The water table is the term for how deep underground you have to dig to find ground water.
No, the water table is the upper surface of underground water, whereas groundwater refers to the water that is stored below the earth's surface in soil and rock formations. Groundwater exists below the water table and can be pumped to the surface for various uses.
The water table is the level below the ground where all spaces are filled with water. Wells are structures dug or drilled into the ground to access the water below the water table. The depth of a well is determined by the distance between the water table and the surface.
Water enters the water table through a process called recharge, which occurs when precipitation, such as rain or snow, infiltrates through the soil and reaches the saturation zone underground. This replenishes the groundwater stored in the water table.
ground water
A spring will flow when the water table is above where the spring exists. If no moisture replentishes the water table, or aquifier, then the spring will discontinue fo flow.
No, the water table is the upper surface of underground water, whereas groundwater refers to the water that is stored below the earth's surface in soil and rock formations. Groundwater exists below the water table and can be pumped to the surface for various uses.
Yes it is above the water table.
Water Table
The top level of ground water is called the Water Table.
The water table is the level below the ground where all spaces are filled with water. Wells are structures dug or drilled into the ground to access the water below the water table. The depth of a well is determined by the distance between the water table and the surface.
The water table
Yes the water table is the level of water under ground .... it is currently very deep under water.
The zone of saturation and the water table share two zones of ground water.
The water table
As ground water is withdrawn, the net effect is to lower the water table for the affected area.
Water enters the water table through a process called recharge, which occurs when precipitation, such as rain or snow, infiltrates through the soil and reaches the saturation zone underground. This replenishes the groundwater stored in the water table.
Ground water.