Groundwater flow is defined as the "...part of streamflow that has infiltrated the ground, has entered the phreatic zone, and has been discharged into a stream channel, via springs or seepage water". In hydrogeology it is measured by the Groundwater flow equation.
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“The first principle of a free society is an untrammeled flow of words in an open forum.”
—Adlai Stevenson (19001965)