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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />I-l <br /> <br />Chapter I <br /> <br />Introduction <br /> <br />The Beaver Park Water, Inc. irrigation system at Penrose, <br />Colorado has experienced difficulty in delivering water to <br />its shareholders in trelast ten years. The board of directors <br />has contacted the Colorado Water Conservation Board for assis- <br />tance in repairing the irrigation system under the Colorado <br />Water Conservation Board Construction Fund. The purpose of <br />this investigation is to examine the feasibility of making <br />repairs to the system and to estimate the cost of repairs. <br />The cost of the study is being shared by the Colorado Water <br />Conservation Board and by Beaver Park Water. <br /> <br />Beaver Park is located around the community of Penrose <br />in eastern Fremont County, Penrose is an unincorporated <br />community near the intersection of U.S. Highway 50 and <br />Colorado 115. It is 10 miles east of Canon City and 40 <br />miles southwest of Colorado Springs. Beaver Park is sit- <br />uated on a south-sloping terrace of the foothills of Pikes <br />Peak. It is bounded on the south by the Arkansas River, on <br />the west by Brush Hollow Creek and by Beaver Creek on the <br />east. Figure I-l is a location map showing the irrigation <br />system and major features, <br />The area has a gently rolling topography with a south- <br />ward slope of about 100 feet per mile. The edge of the ter- <br />race is bounded by limestone cliffs which rise up to 150 feet <br />above the level of the Arkansas River. Elevations range from <br />5300 to 5600 feet above sea level. <br />The geology of Beaver Park is composed of Cretaceous <br />marine limestone and shale outcrops which form the terrace, <br />sloping southward to the Arkansas River, Beaver Park is <br />located on the north flank of the Canon City Embayment and <br />is at the south edge of the foothills formed by upturned <br />sedimentary rocks abutting against the granitic rock uplift <br />of Pikes Peak. <br />