Artesian aquifer

From Simple English Wikipedia, the free encyclopedia
Artesian well at the Messel pit.
Geological strata giving rise to an artesian well.
Drawing of an artesian well

An artesian aquifer is an underground layer which holds groundwater under pressure. This causes the water level in the well to rise to a point where the pressure is equal to the weight of water putting it under pressure. This type of well is called an artesian well. Water may even reach the ground surface if the natural pressure is high enough, in which case the well is called a flowing artesian well.

An aquifer is a geologic layer which can hold water such as sand and gravel, limestone, or sandstone, through which water flows and is stored. An artesian aquifer is trapped between rocks or clay which causes the pressure. Water returns to the aquifers when the water table at its recharge zone is at a higher elevation than the head of the well.

Fossil water aquifers can also be artesian if they are under sufficient pressure from the surrounding rocks. This is similar to how many newly tapped oil wells are pressurized.

Origin[change | change source]

Artesian wells were named after the old province of Artois in France. Many artesian wells were drilled there by Carthusian monks from 1126.[1]

Location[change | change source]

There are artesian aquifers in many countries including Australia, the USA, Spain, Italy, the United Kingdom, Fiji and Canada. The Great Artesian Basin is the largest and deepest artesian basin in the world, occupying 23% of the Australian continent.

References[change | change source]

  1. Gies, Frances and Joseph 1995. Cathedral, forge, and waterwheel: technology and invention in the Middle Ages. Harper Perennial, p112. ISBN 0-06-016590-1