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<br />008~ <br /> <br />Most of the streamflow in Upper Monument Creek is derived from tribu- <br />taries and reservoirs that drain a part of the surrounding Rampart Range and <br />the national forest. As the stream flows southeastward toward Monument, it <br />flows through and drains a few small communities and pastures. Water is <br />diverted in this reach primarily for use as a municipal water supply. Some <br />water also is diverted to ponds and to irrigate pastures, <br /> <br />The streamflow of Upper Monument Creek has been gaged since 1977 at site <br />MIO (station 07103747 Monument Creek at Palmer Lake) (fig, I) located down- <br />stream from the Palmer Lake water-supply diversion, Generally, streamflow has <br />been smallest during the fall and winter (fig, 8A); larger and more variable <br />streamflows occurred during the spring from snowmelt runoff and during the <br />summer from thunderstorms, The mean daily streamflow-duration curve (fig, 88) <br />indicates that streamflows have been less than 2 ft)/s about 50 percent of the <br />time, and streamflows varied substantially as a result of minimal contribution <br />from ground water in storage or from upstream diversions. The frequency curve <br />of instantaneous streamflows made when water-quality samples were collected <br />differs greatly from the mean daily streamflow-duration curve, Therefore, the <br />summary statistics of water-quality constituents affected by streamflow may be <br />somewhat biased toward the larger streamflows. <br /> <br />Lower Monument Creek <br /> <br />Lower Monument Creek comprises the stream segment from Monument to the <br />confluence with Fountain Creek (fig, 2) and has been classified for class 2 <br />recreation, class 2 warm-water aquatic life, domestic water supply, and for <br />agricultural uses, Numeric water-quality standards associated with these <br />classifications are listed in table 1, <br /> <br />As Lower Monument Creek flows south toward Colorado Springs, the stream- <br />flow is affected by storage reservoirs, tributaries that drain a part of the <br />Rampart Range and a part of the Colorado Springs area, sewage effluent, <br />ground-water discharge, and diversions. Much of the stream traverses and <br />drains densely developed commercial and industrial areas, Because of urbani- <br />zation, much of the drainage area is covered by impervious material, which <br />increases the volume and peaks of direct runoff. <br /> <br />The streamflow of Lower Monument Creek has been gaged at site M28 <br />(station 07104000 Monument Creek at Pikeview) (fig. I) and is summarized in <br />figure 9, The streamflow is smallest during the fall and winter (fig, 9A); <br />larger and more variable streamflows occur during the spring from snowmelt <br />runoff and during the summer from thunderstorms, The mean daily streamflow <br />has ranged from 0 to 1,140 ft)/s and usually has been less than 13 ft)/s. <br />The steep slope of the duration curves in figure 98 indicates that stream- <br />flows vary substantially, The streamflow-duration curve for instantaneous <br />streamflow made when water-quality samples were collected is almost identical <br />to the mean daily streamflow-duration curve (fig, 98), except for extreme <br />streamflows. Therefore, the water-quality samples collected at the site <br />should characterize the water-quality conditions that occur approximately <br />96 percent of the time, <br /> <br />15 <br />