Confined groundwater is located in an area between two layers of impermeable rock or sediment, which does not allow water to flow through it easily. It is often under high pressure and can be used as a source of artesian wells.
Confined groundwater is located in an area between two layers of impermeable rock or sediment, which does not allow water to flow through it easily. It is often under high pressure and can be used as a source of artesian wells.