The Grand Wash Basin in the western part of the planning area is located along the boundary of the Colorado Plateau and Basin and Range physiographic regions. Groundwater is found in recent stream alluvium, basin fill, and sedimentary rocks of the Muddy Creek Formation and underlying Cottonwood Wash Formation. The Muddy Creek Formation is composed of siltstones, sandstones and conglomerates with interbedded basaltic lavas in the northern part of the basin. The Cottonwood Wash Formation is composed of sandstones and siltstones.
There is a relatively well-defined basin-fill aquifer interbedded with basalt flows between Grand Wash and Gyp Wash (located west of the Grand Wash Cliffs, see Figure 6.2-1). This aquifer is underlain by the Muddy Creek Formation, which restricts the downward movement of water. This area was identified as favorable for groundwater development in a geohydrologic reconnaissance study of Lake Mead National Recreation Area conducted by the USGS (Bales and Laney, 1992). |