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Hot spring water often contains large amounts of dissolved minerals. The chemistry of hot springs ranges from acid sulfate springs with a pH as low as 0.8, to alkaline chloride springs saturated with silica, to bicarbonate springs saturated with carbon dioxide and carbonate minerals. Some springs also contain abundant dissolved iron.
The hot spring water has a pH of 7.3 to 7.6 and is considered slightly alkaline. The spring water is carbonated, and CO2 gas percolates from the springs. The water contains sodium, calcium, chloride with small amounts of magnesium; analysis shows the spring water is of the Na-Ca-HCO3-Cl type. Trace metals have been detected in the water ...
Mineral springs are naturally occurring springs that produce hard water, water that contains dissolved minerals. Salts, sulfur compounds, and gases are among the substances that can be dissolved in the spring water during its passage underground. In this they are unlike sweet springs, which produce soft water with no noticeable dissolved gasses ...
Hot springs are considered sacred by several Indigenous cultures, and along with sweat lodges have been used for ceremonial purposes. [2] Since ancient times, humans have used hot springs, public baths and thermal medicine for therapeutic effects. [3] Bathing in hot, mineral water is an ancient ritual.
The hot springs and seeps are located in the Sevier Desert on Fumarole Butte which is a basaltic andesite type of shield volcano from the Quaternary period, overlaying basalt and rhyolite. [7] The hot water emerges from a travertine and alluvial mound (sometimes described as a tufa mound) that flank the eastern side of the basalt lava formation ...
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The combined flow of the hot springs complex is estimated at 99 liters (3.5 cu ft) per second; the spring system produces 2.5 million gallons of hot mineral water per day, comprising the "largest mineral water aquifer in the Southwestern United States". [5]
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