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• ~ • <br />TABLE 11 <br />(Continued) <br />~', Date Established/ <br />' Site Number Location Instrumentation Periods of Ooeration Comments, Etc. <br />S-1 Tributary to -/none associated 1979, 1983 Flow and water quality of spring fed creek ere <br /> Hubberson Gulch 0=B8S 1986-present monitored immediately upstream of unregistered <br /> (SN88W14CBB) stock pond. <br /> 7,425 ft. <br />S-5 Tributary to Hubberson -/none associated 1979, 1983 Flow sampled immediately upstream from where <br /> [reek (SN88W22A[B) D=B8S 1986-present road crosses creek. <br /> 7,225 ft. <br />S-7 Hubberson Gulch -/none associated 1979, 1983, 1987, Two springs exist in this area and both have <br /> (SN88W218DA) 6,865 ft. 0=885 1989, 1990 been referred to as S-7. Data from 1983 is <br /> c <br /> (monitoring requirements from the "Peter Spring" which has a very low ~ <br /> no longer in effect) flow (max. observed = 0.04 gpm) and is currently <br /> not in use. It is located approx. 250 ft. WSW <br /> of the homestead and issues from an iron pipe <br /> from the side of the hill. Date beginning in <br /> 1987 (8 also possibly the original 1979 spring <br /> survey) is from an infiltration gallery placed <br /> in the alluvium and discharging into a clear <br /> welt. It is referred to as the "Joshua Spring" <br /> and has a maximum observed flow of 13 gpm. It <br /> is located approx. 30 ft. WSW of the homestead. <br /> Noni[oring continues at the "Joshual Spring". <br />5-23 Tributary to Hubberson -/none associated 1979, 1983 Flow of spring fed creek sampled 100 yards <br /> Gulch (SN88W220AD) 0=B8S 1986-present upstream of stock pond. <br /> 7,470 ft. <br />5-41 Tributary to Hubberson -/none associated 1979, 1983 Composite of several seeps ere monitored in <br /> Gulch (SN88W22ADC) 0=B8S 1986-present spring fed stream channel <br /> 7,315 ft. <br /> r <br />5-45 Dry Creek (SN88W9CDC) -/none associated 1979, 1983 ~' Flow never observed; sampled from alluvial <br /> 6,740 ft. 1985-present clear well; site also known es OLSOn Spring. <br />