hydrogeologic Setting <br />The following information has been summarized from geologic information provided in the <br />University of Minnesota Geological Survey Sherburne County Atlas Series, Surficial Geology, <br />compiled by Barbara Lusardi and Roberta Adams, 2013.Surficial geology at the Property is classified <br />as sand, sandy loam to silt loam. It is described as generally coarse-grained sediment (sand and <br />gravel) in the channels, and finer-grained sediment (fine-grained sand and silt) on floodplains. <br />The following information has been summarized from geologic information provided in the <br />University of Minnesota Geological Survey Sherburne County Atlas Series, Bedrock Geology, <br />compiled by John Mossler and V.W. Chandler, 2013 and the USGS Elk River, MN 7.5 minute <br />topographic quadrangle.Bedrock beneath the Property is categorized as Tunnel City Group, formerly <br />the Franconia Formation, and is divided into two formations: the upper Mazomanie Formation and <br />the lower Lone Rock Formation.The uppermost formation is dominantly white to yellowish-gray, <br />fine to medium grained, cross-stratified, generally friable, quartz sandstone.The Lone Rock <br />Formation is described as pale yellowish-green, very fine to fine-grained, glauconitic, feldspathic <br />sandstone with thin, greenish-gray shale partings. <br />It is presumed that regional groundwater flow is to the west towards the Mississippi River in this area, <br />and is based on the assumption that groundwater flow closely parallels ground surface topography <br />and/or follows natural drainage.This does not take into account any historic cut and fill activity, <br />shallow bedrock or unobserved artificial conditions.The anticipated depth to groundwater, based <br />on the Quaternary Hydrogeology Water-Table System Map in the County Atlas Series <br />for Sherburne County, is 10 - 50 feet below grade. <br />4.1.2 Site Topography <br />Information about the Site topography has been obtained and summarized from the USGS maps and <br />observations made during the site reconnaissance.The approximate elevation of the Property is 894 feet <br />national geodetic vertical datum (NGVD).The topography of the Property itself is fairly level. <br />4.2 Standard Environmental Record Sources <br />At the request of Historical Information Gatherers, Inc., (HIG), Envirosite was contacted to conduct <br />a limited search of accessible State and Federal database files to determine if properties within the <br />vicinity of the Property have had a release or threatened release of a hazardous substance, pollutant <br />Phase I Environmental Site Assessment <br />16330 US Highway 10 NW, Elk River, Minnesota September 4, 2024 <br />Carlson McCain, Inc.Page 6