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The conclusions noted above were further confirmed during 1989. On July 29, 1989 a large <br />flow event occurred in Red Wash. The subsidence trough over LW-2 filled v~ith water. The <br />trough over LW-1 also filled, but to a lesser depth as it had filled vrith sediment in the past. <br />Water level measurements were taken in the monitoring holes while standing water surrounded <br />them. Readings had been taken only 18 days before. Even though the holes were surrounded <br />by standing water (appro~dmately 3 and 4 feet deep at RW-7 and RW-9 respectively) the alluvial <br />' water depths had still decreased. <br />' Although the purpose of the monitoring program was met, BME continued to monitor the Red <br />Wash alluvial holes until water year 1996-1997. The latest monitoring results are reported in <br />Appendix F and hydrographs for each monitoring hole are presented in Appendix G of the <br />' Thirteenth Annual Hydrology Report. <br />iz <br />