Water Supply and Irrigation Papers of the United States Geological Survey . II. GENERAL VIEW OF QUIESCENT MUD VOLCANOES NEAR IMPERIAL JUNCTION. ORIGIN OF UNDERGROUND WATERS. 33 basin, where their source may usually be recognized in a near-by can-yon. South of Salton Sink, where the original lake was larger andthe material with which it was filled was supplied more directly FEET 0- 100 — 200- 300- 400- 500 —. 600- 700- FEET o- -r£_~==ii-i-<- ? .^~- —- ,-r- V E^=5: 100- —-„^r^=^=S ^=-iH^Ti^ gMgj^ 200- llfBIII US - nnnm 300- mSmm IHKS J^^tEEft \^jZ~ZT~ 400- ? .:.;V; - —?.:_-•—l— 500- FEET o- 1
Water Supply and Irrigation Papers of the United States Geological Survey . II. GENERAL VIEW OF QUIESCENT MUD VOLCANOES NEAR IMPERIAL JUNCTION. ORIGIN OF UNDERGROUND WATERS. 33 basin, where their source may usually be recognized in a near-by can-yon. South of Salton Sink, where the original lake was larger andthe material with which it was filled was supplied more directly FEET 0- 100 — 200- 300- 400- 500 —. 600- 700- FEET o- -r£_~==ii-i-<- ? .^~- —- ,-r- V E^=5: 100- —-„^r^=^=S ^=-iH^Ti^ gMgj^ 200- llfBIII US - nnnm 300- mSmm IHKS J^^tEEft \^jZ~ZT~ 400- ? .:.;V; - —?.:_-•—l— 500- FEET o- 100 — 200- Fig. 3.—Section of SouthernPacific well at Mecca, Cal. 300- 400- 500- 600- 700- Fig. 4.—Section of SouthernPacific well at Mortmere,Cal. 900—lFig. 2.—Section of SouthernPacific well at Indio, Cal. 60367—irr 225—09- 34 GROUND WATERS OF INDIO REGION, CALIFORNIA. by the distant Colorado River, the coarser strata are much morerare. Drill records here reveal a comparatively uniform series offine sediments through which the circulation of waters in sufficientamounts to give artesian pressures is scarcely possible. Two orthree deep wells have been drilled near Imperial, but no flow wasobtained, and the water found in limited quantity was too salineto be usable. The northern limit of these nonartesian conditions cannot be predicted closely. North of the southern e
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