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<br />-23- <br />Based on the extensiveness of unconsolidated alluvium along Red Wash and the <br />probable existence of water with the stream alluvium, the area qualifies for <br />further consideration as a potential alluvial valley floor. <br />Water Availability Criteria - Artificial Flood Irrigation <br />The permittee estimated the potential average annual water yield from the Red <br />Wash drainage basin using Grunsky's Formula (Grunsky 1908, Sellars, 1965; see <br />bibliography in permit application). The estimate indicates that an average <br />of 2,090 acre feet of water could be made available annually in Red Wash. <br />This corresponds to approximately 0.32 inches of runoff, which is about 3.5 <br />percent of the annual precipitation falling on the area. <br />Actual measurements of flow on Red Wash have been made using a crest stage <br />gage station located at the mouth of the basin. With the crest stage gage <br />approach towards stream monitoring, only peak flows which occur between <br />monitoring intervals are recorded. Flows which occur at less than the peak <br />flow during any one monitoring interval will not be recorded. The crest gage <br />method is therefore useful for recording peak events only; the method has <br />limited application for determining duration of flow and hence flow volumes <br />which occur during the monitoring interval. <br />The results of the crest gage monitoring efforts on Red Wash indicate that <br />flow is almost entirely in response to snowmelt and storm rainfall events. A <br />total of six runoff events were recorded during the two year inventory period <br />conducted by the permittee. Events which occurred during the fall and summer <br />months resulted from thunderstorm activity; however, peak flows during the <br />year were greatest during the spring as a result of snowmelts. The largest <br />event recorded for Red Wash during the inventory period was 240 cfs, which was <br />generated as a result of late winter snowmelt. Because of the nature and <br />intent of crest gage type flow monitoring, it has limited usefulness for <br />identifying water availability criteria necessary for alluvial valley floor <br />interpretation. Therefore, the most useful information supplied by the <br />permittee for AVF purposes is the estimation of average annual streamflow <br />calculated through Grunskys formula. The amount of water available annually, <br />as estimated through his method, indicates that Red Wash further qualifies as <br />a potential alluvial valley floor. <br />subirrigation <br />At the time of issuance of the initial permanent regulatory program permit, <br />the presence of subirrigation along Red Wash had been investigated by the <br />permittee solely on the basis of vegetation identified along the drainage. <br />Vegetative species indicative of subirrigated conditions were mapped by the <br />permittee and are shown on Map of 129 of Volume 11 of the application. The <br />results indicate that a big sage brush -greasewood community exists along the <br />majority of the streamlaid deposits identified on Map 102. The permittee <br />indicated that water in the alluvium is available to the plant species <br />identified in the big range brush - greasewood community, as most of the <br />species are deep rooted and xerophytic. Since no evidence was provided by the <br />permittee during the original permit review to support the contention that <br />subirrigation was not occurring, it was concluded that subirrigation is a <br />distinct possibility along the entire length of unconsolidated streamlaid <br />deposits identified on Map 129. <br />