The Determination of Safe Yield of Underground Reservoirs of the Closed Basin Ty

Cover The Determination of Safe Yield of Underground Reservoirs of the Closed Basin Ty
The Determination of Safe Yield of Underground Reservoirs of the Closed Basin Ty
Charles H Charles Hamilton Lee
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_J-^Lj. •Urn ^ :'- ' \ > . J, "'--* _ i-_ • - - s : " - ; . . Ryjilcal Well 1. -. . , J, . , . .. "" by L. A, m „. . , . ! . . , „ ' A, . ™, d. I„, r iia, ™ . . , „ L. , , -a„ . . .. L. Y >, ;, „''' ' : . >■ "- ^ ". S '" v > \ > V - ■*■ - * J 1. 1 1, 1 1 l ill lll l . 1 . 1 I I ■ _TX; j IT TT7I l SAFE YIELD OF UNDERGROUND RESERVOIRS 203 region, it must be exceedingly slow, and it would be entirely inter- cepted by the alluvial fan of Lone Pine Creek, which has a ground- water surface higher tha...n the valley fill to the north. The granitic formation of the Sierra Nevada and the granite core of the Inyo Mountains are complete barriers against the escape of underground waters through any formation but the valley fill. It has already been shown that there is no seepage flow into Owens River from the water supply of the region. Hence the outlets by evaporation, transpiration, and spring discharge into Owens River are all that remain to be considered.

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