The Arabian Sea.
Morocco
A confined aquifer, also known as an artesian aquifer, is bounded above and below by impermeable layers of rock or sediment which prevent water from easily entering or leaving the aquifer. This creates high pressure within the aquifer, causing water to flow upward when a well is drilled into it.
People can obtain water from an aquifer by driling a well below the water table.
Aquifers are typically found below the bedrock. Bedrock acts as a barrier that holds the water in the aquifer, with layers of soil, sand, and gravel above the bedrock helping to recharge the aquifer with water.
The bedrock below an aquifer is called the water table. For example if a hole is dug into sand, very wet and saturated sand at shallow depth this would represent the aquifer and the level to which the water rises in this hole would be called the water table.
Confined acquifer:An aquifer which is sandwiched between two layers of less permeavle material is called confined aquifer.Unconfined acquifer:Aquifers having water table in it is called unconfined aquifer.
The artesian aquifer lies deep below the earth's surface. "Don't go down to the aquifer," warned Dr. Warren. "The last couple who went didn't come back!"
The artesian aquifer lies deep below the earth's surface. "Don't go down to the aquifer," warned Dr. Warren. "The last couple who went didn't come back!"
It is either the phreatic zone or it could have an aquifer. (=^.^=)
Aquifer depths can vary greatly, ranging from a few feet to thousands of feet below the Earth's surface. The depth of an aquifer depends on various factors such as geological formations, water table levels, and regional hydrology.
An aquifer is an area below Earth's surface that is completely saturated with water, allowing for the storage and movement of groundwater. This underground reservoir can be a vital source of water for wells and springs.