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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1998 Excerpt: ...Hydrographic area or subarea: See figure 2 and table 1. Do., ditto 275 Blue Creek Valley 184,000 14,000 Bolke and Price, 1972 278 Curlew Valley 868,000 75,600 Bolke and Price, 1969 426,000 76,000 Baker, 1974 Chloride-balance method 16 Duck Lake Valley 243,000 8,900 Derringer, 1989b 36 Independence Valley2 251,000 9,700 Do 56 Upper Reese River Valley 592,000 30,000 Do 92 Lemmon Valley 30,800 1,600 Do 103B Stagecoach Valley 9,700 320 Do 117 Fish Lake Valley 251,000 26,800 Do 122 Gabbs Valley 381,000 4,900 Do 153 Diamond Valley 227,000 10,500 Do 163 Mesquite Valley 30,000 1,600 Do 170 Penoyer Valley 97,300 3,200 Do 173A Railroad Valley (Southern Part) 130,000 4,900 Do 173B Railroad Valley (Northern Part) 616,000 24,800 Do 178A Butte Valley (Northern Part) 48,700 2,400 Do 178B Butte Valley (Southern Part) 12,200 1,200 Do 184 Spring Valley 787,000 61,600 Do 212 Las Vegas Valley 332,500 28,000 Do 'Two areas are called Grass Valley. Area 71 is part of Humboldt flow system; area 138 forms Grass Valley flow system (see table 4 and fig. 15). Although data from area 36 (Independence Valley) is used in estimating recharge, area is just outside Great Basin study area. enough to afford significant identifiable hydraulic continuity on a regional scale, the local and intermediate types of systems are considered to be subsystems within regional flow systems. Where consolidated rocks have only low permeability and where water-budget studies do not indicate interbasin flow, regional flow was considered insignificant and the local and intermediate systems were considered to be the major flow systems. Where several basins are traversed by a major stream, and continuity between the basins is provided primarily by the stream, these interconnected basins constitute a complex regio...

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