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<D- <br />All soil samples obtained were brought to our laboratory <br />for examination and classification. They will be retained for a <br />period of at least 90 days from date of issue of this report, after <br />which they will be discarded unless we are otherwise notified. <br />Drawing No.l is a site plan showing the soil test hole loca­ <br />tions in relation to the outline of the proposed building. Detailec <br />soil descriptions together with a plot of the standard penetration <br />test blows per foot are given on the Borehole Log, Drawing No.2. <br />Following the regular written soil descriptions are capital letters <br />in parentheses, which represent the appropriate group symbols of th« <br />Unified Soil Classification System. A chart explaining this system <br />is appended. <br />All elevations in this report are to geodetic datum, and were <br />obtained using the bench mark noted on the site plan. These eleva­ <br />tions are approximate only. <br />SITE AND GEOLOGY <br />The site is located on a small peninsula extending into the <br />North Arm of Lake Minnetonka, and is a lake shore lot. The propose <br />building area is flat, and is only slightly higher than lake water <br />level. This was formerly a swamp area, but was filled over to raisu <br />it above lake level. <br />An existing old wood cabin on this property, to be demolishe <br />has sagged and settled. <br />The underlying soils in this area, in order of their age fron <br />youngest to oldest, are post-glacial organic swamp deposits, clayey <br />and sandy, water modified glacial till related to the Des Moines <br />ice lobe of the Wisconsin glaciation, and glacial outwash sand. <br />According to information published by the State of Minnesota <br />Geological Survey, the uppermost bedrock stratum under this area is <br />believed to be Jordan sandstone or St. Lawrence dolomite, and <br />probably occurs at considerable depth below ground surface. <br />SUBTERRANEAN <br />ENGINEERING CORP. <br />MINNEAPOLIS. MINNESOTA