Ground water in the San Jacinto and Temecula basins, California . A. TEMESCAL WASH AND BENCH LANDS BELOW £. BENCH LANDS ALONG SOUTHWEST SIDE OF TEMESCAL W ASH BELOW LLE L\KE TEMESCAL ABEA. 79 to be growing well. As good drainage to the lake can be obtainedfrom the sun-ovmding cultivable land, toward theaccumulation of alkali after irrigation can probably be successfullyovercome by proper ditching. TEMESCAL AND Temescal Wash, the natural outlet of Elsinore Lake, extendsnorthwestward from the lake to Santa Ana River near Corona. Inmiddle stretch,
Ground water in the San Jacinto and Temecula basins, California . A. TEMESCAL WASH AND BENCH LANDS BELOW £. BENCH LANDS ALONG SOUTHWEST SIDE OF TEMESCAL W ASH BELOW LLE L\KE TEMESCAL ABEA. 79 to be growing well. As good drainage to the lake can be obtainedfrom the sun-ovmding cultivable land, toward theaccumulation of alkali after irrigation can probably be successfullyovercome by proper ditching. TEMESCAL AND Temescal Wash, the natural outlet of Elsinore Lake, extendsnorthwestward from the lake to Santa Ana River near Corona. Inmiddle stretch, at and below Temescal, the canyon of the washbroadens to a vaUey (see PI. XIV, A) with a belt of lowland varyingfrom a quarter to a haK mile in width. Along its west side, bothabove and below Temescal, the cultivable area is greatly increasedby extensive bench lands (see Pl. XIV, B) that extend upward in along, uniform slope to the base of Santa Ana Mountains. Through-out its course the wash follows the base of the granitic and schistosehills that border it on the east, and a short distance below the junc-ti
Size: 2713px × 921px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookdecade1910, bookpublisherwashingtongovtprin
