An aquifer is a geologic layer of porous and permeable material such as sand and gravel, limestone, or sandstone, through which water flows and is stored. An artesian aquifer is a confined aquifer containing groundwater under positive pressure. An artesian aquifer is trapped water, surrounded by layers of impermeable rock or clay which apply positive pressure to the water contained within the aquifer. If a well were to be sunk into an artesian aquifer, water in the well-pipe would rise to a height corresponding to the point where hydrostatic equilibrium is reached.
- See Great Artesian Basin for the water source in Australia.
A well drilled into such an aquifer is called an artesian well. If water reaches the ground surface under the natural pressure of the aquifer, the well is termed a flowing artesian well.
From the previous statement, it can be inferred that not all aquifers are artesian (i.e., water table aquifers occur where the groundwater level at the top of the aquifer is at equilibrium with atmospheric pressure). The recharging of aquifers happens when the water table at its recharge zone is at a higher elevation than the head of the well.
- Wheeler, H. W (1980), Artesian bores of South Australia : an annotated photographic record, 1939-1948, Pioneer Books, ISBN 978-0-908065-06-6
- Federal Water Resources Assistance Program (Australia); New South Wales. Department of Water Resources. Technical Services Division; Australian Water Resources Council. Interstate Working Group on the Great Artesian Basin (1990), Specification for construction, reconditioning or plugging of bores tapping recognised aquifers of the Great Artesian Basin in New South Wales (1st ed.), Dept. of Water Resources, Technical Services Division, retrieved 19 January 2014
- Frances Gies and Joseph Gies, Cathedral, Forge, and Waterwheel subtitled "Technology and Invention in the Middle Ages". Harper Perennial, 1995 ISBN 0-06-016590-1, page 112.
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