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<br />10 <br /> <br />.- <br />BCJ'r'LE.'f <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Chapter III . Background Information <br /> <br />the beached area. Some erosion gullies, about I to 2 feet deep, were observed on the slope near <br /> <br />the dam crest. The entire slope above the beached area was overgrown with vegetation, which <br /> <br /> <br />consists of thick brush, shrubs, and small to large pine trees. Our observations are consistent <br /> <br />with that reported in the 1997 SEa inspection report. Based on these observations, the <br /> <br /> <br />conditions of the upstream slope are considered to be poor. <br /> <br />The dam crest is uneven with numerous depressions and surface erosion gullies. No <br /> <br /> <br />surface protection materials such as gravels were observed. Over six deep erosion gullies, about <br /> <br />I to 2 feet deep, were observed on both downstream edge and upstream edge of the crest. As a <br /> <br /> <br />result of the erosion gullies, the crest widths vary significantly along the length of the crest. <br /> <br /> <br />Numerous medium to large pine trees are presently growing along the entire length of the dam <br /> <br /> <br />crest near both downstream and upstream edges of the crest. Our observations are consistent <br /> <br />with that reported in the 1997 SEa inspection report. Based on these observations, the <br /> <br />conditions of the dam crest are considered to be poor. <br /> <br />The downstream slope is uneven with numerous surface erosion gullies about I to 2 feet <br /> <br /> <br />deep. These gullies start from the top of the slo]Je and run along the entire length to the toe. The <br /> <br /> <br />entire slope is essentially overgrown with medium to very large pine trees and cottonwoods. <br /> <br />Some of the largest trees, with estimated diameters of 4 to 6 feet, had been cut down, but huge <br /> <br /> <br />stumps were still left on the dam. No evidence of slope instability of seepage, however, was <br /> <br /> <br />observed on the downstream slope. Our observqtions are consistent with that reported in the <br /> <br /> <br />1997 SEa inspection report. Based on these ob:,ervations, the conditions of the downstream <br /> <br /> <br />slope are considered to be poor. <br /> <br />The downstream toe and area downstream of the toe of the embankment were clear of <br /> <br /> <br />vegetation and well maintained. A chainlink fence along the entire toe of the embankment <br /> <br /> <br />appears to mark the property boundary. No evidence of any seepage was observed at the toe at <br /> <br />the time of our site inspection. <br /> <br />The spillway is located in the left abutment of the embankment. Bedrock is exposed in <br />the left abutment. The bedrock is thin-bedded weak cemented sandstone that is very soft and <br />friable. The bedrock on both sides of the spillway channel has been eroded significantly, as <br /> <br />Monument Lake Dam Feasibility Study <br />