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GENERAL41505
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Last modified
8/24/2016 8:09:38 PM
Creation date
11/23/2007 11:14:22 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981034
IBM Index Class Name
General Documents
Doc Date
5/1/1984
Doc Name
PROPOSED DECISION AND FINDINGS OF COMPLIANCE
Permit Index Doc Type
FINDINGS
Media Type
D
Archive
No
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Flood irrigation is very prolific in these two valleys. Eleven mayor <br />irrigation ditches were identified in the Ward Creek valley, and six mayor <br />ditches were identified in the Williams Creek valley (See Map 8 of Volume 8). <br />In addition to the main ditches identified, numerous lateral ditches exist to <br />distribute the water from the mayor ditches. Water for these irrigation <br />systems is provided, in part, by the Granby Ditch, which transports irrigation <br />water from reservoirs on Grand Mesa. An exact breakdown of how much water <br />comes from each source; the reservoirs or the natural drainages, has not been <br />provided. <br />The applicant has not provided an assessment of the capability of the area for <br />flood irrigation, but such an assessment is not necessary, since the only <br />areas that meet the geomorphic criteria are closely associated with existing <br />flood Irrigation systems. <br />The applicant has examined both vegetation information and the ground water <br />studies with regard to the potential for subirrigation. The vegetation survey <br />indicates that the only vegetation species which appear to take advantage of <br />the alluvial ground water to any extent are the hardwoods (which have no <br />agricultural significance to the area). The subirrigated hardwoods are found <br />1n areas immediately along Ward and Williams Creek, the first and second <br />terraces, and the lower fan surface near the streams. The ground water data <br />indicate that the alluvial water levels are generally 10 to 15 feet below the <br />land surface. The ground water levels are highest immediately adjacent to the <br />streams and near irrigation ditches due to leakage. The capillary fringe may <br />raise the available water levels, but this was not indicated in the vegetation <br />survey. <br />Based on the information provided by the applicant, the areas designated as <br />Qaf, Q+1, Q+2, and Q+3 along the Ward Creek and Williams Creek valleys are <br />designated as alluvial valley floors because of flood irrigation capability. <br />The applicant has indicated that the agricultural practices along the two <br />valleys are predominantly native pasture and hay for stock. There are also <br />some apple orchards in the area, and some fields in small grains (e.g. wheat, <br />oats, and barley). The applicant has provided no specific information <br />concerning the agricultural significance of the alluvial valley floor to <br />farming. Therefore, the areas designated as alluvial valley floor are assumed <br />to be agriculturally significant, and the Division will make all three <br />alluvial valley floor findings for the Ward Creek - Williams Creek alluvial <br />valley floor. <br />Alluvial Valley Floor Findings <br />Pursuant to Rule 2.06.8, the Division is required to make specific written <br />findings on the effect of mining on all AVF's within the permit and adjacent <br />area. The required findings are presented below. <br />-20- <br />
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