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(1) Silty Tovsotl: The majority of the site is overlain <br /> by a one-foot layer of silty topsoil. The topsoil <br /> has been penetrated by plant roots and organic <br /> matter. <br /> (2) Silty Clay and/or Sandy Silt: This stratum under- <br /> lies the topsoil and extends to the gravel layer <br /> below. The majority of this stratum consists of <br /> non-plastic sandy silts. The silty clays make up <br /> a small portion of the overburden. Heavy concen- <br /> trations of sugar lime slurry waste were noted in <br /> the clay stratum in Borings 3 and & The lime was <br /> noted on the surface in the area of Boring No. • <br /> and covered an area approximately two hundred (200) <br /> square feet, The lime does not appear on the <br /> surface in the area of Baring No. 3. No evidence of <br /> concentrations of this lime material was noted in <br /> the upper clays or silts in any of the other test <br /> borings. <br /> (3) Sand. Gravel and Cobbles: The gravel stratum under- <br /> lies the upper clays and silts at depths of one and <br /> one-half (1-1/2) to six and one-half (8-1/2) feet below <br /> the surface and extends to depths of fifteen (15) to <br /> eighteen (18) feet below the surface. The sand and <br /> gravels are clean, and poorly graded Generally, <br /> small cobbles three (3) to six (6) inches in six* <br /> and ranging in size up to eight (8) to ten (10) inches <br /> are distributed throughout the gravel stratum. <br /> Numerous thin lenses of sand were noted in the <br /> granular layer. <br /> (4) Siltstone (Bedrock): The bedrock underlies the <br /> gravel at depths of fifteen (15) to eighteen (18) feet <br /> below the surface and extends to greater depths, <br /> (5) Groundwater: At the tier a of the investigation, free <br /> groundwater was noted at depths' of three and one- <br /> half (3-1/2) to seven (7) feet below the surface. <br /> These water levels are subject to change depending <br /> upon seasonal variations and irrigational demands <br /> on and adjacent to the property. <br /> The test borings indicate that a layer of sand and gravel, ten <br /> (10) to fifteen " one-half (15-1/2) feet thick is overlain by one and <br /> one-half (1-1/2) to six and one-half (6-1/2) feet of overburden. The <br /> majority of the gravel deposits are below existing groundwater levels, <br /> and water levels can be expected to rise one (1) to two (2) feet <br /> during the irrigation season. It is estimated that approximately <br />