Physical Geology
Groundwater recharge is the process through which water from precipitation, rivers, and lakes infiltrates the ground and replenishes aquifers, which are underground layers of water-bearing rock. This vital part of the hydrologic cycle ensures that groundwater resources are sustained over time, providing essential water for ecosystems, agriculture, and human use. It occurs in various settings, including urban and rural areas, and is influenced by factors like soil type, land use, and climate.
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