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<br />remainder of the streamfln <br />charged ground water. Nai. <br />mountain and transbasin di <br />developments, diversions i <br />sions for irrigation, and <br />Surface water in the Cache. <br />under the doctrine of apps. <br />flow of the stream is suk~ <br />reservoirs located above <br />Ditch and Fossil Creek Re: <br />property. <br />The Cache la Poudre River <br />direction. The Boxelder <br />Cache la Poudre River in <br />North of the Cache la Pore.` <br />drains are evident. On t:; <br />occurring drain flows sc:; <br />Poudre River south of Co;• <br />Ground Water <br />Ground water is availab].i: <br />underlies the flood plait: <br />aquifer is 12 + feet Chic <br />per minute to properly co. <br />is hydrolically connecter? <br />from precipitation and dis- <br />t streamflow is affected by trans- <br />;;ions, storage reservoirs, power <br />municipal supply, upstream diver- <br />ern flow from irrigated areas. <br />Poudre River is fully appropriated <br />ation practiced in Colorado. The <br />to diversions by ditches and <br />Below the mining site. The Boxelder <br />,ir Inlet cross the East Rigden <br />rs in a generally southeasterly <br />flows southerly and joins the <br />northeast corner of Section 28. <br />River, a number of artificial <br />iumgartner property a naturally <br />~terly, and joi.tis the Cache la <br />~:;oad 40. <br />n a sand and gravel aquifer which <br />the Cache la Poudre River. The <br />.t yields as much as 25 gallons <br />acted wells. Water in the aquifer <br />the Cache la Poudre River and is <br />!;- 2 <br />