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<br />. <br /> <br />. <br /> <br />. <br /> <br />on205 <br /> <br />CHAPTER I <br /> <br />INTRODUCTION <br /> <br />of 12 feet. For approximately half of its length from its beginning <br />at the diversion from the Gunnison River, the tunnel waS constructed <br />in sound crystalline rock and is unlined. For the remaining half of <br />its length, the tunnel was constructed in the Mancos shale formation <br />where concrete lining was installed for stability purposes. Little <br />rehabilitation work has been necessary in the initial half of the <br />tunnel but the lining in various reachea of the latter half has <br />cracked, bulged and otherwise deteriorated. Due to frequent surveil- <br />lance followed by any necessary repair work, no major failures of <br />the tunnel lining have occurred. <br /> <br />The project includes a total of seven major diversion dams, one <br />on the Gunnison River at the head of Gunnison Tunnel, and the remain- <br />ing six on the Uncompahgre River at the heads of the Montrose and <br />Delta, Loutzenhizer, Selig, Ironstone, East and Garnet Canals. The <br />diversion dams for the Montrose and Delta, Selig, and Ironstone Canals <br />are constructed of concrete except for steel gates in the canal head- <br />works and river control sections. The remaining major diversion dams <br />are partially of timber construction. <br /> <br />The South Canal receives its water directly from the Gunnison <br />Tunnel, and, except for winter stock water diversions, water for West <br />Canal is conveyed from South Canal by a flume across the Uncompahgre <br />River. A small temporary dam is constructed each fall using stream- <br />bed materials to divert stock water from the Uncompahgre River into <br />West Canal. Other minor diversion structures are located at points <br />where flows of small streams of the area are taken into the canal <br />and lateral system. The largest of these structures is located where <br />the Hontrose and Delta Canal diven:s from Coal Creek. <br /> <br />With exception of South and West Canals, the locations for the <br />project water distribution system were essentially established prior <br />to authorization of the project. Some of the canals and laterals <br />include reaches with steep gradients and nUmerous points of abrupt <br />drops in elevation. Chutes or other types of drop structures have <br />been constructed at most of the points of abrupt elevation drop but <br />at some locations no drop structures have been provided. The amount <br />of erosion that has occurred at these latter locations varies with <br />the amount of water conveyed, the gradient through the drops, and <br />the types of lnaterials in the drop areas. A reach of the Hontrose <br />and Delta Canal about 4~ miles in length consists of the natural <br />channel of Coal Creek. Although some erosion of the channel has <br />occurred in the past, riprap has been placed at numerous locations <br />to protect against erosion and the channel is now well stabilized. <br /> <br />Combined lengths of the project canals and laterals as originally <br />constructed total about 568 miles. Hinor changes in alignment and <br />abandonment of terminal portions of a few of the laterals have reduced <br />the combined lengths of the distribution system to a current total of <br />about 565 miles. Additional data concerning lengths and capacities <br />of the canals and laterals are shown in the tabulation on page 11. <br /> <br />8 <br />