23% share of u.s. freshwater is provided by groundwater.
Water that is found in soil, rock, and rock formation fissures below the surface of the Earth is known as groundwater.
Groundwater makes up around 30% of all the freshwater that is readily available worldwide.
When it can produce a sufficient amount of water, a unit of rock or an unconsolidated deposit is referred to be an aquifer.
The water table is the depth at which rock cavities, fractures, and soil pore spaces are totally saturated with water.
Groundwater is replenished from the surface, where it may also naturally release at springs and seeps, as well as form oasis or wetlands.
By building and using extraction wells, groundwater is frequently withdrawn for agricultural, municipal, and industrial usage.
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