Hot spring

A hot spring is a spring that is produced by the emergence of geothermally heated groundwater from the Earth's crust. There are hot springs all over the earth, on every continent and even under the oceans and seas.

Definitions

"Blood Pond" hot spring in Beppu, Japan

There is no universally accepted definition of a hot spring. For example, one can find the phrase hot spring defined as

The related term "warm spring" is defined as a spring with water temperature less than a hot spring by many sources, although Pentecost et al. (2003) suggest that the phrase "warm spring" is not useful and should be avoided. The US NOAA Geophysical Data Center defines a "warm spring" as a spring with water between 20 °C (68 °F) and 50 °C (122 °F).

Sources of heat

The water issuing from a hot spring is heated by geothermal heat, i.e., heat from the Earth's interior. In general, the temperature of rocks within the earth increases with depth. The rate of temperature increase with depth is known as the geothermal gradient. If water percolates deeply enough into the crust, it will be heated as it comes into contact with hot rocks. The water from hot springs in non-volcanic areas is heated in this manner.

In active volcanic zones such as Yellowstone National Park, water may be heated by coming into contact with magma (molten rock). The high temperature gradient near magma may cause water to be heated enough that it boils or becomes superheated. If the water becomes so hot that it builds steam pressure and erupts in a jet above the surface of the Earth, it is called a geyser. If the water only reaches the surface in the form of steam, it is called a fumarole. If the water is mixed with mud and clay, it is called a mud pot.

Note that hot springs in volcanic areas are often at or near the boiling point. People have been seriously burned and even killed by accidentally or intentionally entering these springs.

Warm springs are sometimes the result of hot and cold springs mixing but may also occur outside of volcanic areas, such as Warm Springs, Georgia (frequented for its therapeutic effects by paraplegic U.S. President Franklin D. Roosevelt, who built the Little White House there).

Flow rates

Deildartunguhver, Iceland: the highest flow hot spring in Europe
Picture of Las Sopas hot springs on the north side of Cordón Caulle, Chile

Hot springs range in flow rate from the tiniest "seeps" to veritable rivers of hot water. Sometimes there is enough pressure that the water shoots upward in a geyser, or fountain.

A very low flow rate hot spring fed the closed resort, Fales Hot Ditch, which is north of Bridgeport, California. There is a huge subterranean lake below Tonopah, Arizona, which provides natural hot mineral waters to several hot springs. These hot springs were used by the seven or more hot spring spas that once operated in Tonopah. The ruins of two such spas are still visible in Tonopah.

High flow hot springs

There are many claims in the literature about the flow rates of hot springs. Some of the hot springs with high flow rates and high claimed flow rates. It should be noted that there are many more very high flow nonthermal springs than geothermal springs. For example, there are 33 recognized "magnitude one springs" (having a flow in excess of 2,800 liters/second) in Florida alone. Silver Springs, Florida has a flow of more than 21,000 liters/second. Springs with high flow rates include:

Therapeutic uses

Japanese open air hot spring in Nachikatsuura, Wakayama
Hammam Essalihine, Roman hot spring in Algeria

Because heated water can hold more dissolved solids, warm and especially hot springs also often have a very high mineral content, containing everything from simple calcium to lithium, and even radium. Because of both the folklore and the claimed medical value some of these springs have, they are often popular tourist destinations, and locations for rehabilitation clinics for those with disabilities.The web site of the Roosevelt rehabilitation clinic in Warm Springs, GeorgiaWeb site of rehabilitation clinics in Central Texas created because of a geothermal spring

Biota in hot springs

A thermophile is an organism — a type of extremophile — that thrives at relatively high temperatures, between 45 and 80 °CMadigan MT, Martino JM (2006). Brock Biology of Microorganisms (11th ed.). Pearson. pp. 136. ISBN 0-13-196893-9. (113 and 176 °F). Many thermophiles are archaea. Thermophiles are found in hot springs, as well as deep sea hydrothermal vents and decaying plant matter such as peat bogs and compost.

Algal mats growing in a New Zealand hot pool

Some hot springs biota are infectious to humans. For example:

List of hot springs

Distribution of geothermal springs in the US
Macaques enjoying an open air hot spring or "onsen" in Nagano
Churning Caldron in Yellowstone National Park

There are hot springs on all continents and in many countries around the world. Countries that are renowned for their hot springs include China, Costa Rica, Iceland, Iran, New Zealand, Peru, United States, Taiwan, and Japan, but there are hot springs in many other places as well:

References

Further reading

  • Marjorie Gersh-Young, Hot Springs and Hot Pools of the Southwest: Jayson Loam's Original Guide, Aqua Thermal Access, 2007. ISBN 1-890880-07-8
  • Marjorie Gersh-Young, Hot Springs & Hot Pools Of The Northwest, Aqua Thermal Access, 2008. ISBN 1-890880-08-6
  • G. J Woodsworth, Hot springs of Western Canada: a complete guide, West Vancouver: Gordon Soules Book Publishers. 1999. ISBN 0-919574-03-3
  • Clay Thompson, "Tonopah: It's Water Under The Bush", the Arizona Republic 1-12-03, p. B12

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