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Groundwater

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Letter enclosing report on Las Vegas water supply from Henry Albert (Reno) to Walter R. Bracken (Las Vegas) postmarked May 26, 1925

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Map showing estimated average recharge to and discharge from ground-water reservoirs by basins, and hydraulic potential in Clark and Nye counties, Nevada, 1963

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Map of part of Las Vegas Valley, Nevada, showing the approximate piezometric surface in 1912

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Map of part of Las Vegas Valley, Nevada, showing changes in the piezometric surface between February 1944 and February 1956

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Map of part of Las Vegas Valley, Nevada, showing changes in the piezometric surface between February 1955 and February 1956

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Map of part of Las Vegas Valley, Nevada, showing the piezometric surface in September 1955

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Map of part of Las Vegas Valley, Nevada, showing the piezometric surface in February 1955

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Map of part of Las Vegas Valley, Nevada, showing the approximate area of artesian flow, 1965

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Map of the Las Vegas ground-water basin, Clark, Nye, and Lincoln Counties, Nevada, 1965

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Map of the Nevada Test Site and vicinity showing principal rock types and chemistry of ground water, 1964

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Map showing configuration of potentiometric surfaces in Paleozoic and Cenozoic aquifers in the area between the Las Vegas Valley and the Amargosa Desert, Nevada, 1963

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Map showing general geology and areas of artesian flow of the Las Vegas, Pahrump, and Indian Spring Valleys, Clark and Nye Counties, Nevada, 1946

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Topographic map of groundwater in the southeast quadrangle of Las Vegas, Nevada, 1980

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Topographic map of groundwater in the southwest quadrangle of Las Vegas, Nevada, 1985

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Map of Las Vegas artesian basin, Clark County, Nevada, April 1946 (Water Resources Bulletin no. 5, plate 5)

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Map of Las Vegas Valley artesian basin, circa 1940

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Map of part of Las Vegas Valley showing the piezometric surface of the "near-surface" water during the spring of 1946 by contours, and areas of discharge by evaporation and transpiration

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Map of part of Las Vegas Valley showing contours of the composite piezometric surface during the spring of 1944, and specific capacities of wells tapping the confined water

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