Ground water is water which lies in an aquifer below ground surface. Major aquifers are generally contained in deposits of gravel or other highly porous alluvial material. Aquifers are recharged by seepage from bodies of water and by precipitation. Some aquifers, such as the Ogallala Aquifer beneath the Great Plains of North America, contain water from earlier wetter periods. Intensive withdrawal from such aquifers may exceed the rate of recharge, water mining.
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