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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />November 29, 2006 <br />-Project 06-507B <br />2007 Street Reconstruction <br />Deerfield 3rd Addition Improvements <br />Elk River, Minnesota <br /> <br />2. To provide a report of our findings including the results of our subsurface <br />investigation and recommendations regarding earthwork, fill and <br />compaction, utility installation, subgrade preparation, and a design R-value <br />for pavement design. <br /> <br />General Site Conditions: <br />The proposed project site is located in an existing residential neighborhood east of <br />US Highway 169, North of 189th Avenue NW and south of 192nd Lane NW in the <br />City of Elk River. The existing residential streets are bituminous surfaced with no <br />curb and gutter. The site is gently rolling with slopes of 6-12 percent. The streets _ <br />throughout the neighborhood are generally showing their age with distress <br />cracking common. <br /> <br />Available Subsurface Information: <br />According to the Geologic Map of Minnesota, Quaternary Geology, prepared by Howard <br />C. Hobbs and Joseph E. Goebel (1982, Minnesota Geological Survey), this site lies within <br />an end moraine of the Pine City Moraine association. It is associated with the Des <br />Moines Lobe glaciation of Pleistocene, Late Wisconsinan age. The till of this moraine <br />consists of grey, calcareous drift with shale and limestone clasts derived from parent <br />material in Manitoba and eastern North Dakota, but is often mixed with reddish till <br />incorporated from the underlying Superior Lobe. <br /> <br />According to the Soil Survey of Sherburne County prepared by the Soil Conservation <br />Service, this site lies within the Hayden-Braham-Emmert Soil Association. These consist <br />of undulating to steep soils over limy, grey glacial till mixed with red till or gravel or <br />capped with fine sand. Most of the individual soils mapped on this site have slight to <br /> <br />Page 2 <br />