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What is the level water naturally sinks to?
The level water naturally sinks to is known as the water table. This is the underground depth at which the soil and rock are saturated with water. The water table can vary depending on factors such as rainfall, geological formations, and human activities.
What factors have led to the reduction of water table level in fields?
what factors have led to reduction of water table level in the field
What does the water table and water wells have in common?
"Water table" means the level of water underground. So when you dig a well, you have to dig down at least to that level.
What is the top level of ground water called?
The top level of ground water is called the Water Table.
What do you call the upper level of underground water?
the water table
What is the top level of groundwater in a aquifer?
Water table
What is formed when the level of land drops below the level of the water table?
When the level of land drops below the water table, it forms a depression called a groundwater basin. This basin becomes saturated with water and can lead to the formation of a lake or wetland.
What is the top level of groundwater in a aquifer called?
Water table
What is the top level groundwater in an aquifer called?
The water table.
What is the upper surface of saturated aquifer called?
The top level of groundwater in an aquifer is called the water table.
What is the top level of an aquifer referred to?
water table
What happens when the water table is above the surface at various places?
If the water table is higher the the surface of the land, water will seep out of the land surface and form a puddle, pool or lake. The depth of the water body will increase until the water surface is at the same level as the surrounding water table - this is a state of equilibrium. If the water table lowers, so will the water level in the water body, until equilibrium is reached. Water moves slowly into and out of the land surface and follows the movement of the water table in the area. Don't confuse this with storage reservoirs behind dams. These have an artificially high water level and the surrounding water table can be lower than the reservoir.
