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<br />1966), especially Recommendation 9(c), RFg1l1ation of r,ann1JRF, <br />which recommended the preparation of preliminary reports for <br />guidance in those areas where assistance is needed before a full <br />flood plain information report can be prepared or where a full <br />report is not scheduled. <br /> <br />Authority for funding flood plain management studies is provided by <br />Section 6 of Public Law 83-566, which authorizes the u.s. <br />Department of Agriculture to cooperate with other Federal, state <br />and local agencies to make investigations and surveys of the <br />watersheds and rivers and other waterways as a basis for the <br />development of coordinated programs. In carrying out flood plain <br />management studies, the Natural Resources Conservation Service is <br />responding to Executive Order 11988, entitled "Flood Plain <br />Management," and Executive Order 11990, entitled "Protection of <br />Wetlands" (both effective May 24, 1977). <br /> <br />DESCRIPTION OF STUDY AREA <br /> <br />A. Basin Characteristics <br />The watersheds that produce runoff to Douglas Wash in <br />Unincorporated Clifton are small in size (total area: 8.43 sq. <br />miles), elevation ranges from 6,500 ft. to 4,620 ft. The upper <br />half of the watershed, which is immediately north of Interstate <br />HighWay 70, is semi-arid land in very poor condition. The lower <br />half of the watershed from the Interstate HighWay 70 to the <br />Colorado River is mostly cultivated agricultural land with <br />residential sub-divisions concentrated in the upper portion of the <br />western boundary. The length and width of the drainage are roughly <br />5 miles and 2 miles respectively, and an average channel slope of <br />280 feet per mile or 5.3 percent. <br /> <br />The soils in the basin, along the stream channels, are mostly of <br />hydrologic group B. They are moderately deep to very deep, well <br />drained soil formed in mixed alluvium derived from Cretaceous <br />Mancos Shales and other calcareous sedimentary rocks, (Hunter <br />Canyon Formation, Mount Garfield Formation, and Sego Sandstone; all <br />of which are sandstone and shale) . <br /> <br />The vegetation in the watersheds north of the Interstate 70 is <br />range land in very poor condition; south of Interstate 70 is mostly <br />orchards and pastures in very good condition. <br /> <br />The flood plains, within the study limits, generally contain <br />typical residential and commercial property improvements such as <br />buildings, yards, fences, streets, vehicles, etc. Vegetation such <br />as lawns, shrubs, trees, flowers, and forbs are a part of the <br />landscape. There are some willows and cottonwoods along those <br />channels that have a sustained water supply. The channel does a <br />considerable amount of meandering which enhances the visual <br />aesthetics and wildlife habitat values in the area. It is also <br />important to notice that, at several places along the reaches, the <br />original stream channels are no longer there because of back- <br />filling and land-leveling. <br /> <br />2 <br /> <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 />