SPRINGS
MAIN INDEX | Spring pictures | Springs & the aquifer | Spring magnitude | Types of springs | Water quality | Water temperature | Gateways to underwater caves | Spring life | Plant management in springs | Human impact | Springs & recreation
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| Ponce de Leon Springs, a Florida state park. |
CLEAR, FRESH WATER POURING FROM BENEATH Florida's rocky terrain has captured human interest for thousands of years. Ancient artifacts found near springs suggest that early Native Americans took advantage of the steady supply of fresh water and settled their villages along spring banks. International interest in Florida's springs erupted in the early 1500s when Spanish explorer, Ponce de Leon, scoured Florida's landscape in search of the "Fountain of Youth." By the twentieth century, "spring houses" had become popular recreation sites offering cool refuge from the scorching Florida sun. Today, Florida's springs continue to attract world-wide interest as millions of tourists and thousands of geologists travel from around the globe to appreciate and enjoy Florida's natural wonders.
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| Once popular recreation sites, spring houses
offered cool refuge from the Florida sun. Springs continue to attract millions of tourists. |
Releasing over eight billion gallons of freshwater each day, Florida has the most productive spring system in the world. Over 600 springs have been documented and geologists estimate that hundreds more are waiting to be discovered. Each spring is unique, but geologists categorize them according to specific hydrogeologic characteristics such as water flow, temperature, associated aquifer, water composition, and the shape of their opening.
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| Source: USGS |
SPRING FORMATION
Although people have enjoyed Florida's springs for thousands of years, spring development began
millions of years ago. Eons of geologic and erosional processes modelled
the limestone peninsula into a karstic region that is
characterized by a variety of unique geologic features that include freshwater springs, sinkholes,
and a poorly developed drainage system.
As a result, surface water enters the water-bearing limestone bedrock and enters the underground aquifer. When the water-table intersects the surface, freshwater flows from natural openings in the ground.
SPRINGS AND THE AQUIFER
Springs are actually the visible feature of an extensive underground aquifer system. Beneath the surface, groundwater continuously
travels from areas of
recharge, or replenishement. As groundwater accumulates beneath the surface, the
water-table rises and the subsurface water-pressure, or the hydrostatic head, increases.
Groundwater pushes along the hydraulic
gradient toward areas of discharge. Under
pressure, groundwater is
pushed to the surface through natural openings in the limestone bedrock, creating springs of
flowing water.
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Magnitude 1 - 45,000 or more gallons per minute Magnitude 2 - 4,5000-45,000 galons per minute Magnitude 3 - 450 to 4,500 gallons per minute Magnitude 4 - 100 to 450 gallons per minute Magnitude 5 - 10 to 100 gallons per minute Magnitude 6 - 1 to 10 gallons per minute Magnitude 7 - 1 pint to 1 gallon per minute Magnitude 8 - Less than 1 pint per minute Source: USGS |
Florida has twenty-seven, or one-third, of all the first magnitude springs in the U.S., more than any other state. Together, they discharge 6.2 billion gallons of water daily. This exceeds the combined output of all other springs in the world. In addition, 70 second magnitude springs and 190 smaller springs contribute another 1.8 billion gallons of water each day.
The amount of water released from a spring depends on hydrologic and geologic factors such as rainfall, permeability of the aquifer, porosity of the limestone, water pressure, subsurface flow, well pumping, shape of the spring vent, and in submarine springs, atmospheric pressure and oceanic tides.
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| Source: USGS |
SURFICIAL AND FLORIDAN SPRINGS
The type of aquifer a spring is associated with determines its magnitude, temperature, and quality
of water.
All of Florida's first magnitude springs and many of the smaller springs are associated with the Floridan Aquifer. The amount of water discharged from a Floridan spring pales in comparison to the amount of confined groundwater stored in the aquifer. As a result, Floridan spring flow remains relatively unchanged during periods of drought or heavy rains. Likewise, the water quality and average temperature of Floridan spring water remains generally constant.
In contrast, surficial springs can experience dramatic
variations in flow, temperature, and water quality. Groundwater in surficial aquifers is unconfined and continuosly
flows
from areas of recharge, or replenishment, to sites of discharge to the surface. Therefore, flow
rates of
surficial springs are affected by periods of drought and heavy rains. Water quality in a surficial
spring
may also reflect the quality of water leaching into the aquifer.
SUBMARINE SPRINGS
Along the Gulf and Atlantic coasts, submarine Floridan springs
release freshwater from beneath the ocean floor. Although they are difficult
to detect, fifteen submarine springs were discovered by 1995. If the spring is
large enough, it will disturb flat seas by creating a slick, or boil, at the
water's surface. Most occur in bays and estuaries along the Gulf coast between Lee and Wakulla
counties. At least one has been located on the Atlantic coast
2.5 miles offshore of Crescent Beach.
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WATER QUALITY
Generally, the water quality in a spring will reflect the overall conditions of the aquifer.
It can be affected by the quality of water replenishing the aquifer and the
type of rock the groundwater comes in contact with. The more time groundwater
spends in the aquifer, the greater the amount of minerals that are dissolved
in it. Spring water may also become brown from tannins. Tannins are from organic
matter such as leaves; tannic spring water is not toxic. Tannins get into the springs usually as a
result of river
water intrusion, or from surface water entering a surficial aquifer through recharge areas
and moving quickly through subsurface channels, not having the benefit of filtering through the
limestone. Spring water may also contain traces of contaminants
that have leached into an aquifer through polluted surface water.
Spring waters are well known for their clarity and freedom from algae. Algae does not flourish, even though there are sufficient nutrients and sunlight penetration into the water, because spring water is fast moving and flows away before algae has time to develop.
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| Springs are where aquifers meet the surface; looking into springs is looking into aquifers. |
The maze of underground water conduits represents a new frontier in exploration; highly skilled cave-divers continue to survey and investigate thousands of feet into underwater caves where they collect data on Florida's water quality, drainage patterns, hydrogeology, and cave biology.
SPRING LIFE
PLANTS and PLANT MANAGEMENT in FLORIDA
SPRINGS
However, non-native, invasive aquatic plants are also present in Florida springs,
sometimes
infesting them and covering them entirely. The most common invasive plants in our springs
include hydrilla,
water lettuce,
and egeria.
Springs sustain ecosystems that support life of a multitude of organisms,
including humans. Above ground, plants and animals living above and below the
water
depend on the constant supply of clean fresh springwater that feeds hundreds of freshwater
habitats in
Florida's wetlands, lakes, and rivers. Beneath the surface, aquatic cave creatures called troglobites, live in a lightless underwater environment,
relying on
consistent water temperature and water quality for survival. Slight changes in water quality or
water
flow, can
annihilate an entire population. Today, over one quarter of all
known aquatic troglobite species in
Florida are threatened or are of special concern.
Of hundreds of native aquatic and wetland plant species in Florida, relatively few are found in
the cool, fast-moving waters of springs and spring runs.
Among the most common natives found in springs are tape grass and
strap-leaf sagittaria.






sagittaria
water cress
| When exotic plants invade our springs, the plants must be controlled. Springs are generally the responsibility of the state, county, and local governments. For information about aquatic plant control in springs, please visit this page on this web site. |
HUMAN IMPACT
SPRINGS AND RECREATION
Care is necessary. Minor disturbances in a spring's water supply or ecosystem can have
devastating effects on the plants, wildlife, and people that
depend upon it. Conservation of these aquatic gems is essential in order to insure their survival for
generations to come. If protected and managed properly, springs can provide an assortmant of
recreational activities.
Here are some Florida State Parks that feature springs:
For information on what you can do to conserve Florida's waters, go to this page on our web site.
For more information about springs in Florida, visit:
Springs of
Florida, the searchable online book
Florida's Springs
U.S. Geological Survey, Groundwater
Information Pages web site
U.S. Geological Survey, Water Science for
Schools web site
Visit the Florida Springs Blog to discuss and post information and photographs.
This page was authored by Sarah Cervone.
DEP review is by Jeff Schardt and Judy Ludlow.
This project is a collaboration of
Changes in a spring's ecosystem will create a chain reaction,
jeopardizing thousands of species, including humans, for hundreds of
miles. Many of Florida's springs are threatened by urbanization and
inadequate management. As Florida's population rises, springs are increasingly
threatened by contamination, destruction, and decreased water flow. Go to this page of this web site to learn about over-pumping, bank
erosion, pollution, invasive plants and animals, scuba divers, fossil digging and other human
impacts in our springs.
Federal, state, county and city departments, as well as some private companies, manage and
protect
hundreds of Florida's freshwater springs for the public to enjoy.
by J.C. Rosenau; G.L. Faulkner; C.W.
Hendry, Jr.; and R.W. Hull
a web site of the Florida D.E.P.; scroll down for the Florida's Springs Report
Data is from the APIRS
database.
This page was designed by Sara Reinhart.
Photography and graphics are by Ann Murray, Sara Reinhart and Vic Ramey.
Vic Ramey is the editor.
the Center for Aquatic and Invasive Plants, University of Florida,
and the Bureau of Invasive Plant Management, Florida Department of Environmental
Protection
CAIP-WEBSITE@ufl.edu
Copyright 2003 University of Florida