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1 <br />pond. The pond would trap sediments carried in the flow(s) until full, at which time flow in Red Wash <br />would likely resume flowing in a relatively narrow active channel. <br />' The conclusions noted above were further confirmed during 1989. On July 29, 1989 a large flow <br />event occurred in Red Wash. The subsidence Vough over LW-2 filled with water. The Vough over <br />LW-1 also filled, but to a lesser depth as it had filled with sediment in the past. Water level <br />measurements were taken in the monitoring holes while they were surrounded by standing water. <br />' Readings had been taken only 18 days before. Even though fhe holes were surrounded by standing <br />water (approximately 3 and 4 feet deep at RW-7 and RW-9 respectively) the alluvial water depths <br />had still decreased. <br />Again this year, very little change in the water levels was recorded. <br /> <br />1 <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />17 <br /> <br />