groundwater's Usage Examples:

materials that are saturated with groundwater in a given vicinity.

The groundwater may be from precipitation or from groundwater flowing into the aquifer.

The oldest and most common kind of well is a water well, to access groundwater in underground aquifers.

Groundwater recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater.

distribution and movement of groundwater in the soil and rocks of the Earth's crust (commonly in aquifers).

The terms groundwater hydrology, geohydrology,.

The remaining unfrozen freshwater is found mainly as groundwater, with only a small fraction present above ground or in the air.

Groundwater pollution (also called groundwater contamination) occurs when pollutants are released to the ground and make their way down into groundwater.

Water bodies include for example lakes, rivers, oceans, aquifers and groundwater.

glaciers, icebergs, bogs, ponds, lakes, rainfall, rivers, streams, and groundwater contained in underground aquifers.

had a planet-wide groundwater system and several prominent features on the planet have been produced by the action of groundwater.

quantity or quality, disputes between users, irreversible depletion of groundwater, and negative impacts on the environment.

Overdrafting is the process of extracting groundwater beyond the equilibrium yield of the aquifer.

gardens and agricultural fields or replenishing surface water and groundwater (i.

, groundwater recharge).

subsurface water and groundwater.

Arsenic contamination of groundwater is a problem that affects millions of people across the world.

Hydrology subdivides into surface water hydrology, groundwater hydrology (hydrogeology), and marine hydrology.

Department of Water Resources stated, "Because of increased pumping, groundwater levels are reaching record lows—up to 100 feet lower than previous records.

the Earth's surface (recharge area), becoming part of the area groundwater.

The groundwater then travels through a network of cracks and fissures—openings.