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<br />1 <br />I <br />1 <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />1 <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />1.2.2 Crest <br /> <br />The crest of the dam is roughly 14 feet wide and the service and National <br />Forest access road that runs along its length is well maintained, with only <br />minor irregularities in elevation. <br /> <br />1.2.3 Upstream Face <br /> <br />The upstream face of the dam is generally in good condition. The slope is <br />uniform at 3.5H to lV and sparsely covered with hard, angular riprap derived <br />from Precambri an crystal 1 i ne rock in a quarry wi thi n the reservoi r; The <br />riprap was probably hand placed and is of a small diameter, nominally 12 <br />inches, but considering the size of the reservoir is probably adequate; No <br />si gn of erosion or sl oughi ng of ri prap was observed, although the top fi ve <br />feet of the slope above the normal water surface have been covered wi th sand <br />and grass. <br /> <br />1.2.4 Downstream Face <br /> <br />The downstream face is variable in the maKimum section with alternating <br />steeper and fl atter slopes rangi ng from 3H to 1 V near the top; to 1. 3H to 1 V <br />at the toe. The steep slope at the toe is stabilized by a hand placed loose <br />masonry rock wall about eight feet high. The downstream face is protected <br />from erosion by a thick carpet of grass. <br /> <br />1. 2. 5 Seepage <br /> <br />One of the concerns at Twi n Lakes Dam is uncontroll ed seepage. Seepage <br />measurement weirs have been in place for years and the City inspects the dam <br />on a daily basi s when the reservoi r is in operati on. Although the reservoi r <br />was empty at the time of the i nspecti ons, seepage i nformati on was gathered <br />from inspection reports on file at the State Engineer's Office and from a <br />visit to the dam by MKE personnel when the reservoir was full in 1982. <br />Consi derabl e seepage flow emerges at the toe of the dam renderi ng the area <br />immedi ately downstream a bog as evi denced by the 1 ush growth of grass. A <br /> <br />-43- <br />