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Phosphites, which are present at hot springs, would have bonded together into pyrophosphite within hot springs through wet-dry cycling. [50] Like alkaline hydrothermal vents, the Hakuba Happo hot spring goes through serpentinization, suggesting methanogenic microbial life possibly originated in similar habitats.
Hot Springs Camp, the original name of Ainsworth Hot Springs, British Columbia, Canada Hot Springs Cove near Tofino, British Columbia, Canada Hotspring Island , part of the Haida Gwaii archipelago, British Columbia, Canada
Hot Springs National Park is a national park of the United States in central Garland County, Arkansas, adjacent to the city of Hot Springs. Hot Springs Reservation was initially created by an act of the United States Congress on April 20, 1832, to be preserved for future recreation. Established before the concept of a national park existed, it ...
Hot Springs is a resort city in the state of Arkansas and the county seat of Garland County. The city is located in the Ouachita Mountains among the U.S. Interior ...
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.
There are hot springs on all continents and in many countries around the world. Countries that are renowned for their hot springs include Bulgaria, Canada, Chile, Fiji, Honduras, Hungary, Iceland, India, Japan, Romania, Turkey, Taiwan, New Zealand, and the United States, but there are interesting and unique hot springs in many other places as well.
These springs range in volume from the hot springs around Glenwood Springs which keep the Colorado River from freezing for 50 miles (80 km) downstream to little springs with just a trickle of water. Water temperatures range from scalding to tepid.
Articles relating to hot springs, springs produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circulation through faults to hot rock deep in the Earth's crust.