The Water Table
The water table is the top level of groundwater. Surface water is an exposed part of the water …
The topmost level of groundwater is called the water table; below this level the soil is waterlogged. If a hole is dug deep enough in the soil, it may reach the water table. The water table is not at the same level everywhere. It may be close to the surface in some places and hundreds of feet beneath the soil in others. Sometimes a deep cut in the land will expose the water table. Then the groundwater runs off as a stream or river.
Changes in climatic conditions and in the amount of precipitation used by vegetation may cause the water table to rise or fall. Heavy rainfall can raise the water table. If the level becomes too high, damage can occur to plants. During times of sparse rainfall, the soil becomes extremely dry, and groundwater that seeps to the surface and evaporates is not replaced. The water table then becomes lower. If much of the lost water is not soon replaced, a drought may occur.
Water that is drawn from wells may affect the level of the water table in a given area. When groundwater is pumped to the surface, the water level in the well becomes slightly lower than the surrounding water table. Groundwater then flows downward to the level of water in the well, causing a cone of depression in the water table. This lowers the water table slightly. If water is rapidly drawn from a number of wells in the same area, the water table may be lowered considerably. The water table may rise again when sufficient rainfall occurs or when there is a decrease in the amount of water taken from wells.