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<br />Revised 1/28/80 <br />Section 785.19(c) Continued <br />Information was used fran the Geologic Map of Routt County, Colorado <br />Geologic Survey, 1975, by A. E. Miller; Reconnaisance of Ground-iAater <br />Resources in apart of the Yampa River Basin between Craig and Steamboat <br />Springs, Colorado, U.S. C~ologic Survey Water-Resources Investigations <br />Report 77-4, 1977, by R. E. Brogden and T. F. Giles; and Surface Geologic <br />Map of the Twentymile Park Area, 1977, proprietary map by Amuedo and <br />Ivey, Consultant Geologists, Denver, Colorado. The above referenoed <br />maps xere drawn using aerial photography and ground reoonnaisance. The <br />• information carQiled fran these references was verified by field observa- <br />tions in May, 1979 by Enexyy Fuels personnel. <br />• <br />The alluvial, terrace and landslide deposits of more than 30 feet in <br />width in the drainages of Middle, Foidel and Fish Creek and their asso- <br />crated stream channels are shown on the Twentymile Park Hydrology (Map 6). <br />Also shoran are delineations of the Middle, Foidel and Fish Creek watersheds <br />and the general topography of the flood plain areas. Areas where <br />unconsolidated deposits are less than 30 feet in width or where unconsoli- <br />dated deposits have been completely removed by erosion do not meet the <br />geomorphic criteria. An example of this exclusion is where Foidel Creek <br />passes through the watergap formed by the Twentymile Sandstone Formation <br />in Section 26, Township 5 North, Fange 86 West. <br />785-9(p) <br />