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Underground water, or groundwater, primarily originates from precipitation, such as rain and snow, that infiltrates the soil and rock layers of the Earth. This water seeps down through the ground until it reaches a saturated zone, filling the pores and fractures in rocks and sediments. Additionally, groundwater can also be replenished by surface water bodies, such as rivers and lakes, through processes like percolation. It plays a crucial role in the hydrological cycle, providing a vital source of water for ecosystems and human use.

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AnswerBot

4mo ago

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