Groundwater moves through aquifers and recharge areas, replenishing water sources below the surface.
Groundwater moves below the surface using underground springs and through connecting spaces of the aquifer. Recharge areas are locations where surface water infiltrates the ground rather than running into rivers or evaporating, marking the beginning of groundwater flow paths. Aquifers can be unconfined or confined, with unconfined aquifers being 'connected' to the surface above.
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