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-5- <br />thousands of years ago. The unweathered glacial till consisted of very dense, <br />silty fine to coarse sand with some fine to medium gravel. <br />Wet soil conditions were noted in boring B-1 from 5.1 to 5.8 feet within a <br />more sandy layer. Since there were no wet conditions noted in boring B-2, we <br />believe that the observed wet conditions represent a perched groundwater <br />condition. <br />DISCUSSION AND RECOMMENDATIONS <br />Site Preparation <br />The on -site soils contain a significant percentage of silt which make them <br />particularly sensitive to moisture with regard to trafficability and fill <br />placement. These soils may degrade to a slurry -like consistency when sub- <br />jected to construction traffic or are otherwise disturbed in wet conditions. <br />The moisture content determinations from the boring samples indicate that the <br />soils are most probably near or slightly above their optimum moisture content. <br />Therefore, any grading which includes utilization of the on -site soil for <br />foundation backfill should be accomplished in dry weather so that these soils <br />can be dried slightly or maintained at their present moisture content during <br />placement and compaction. <br />If on -site excavated soils cannot be used during a period of dry weather, it <br />will be necessary to import a clean granular material for backfilling <br />foundations. Imported granular backfill should be free of organic and <br />deleterious materials, and should satisfy the following gradation require- <br />ments: <br />Converse Consultants NW <br />