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ShareGroundwater is water located beneath the ground surface in soil pore spaces and in the fractures of geologic formations.
See also:
A formation of rock/soil is called an aquifer when it can yield a useable quantity of water.
The depth at which soil pore spaces become saturated with water is called the water table.
For more information about the topic Groundwater, read the full article at Wikipedia.org, or see the following related articles:
Artesian aquifer — An artesian aquifer is a confined aquifer whose water is pressurized. Water will thus flow out of an artesian well without ... > read more
Quicksand — Quicksand is loose, water-logged soil that yields easily to weight or pressure. It can be formed when sand, silt, clay, or other grainy soil is ... > read more
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Water resources — Water resources are sources of water that are useful or potentially useful to humans. It is important because it is needed for life to exist. Many ... > read moreNote: This page refers to an article that is licensed under the GNU Free Documentation License. It uses material from the article Groundwater at Wikipedia.org. See the Wikipedia copyright page for more details.
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