We compare isotopic data on modern groundwater recharge, estimated from a 7-year collection of precipitation samples, with the isotopic compositions of 82 samples from wells and perennial springs collected in southeastern California. Over half the samples represent recharge that is considerably more depleted in deuterium (ΔD) than the lightest (winter) precipitation ΔD values now precipitating in nearby areas. Wells in the vicinity of irrigation canals fed from the Colorado River contain water whose ΔD resembles that of the irrigation canals, and wells adjacent to the Mojave River are recharged by Mojave River water. The remainder of the samples from the 17 hydrologic units discussed in this paper include one or more whose ΔD values are depleted in deuterium by a least 10% compared to recharge estimated from modern winter precipitation. A plot of Δ18 O versus ΔD for 56 wells and 22 springs shows substantial scatter (R2=0.66) and defines a slope of 4.9, which is lower than the slope of the Meteoric Water Line. This slope and the scatter of the data suggest these diverse waters were evaporated to different degrees before recharge, and they may also have exchanged oxygen with solid mineral phases. We interpret the fact that many groundwaters in this region have lower ΔD values than modern precipitation to indicate that recharge of many of the groundwater basins occurred during an earlier period, probably the late Pleistocene, when winters were colder, evaporation rates were lower, and precipitation was quantitatively greater and isotopically lighter. ¿ American Geophysical Union 1992