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<br />Similarity Of The Three Alluvial Aquifers <br /> <br />· River is hydraulically connected to the underlying aquifer <br /> <br />· Natural recharge occurs from deep percolation of both <br />irrigation water and precipitation <br /> <br />· Wells were constructed to supplement surface flows <br /> <br />· Wells intercept and consume ground water, which would <br />have flowed to the stream <br /> <br />· The river systems are over appropriated <br />· Each has a river compact with downstream states <br />· There are transbasin diversions into each system <br />