A confined aquifer is a groundwater storage area that is trapped between layers of impermeable rock or sediment, which restricts the flow of water in and out of the aquifer. This layering creates pressure within the aquifer, allowing water to rise above its original level when tapped by wells. Confined aquifers are crucial for understanding groundwater flow because they often yield water under pressure, making them a vital resource for irrigation, drinking water, and industrial use.
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