The LLNL site land surface slopes approximately 1% to the northwest. Hills of the Diablo Range flank the site to the south and east. The site is underlain by several hundred feet of complexly interbedded alluvial and lacustrine sediments.
Ground water beneath the site is partly within the Spring and Mocho I hydrologic subbasins (DWR, 1974). Depth to ground water at the site varies from about 120 feet in the southeast corner to about 25 feet in the northwest corner. Ground water about 2 miles west of LLNL is used for municipal supply in downtown Livermore. Ground water about 1,000 feet south of East Avenue and about 1,000 feet west of Vasco Road and south of East Avenue is used for domestic and agricultural irrigation. Two intermittent streams, the Arroyo Seco and the Arroyo Las Positas, traverse the area (Fig. 2) and recharge the ground water system during wet periods.
Land immediately north of the LLNL site is zoned for industrial use. To the west, the land use is zoned for high-density urban use. Sandia National Laboratories (SNL), Livermore are located south of the site (Fig. 2) in an area zoned for industrial development. The area east of LLNL is zoned for agriculture and is currently used as pasture land [LLNL Remedial Investigation (RI), Thorpe et al., 1990].
As reported in the Draft Environmental Impact Statement and Environmental Impact Report for LLNL and Sandia National Laboratories, Livermore (DOE and University of California, 1992), no threatened or endangered species are present at the LLNL Livermore site. Wetlands are very limited at the Livermore site and consist of three small areas associated with culverts that channel runoff from the surrounding area into Arroyo Las Positas at the northern perimeter of the site (DOE and University of California, 1992).
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