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<br />. <br /> <br />SECTION VII <br />WATER SOURCES <br /> <br />GENERAL <br /> <br />A municipal water system must furnish water to its customers on a con- <br /> <br /> <br />tinuous basis. Carbondale must have the legal right to take water at the <br /> <br /> <br />times and in the amounts n~eded; and the water must be physically in the <br /> <br /> <br />streams, -eservoi rs, and aqui fers to be taken. From a water resources <br /> <br /> <br />point of view, there are three princiJal limitations on a municipal water <br /> <br /> <br />supply. Fi rst is the physical avai labi 1 ity of water at the natural water <br /> <br /> <br />source, which is nonnally a stream or an aquifer; the second is the legal <br /> <br /> <br />right to divert from the natural streams and aquifers; and the third is the <br /> <br /> <br />water quality in the stream or aquifer. <br /> <br />. <br /> <br />A critical evaluation of the amount of water that a particular stream or <br /> <br /> <br />water right can yield for municipalities is based on what it will yield in <br /> <br /> <br />a dry year when natural supply is low and demand is high. Relying on averages <br /> <br /> <br />in analyzing water supplies ofter leads to a false sense of security. <br /> <br />The estimated dry year peak demand for the fi rst phase development program <br /> <br /> <br />for Carbondale is 2.5 mgd and the estimated ultimate peak day demand is 7 <br /> <br /> <br />to 8 mgd. This section of the report discusses the various water sources <br /> <br /> <br />available in the area. <br /> <br />PRESENT PHYSICAL WATER SOURCE <br /> <br /> <br />Carbondale is presently supplied with water from springs on the northwest <br /> <br /> <br />flank of Mt. Sopris along Nettle Creek, approximately seven miles south of <br /> <br /> <br />Town. Spring locations are shown on Drawing 1. The springs are perennial <br /> <br /> <br />in nature, but during periods of high irrigation (summer lawn watering), they <br /> <br /> <br />are inadequate to produce enough water to provide for the present demand. <br /> <br />The Nettle Creek spring flovl is deri ved from runoff and stored ground water <br /> <br /> <br />in the glacial fluvial debris which form an "apron" around the base of Mt. <br /> <br />. <br />