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Camas Creek is the source of water for the ESRP, and water in the ESRP at the base of the aquifer originates from groundwater in the Camas Creek drainage basin. Groundwater in the Camas Creek drainage basin is of meteoric origin and from winter precipitation. Groundwater in the Camas Creek drainage basin is the principal source of recharge to the ESRP aquifer, and the water quality of groundwater in the Camas Creek drainage basin affects the water quality of ground-water in the ESRP aquifer. Camas Creek is a perennial stream, with alluvial deposits (Daly et al. 2007) that indicate some recharge of groundwater to the ESRP aquifer during baseflow. The percent of total catchment area covered by alluvial deposits in the Camas Creek drainage basin is estimated to be 0.43 percent (Fig. 5).

The Camas Creek drainage basin has two primary hydrogeologic units: the ESRP aquifer underlying the ESRP (Fig. 3) and the alluvial deposits underlying the Camas Creek watershed (Daly et al. 2007). The alluvial deposits underlying the Camas Creek watershed are mapped to be thick (57.2+/-14.2 m) and relatively impermeable (Klinck et al. 2001) with limited infiltration of surface water. The thickness of the alluvial deposits is estimated to be 0.5 to 4.9 times the thickness of the ESRP aquifer (Fig. 3). The alluvial deposits underlying the Camas Creek watershed are mapped to contain no significant amounts of dissolved organic carbon (Daly et al. 2007); however, Camas Creek and the ESRP aquifer are mapped to contain dissolved organic carbon (Daly et al. 2007; Klinck et al. 2001). The total thickness of alluvial deposits underlying the Camas Creek watershed and the ESRP aquifer is estimated to be roughly equivalent to the combined thickness of the Camas Creek drainage basin and the ESRP aquifer (Fig. 3), indicating that most of the flow of groundwater in the ESRP aquifer is derived from the Camas Creek drainage basin.

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