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Alkali Creek Only a small portion of the permit area was within the Alkali Creek drainage basin. The applicant submitted very little information in regard to alluvial valley floor designation of this drainage. Therefore, the Division conservatively assumed that the unconsolidated streamlaid deposits in Alkali Creek comprise a significant alluvial valley floor. There is no current groundwater monitoring, and this road will not be used for access during the ensuing permit term. Alkali Creek Findings 1) None of the light use road was located within the alluvial valley floor nor will it be used during the ensuing term of the permit. Therefore, the Division finds that the proposed operation does not interrupt, discontinue, or preclude farming on the alluvial valley floor. 2) There is no anticipated effect to surface water in the Alkali Creek drainage as a result of remaining reclamation activities at the site. The Division finds that the proposed operation will not materially damage the quantity and quality of water in the surface and underground water systems that supply the alluvial valley floor or portions of the alluvial valley floor. 3) The proposed mining operation will not physically disturb the alluvial valley floor. As discussed above, there will be no effects on the quantity and quality of water supplied to the AVF Therefore, the Division finds that the proposed mining operations will be conducted to preserve, throughout the mining and reclamation process, the essential hydrologic functions of the alluvial valley floor. Colorado River The applicant identified unconsolidated streamlaid deposits within and adjacent to the proposed permit azea which meet the minimum size requirement of 50 feet in width by 10 acres in extent as set by the OSM alluvial valley floor guidelines. These unconsolidated streamlaid deposits border the Colorado River. Three distinct types of unconsolidated deposits were mapped which meet the geomorphic criteria for alluvial valley floors. These deposits are Quaternary terrace deposits, Quatemary transition zone between terrace and colluvial outwash, and Quatemary colluvial outwash. The unconsolidated sediments cover approximately 500 acres in the azea of the surface facilities between the Colorado River and the Grand Hogback. Of the 500 acres, 216 acres aze colluvial outwash; 136 acres are terrace deposits. Most of the azea mapped as teaace and transition zone deposits is presently used for imgated agriculture. Only a small portion of the azea mapped as colluvial outwash is presently used for irrigated agriculture. The source of water for irrigation is the Vulcan ditch which diverts water from Canyon Creek. Canyon Creek is located north of the Colorado River. 25 June 1, 2006