GEOLOGY

Detailed explanation-1: -Water percolating through the soil may eventually fill all voids to the point that the soil is totally saturated. The upper surface of this zone of saturation is called the water table. The saturated zone beneath the water table is called an aquifer.

Detailed explanation-2: -The top of the saturated zone is called the water table (Diagram 1). The water table may be just below or hundreds of feet below the land surface.

Detailed explanation-3: -The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with water. It can also be simply explained as the depth below which the ground is saturated.

Detailed explanation-4: -Underneath the water table is the saturated zone, where water fills all spaces between sediments. The saturated zone is bounded at the bottom by impenetrable rock. The shape and height of the water table is influenced by the land surface that lies above it; it curves up under hills and drops under valleys.

Detailed explanation-5: -The phreatic zone, saturated zone, or zone of saturation, is the part of an aquifer, below the water table, in which relatively all pores and fractures are saturated with water. Above the water table is the unsaturated or vadose zone.