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An artesian well is a well that brings groundwater to the surface without pumping because it is under pressure within a body of rock or sediment known as an aquifer. [1] When trapped water in an aquifer is surrounded by layers of impermeable rock or clay, which apply positive pressure to the water, it is known as an artesian aquifer . [ 1 ]
Hornsby, Tennessee wells including one at Hornsby Elementary School; Ludowici Well, Ludowici, Georgia; Maka Yusota, Savage, Minnesota; McConnell Springs Park, Lexington, Kentucky; Olympia Brewery, Olympia, Washington (see Olympia Brewing Company#Use of artesian water) Polk Theater well, Lakeland, Florida; possibly used in the loop of the first ...
The majority of deep aquifers are classified as artesian because the hydraulic head in a confined well is higher than the level of the top of the aquifer. If the hydraulic head in a confined well is higher than the land surface it is a "flowing" artesian well (named after Artois in France). [citation needed]
Well Number 5, also called 164th Street Artesian Well, is an artesian well in North Lynnwood, Washington at Swamp Creek. The well puts out between 10–50 US gallons (38–189 L; 8.3–41.6 imp gal) per minute. [a] It is one of ten artesian wells that originally supplied the Alderwood area in the 1950s. [4]
Edwards and Trinity Aquifers map. The Edwards Aquifer is one of the most prolific artesian aquifers in the world. [2] Located on the eastern edge of the Edwards Plateau in the U.S. state of Texas, it is the source of drinking water for two million people, and is the primary water supply for agriculture and industry in the aquifer's region.
The Great Artesian Basin (GAB) [1] of Australia is the largest and deepest artesian basin in the world, extending over 1,700,000 square kilometres (660,000 sq mi). Measured water temperatures range from 30 to 100 °C (86 to 212 °F).
Artesian Well Park is a small pocket park near downtown Salt Lake City, Utah that contains a natural artesian spring fed by an underground aquifer. It occupies a quarter acre on the southwest corner of the intersection at 800 South and 500 East.
From the 1880s, residents and businesses in the Hutt Valley and Petone area sank wells into the aquifer for fresh water, [9] and in 1908 Lower Hutt Borough introduced a public water supply fed from artesian bores. [10] [11] Wellington and Lower Hutt also built dams and used water taken from rivers. Over the years, bores and pumping stations ...