Spring (hydrology)(Redirected from Spring (hydrosphere))
A spring may be the result of karst topography where surface water has infiltrated the Earth's surface (recharge area), becoming part of the area groundwater. The groundwater then travels through a network of cracks and fissure—openings ranging from intergranular spaces to large caves. The water eventually emerges from below the surface, in the form of a karst spring.
The forcing of the spring to the surface can be the result of a confined aquifer in which the recharge area of the spring water table rests at a higher elevation than that of the outlet. Spring water forced to the surface by elevated sources are artesian wells. This is possible even if the outlet is in the form of a 300-foot-deep (91 m) cave. In this case the cave is used like a hose by the higher elevated recharge area of groundwater to exit through the lower elevation opening.
Non-artesian springs may simply flow from a higher elevation through the earth to a lower elevation and exit in the form of a spring, using the ground like a drainage pipe.
- Seepage or filtration spring. The term seep refers to springs with small flow rates in which the source water has filtered through permeable earth.
- Fracture springs, discharge from faults, joints, or fissures in the earth, in which springs have followed a natural course of voids or weaknesses in the bedrock.
- Tubular springs, in which the water flows from underground caverns.
Spring discharge, or resurgence, is determined by the spring's recharge basin. Factors that affect the recharge include the size of the area in which groundwater is captured, the amount of precipitation, the size of capture points, and the size of the spring outlet. Water may leak into the underground system from many sources including permeable earth, sinkholes, and losing streams. In some cases entire creeks seemingly disappear as the water sinks into the ground via the stream bed. Grand Gulf State Park in Missouri is an example of an entire creek vanishing into the groundwater system. The water emerges 9 miles (14 km) away, forming some of the discharge of Mammoth Spring in Arkansas. Human activity may also affect a spring's discharge—withdrawal of groundwater reduces the water pressure in an aquifer, decreasing the volume of flow.
Springs are often classified by the volume of the water they discharge. The largest springs are called "first-magnitude", defined as springs that discharge water at a rate of at least 2800 liters or 100 cubic feet (2.8 m3) of water per second. Some locations contain many first-magnitude springs, such as Florida where there are at least 27 known to be that size; the Missouri and Arkansas Ozarks, which contain 10 known of first-magnitude; and 11 more in the Thousand Springs area along the Snake River in Idaho. The scale for spring flow is as follows:
|Magnitude||Flow (ft3/s, gal/min, pint/min)||Flow (L/s)|
|1st magnitude||> 100 ft3/s||2800 L/s|
|2nd magnitude||10 to 100 ft3/s||280 to 2800 L/s|
|3rd magnitude||1 to 10 ft3/s||28 to 280 L/s|
|4th magnitude||100 US gal/min to 1 ft3/s (448 US gal/min)||6.3 to 28 L/s|
|5th magnitude||10 to 100 gal/min||0.63 to 6.3 L/s|
|6th magnitude||1 to 10 gal/min||63 to 630 mL/s|
|7th magnitude||2 pint to 1 gal/min||8 to 63 mL/s|
|8th magnitude||Less than 1 pint/min||8 mL/s|
|0 magnitude||no flow (sites of past/historic flow)|
Minerals become dissolved in the water as it moves through the underground rocks. This may give the water flavor and even carbon dioxide bubbles, depending on the nature of the geology through which it passes. This is why spring water is often bottled and sold as mineral water, although the term is often the subject of deceptive advertising. Springs that contain significant amounts of minerals are sometimes called 'mineral springs'. (Springs without such mineral content, meanwhile, are sometimes distinguished as 'sweet springs'.) Springs that contain large amounts of dissolved sodium salts, mostly sodium carbonate, are called 'soda springs'. Many resorts have developed around mineral springs and are known as spa towns.
In parts of the United States a stream carrying the outflow of a spring to a nearby primary stream may be called a spring branch or run. Groundwater tends to maintain a relatively long-term average temperature of its aquifer; so flow from a spring may be cooler than a summer day, but remain unfrozen in the winter. The cool water of a spring and its branch may harbor species such as certain trout that are otherwise ill-suited to a warmer local climate.
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Springs have been used for a variety of human needs including drinking water, domestic water supply, irrigation, mills, navigation, and electricity generation. Other modern uses include recreational activities such as fishing, swimming, and floating; therapy; water for livestock; fish hatcheries; and supply for bottled mineral water.
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A sacred spring, or holy well, is a small body of water emerging from underground and revered either in a Christian, pagan or other religious context, sometimes both. The lore and mythology of ancient Greece was replete with sacred and storied springs—notably, the Corycian, Pierian and Castalian. In medieval Europe, holy wells were frequently pagan sacred sites that later became Christianized. The term "holy well" is commonly employed to refer to any water source of limited size (i.e. not a lake or river, but including pools and natural springs and seeps), which has some significance in local folklore. This can take the form of a particular name, an associated legend, the attribution of healing qualities to the water through the numinous presence of its guardian spirit or Christian saint, or a ceremony or ritual centred on the well site. In Christian legend, the spring water is often said to have been made to flow by the action of a saint, a familiar theme especially in the hagiography of Celtic saints.
- Baotu Spring, Jinan, Shandong, China ("City of Springs")
- Gihon Spring, Jerusalem
- Wolmyeongdong Spring, South Korea
- Al-Hasa Springs, Saudi Arabia
- Aachtopf, Germany
- Castalian Spring, Delphi, Greece
- Fontaine de Vaucluse, France
- Pierian Spring, Pieria, Greece
- Sachsenbrunnen, Bad Harzburg, Germany
- Spring of Juturna, Roman Forum, Rome, Italy
- 20-Pipe Well, Altleiningen, Germany
- Farmakas, Troodos Mountains, Cyprus
- Bagby Hot Springs, Oregon
- Berkeley Springs, West Virginia
- Bennett Spring, Missouri
- Big Spring, Missouri
- Big Springs, Idaho
- Blue Spring, Florida
- Comal Springs, Texas
- Giant Springs, Montana
- Greer Spring, Missouri
- Mammoth Spring, Arkansas
- Maramec Spring, Missouri
- Montezuma Well, Arizona
- Niagara Springs, Idaho
- Poland Spring, Maine
- Kitch-iti-kipi, Michigan
- Little Salt Spring, Florida
- Rainbow Springs, Florida
- San Marcos Springs, Texas
- Saratoga Springs, New York
- Silver Springs, Florida
- Wakulla Springs, Florida
- Warm Springs, Georgia
- Wekiwa Springs, Florida
- Ojo Caliente, New Mexico
- Body of water
- Chalk stream
- Drinking water
- Holy well
- Hot spring
- Intermittent spring
- Karst spring
- List of Ozark springs
- List of spa towns
- List of springs in Florida
- Mineral water
- Petroleum seep
- Spa towns
- Spring supply
- Source (river or stream)
- Thousand Springs State Park
- Water cycle
- Water well
- "Springs - The Water Cycle, from USGS Water-Science School". ga.water.usgs.gov. Archived from the original on 9 May 2009.
- "USGS Surface-Water Data for Missouri". waterdata.usgs.gov.
- Vineyard and Fender, 1982. p. 12
- "USGS Surface-Water Data for Missouri". waterdata.usgs.gov.
- LaMoreaux, Philip E.; Tanner, Judy T, eds. (2001), Springs and bottled water of the world: Ancient history, source, occurrence, quality and use, Berlin, Heidelberg, New York: Springer-Verlag, ISBN 3-540-61841-4, retrieved 13 July 2010
- Springs of Missouri, Vineyard and Feder, Missouri Department of Natural Resources, Division of Geology and Land Survey in cooperation with U.S. Geological Survey and Missouri Department of Conservation, 1982
- Cohen, Stan (Revised 1981 edition), Springs of the Virginias: A Pictorial History, Charleston, West Virginia: Quarrier Press.