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i;::x;:x:::::;:x:x:x:::;::x:::::;:i:::::::;:::x::;x <br />»iirt:-x::??x:::x;x'x::wmm <br />'vx:v:v:x:: <br />V::x-x:x::k::;:x:x:x • • • « • <br />V \ <br />my^. <br />17, ' <br />'V <br />%■■ <br />i-/ ^ <br />-L :. ^ <br />ttlmmm <br />•t't <br />'mS; <br />'iSSiSS <br />' <br />•Is are visible near Highway 12 just northloams. Exposures of these soxls are vxsx <br />of the proposed landfill sxte. gravels <br />The presence of datively free seepage path for land- <br />beneath the £1U couH provtde^a^ ^ <br />nil leachatea away Item la <br />o£ such extremely permea y ^^e <br />as follows. Topographic maps s ow <br />gislnger property is a P-;;-;- -:;reing up to 33 feet in depth <br />southward about H P „,<tion of the morainic soils, <br />indicate that l^ediately fol^rng^ ep <br />the lake bottom was .trough a ridge which serves <br />let for the large mars o control takes the form <br />as the water level ""i^h has degraded to its present <br />of an eroded channel g „„at been <br />level of approximately 965^ ^ or <br />below 965 during postg ac . streams should be <br />swamp. Therefore no granular ep draining seepage <br />ptesent beneath the site and the potentral for <br />paths is remote. <br />». ..-nu ... ■- *• ■•Tbe drainage areas affect <br />Area A is the A and B comprise the take Classen <br />south limits of the Ian ^ ^ ^^.,„cary to take <br />Creek drainage area. Areas fl, <br />Minnetonka's Stubbs Bay. including the construction <br />Filling of marsh areas for P <br />1 Afn\ will have an effect on tne <br />ofa demolition la pcocesses are changed: <br />surface water runo . rainfall <br />1. the filled area thus <br />will infiltrate into the sol ^ <br />reducing the total volume of runo snowmelt <br />(Mote: this will not necessari y <br />nr if the filled area is paved). <br />rain will fall on water areas and will go <br />- 4 • <br />i.••.A <br />P