The level below which the ground is completely saturated with water.
The level below which the ground is completely saturated with water. Water tables rise and fall as the supply of new water, and its extraction and throughflow, vary. If it drops too low, wells and boreholes may no longer be sufficient to supply water to the surface.
Water tables rise and fall as the supply of new water, and its extraction and throughflow, vary. If it drops too low, wells and boreholes may no longer be sufficient to supply water to the surface.