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Ponce de León Springs State Park | |
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IUCN category V (protected landscape/seascape) | |
Location | Holmes County, Florida, USA |
Nearest city | DeFuniak Springs, Florida |
Coordinates | 30°42′29″N85°55′37″W / 30.70806°N 85.92694°W |
Governing body | Florida Department of Environmental Protection |
Ponce de Leon Springs State Recreation Area is a Florida State Park in Holmes County, Florida, USA, located in the town of Ponce de Leon. The initial acquisition of the park on September 4, 1970, used funds from the Land Acquisition Trust Fund [1] for the self-proclaimed purpose developing, operating, and maintaining the property. The plan was to develop the park for outdoor recreation, historic conservation, and offering abundant opportunity for nature appreciation and wildlife viewing. [1] Today, it grants park-goers the opportunities to swim in the spring and hike along the park's nature trails.
The park's significance lies in the Ponce de Leon Spring, its most distinctive feature, which is fed by the Floridan Aquifer. The spring was named in honor of Juan Ponce de León, an explorer who, in 1513, led the first Spanish expedition to Florida. [2] It is rumored that the objective of Ponce de Leon's expedition was to search for a spring that, according to a Taino Indian legend, would restore youth to those who bathed in their waters. The legend contributes to the Ponce de Leon Springs’ unofficial title, “The Fountain of Youth”. [2]
Although named after the Spanish explorer, the springs were previously inhabited by a group of Native Americans with a rich history of activity within the area. [2] [3]
The park has a unique ecology, flora, fauna, and is covered by specific conservancy and protective efforts. [1] [4] [5] [6] [7] It is also linked to the Civil War,
Although named after the Spanish colonial explorer Ponce de León, long before the Europeans arrived in Florida, the springs were previously inhabited by a group of Native Americans known as the Chatot and Chisca Indians. [1]
It is believed that the Chisca were once the Yuchi. Hailing from Tennessee, the Yuchi left the Appalachian Highlands due to colonial wars in the 1650s. With a little record of them afterwards, it is believed that the tribe split into distinct groups; those that settled near the Choctawhatchee River became the Chisca, who are now extinct. [2] [3]
The Chatot lived west of the Apalachicola River and Chipola River basins. They once had territory spanning from the Chattahoochee River to the Choctawhatchee River. The Chatot were fierce defenders of their land, and are mentioned in a 1639 letter from the governor of Florida, in which he expresses surprise about a peace agreement between the Chatot and another tribe as "[the Chatot] never maintained peace with anybody." [8]
Following the migration of Spanish settlers to Florida, the springs quickly generated considerable attraction. The clear waters were popular for fishing, drinking, and swimming. In 1840, a log hotel was established, drawing several families into this area. [1] These early settlers were harassed and traumatized by the brutal activities of deserter gangs during the Civil War. [1]
On September 24, 1864, 700 Union soldiers briefly paused at the springs on their way to the Battle of Marianna. The soldiers, on a raid led by Brigadier General Alexander Asboth, destroyed the hotel and looted neighboring homes. Records indicate that, following the raid, the Union force sustained its first loss near the park and in the Ponce de León area. Also in the vicinity of the park, it is reported that Private Joseph Williams of Company H, the 86th U.S. Colored Infantry, was mortally wounded in an accidental shooting and left bleeding “in the lines of the enemy at Big Sandy Creek”. [1]
Ponce De León Springs comprises 386.94 acres of land in Holmes County and Walton County, Florida. The second-magnitude spring produces about 14 million gallons of water daily, outputting a 350 ft. spring-run stream. [4] The water is approximately 20 ft. deep at the spring's head, where a vent concentrates groundwater discharge to the surface. [5] [6] Like other parts of the Floridan aquifer, the water remains a constant 68 °F. [4] [7]
The springs' topography ranges from sloping to level, with streams collecting their drainage from the slopes, these stream systems[ clarification needed ] of the Choctawhatchee River, River Valley Province, and the Coastal Lowlands Province. [4] The park is also home to underlying Ocala limestone. [4]
The water in the springs emerges from the Floridan aquifer system, one of the most productive sources of groundwater in the United States and a major source of supply for agricultural, industrial, and rural uses. [9] This system is a part of the principal artesian aquifer, "the largest, oldest, and deepest aquifer in the southeastern U.S." [10] The aquifer spans 100,000 mi2, across four states in the southeast U.S. [10]
The aquifer system contains 3,500 ft. of limestone and dolomite. [10] Due to limestone's porous nature, its presence near the surface, along with Florida's rapid population growth, results in groundwater resources being highly susceptible to contamination.
Discovered in its namesake, Ocala, Florida, Ocala Limestone is "soft, white, porous, and apparently very pure" when found in Florida, but can be "very fossiliferous" in other areas. [11]
The state park protects the habitat of four rare species of pitcher plants—the parrot, purple, red, and trumpet-leaf—along the wetland areas. It also protects the habitats of other plant species, including the flame azalea, the mountain laurel, and the longleaf pine, while simultaneously preserving 40+ acres of historic turpentine woodlands. Plants found in the upland portions include rhododendron, red chokeberry, milkweed, hickory, huckleberry, blazing star, aster, oaks, pines, and blueberry. [1]
Ponce De León Springs served 111.775 acres of exotic plant species from 2001 to 2011[ clarification needed ], some invasive. The gravest incidences[ spelling? ] of invasive exotic flora, including cogon grass, wisteria, Chinese tallow trees, and Chinese privet, occurred around 2006 in the northern area of the park, but continuous treatments quelled the infestation. The effects of a later infestation of the Japanese climbing fern in the southern region of the park were minimized by swift action from park staff. [4]
The park is home to a variety of animals, including the gopher tortoise, turkey, fox, white-tailed deer, beaver, bobcat, otter, and various native and migratory birds. Fish species include catfish, largemouth bass, chain pickerel, and panfish. [4]
Some species labeled “nuisance animals” are the armadillo, feral hog, and American alligators. When rooting by armadillos or feral hogs is spotted on park property, park staff may start trapping those animals, as this rooting can damage restored flora-filled slopes. Alligators may prove to be a nuisance if they have frequent contact with park visitors. Signage in the park notifies the public of the alligators’ presence, the dangers of feeding them, and other safety concerns. [4]
The park contains a multitude of species classed by the Florida Natural Areas Inventory as critically imperiled, or listed by the U.S. Fish and Wildlife Service, Florida Fish and Wildlife Conservation Commission, or the Florida Department of Agriculture and Consumer Services as endangered, threatened or of special concern. Many of the park's plant species, such as pitcher plants, orchids and, butterworts, can be considered imperiled species, as although they were not recorded prior to the restoration of this natural park community, have in many ways recovered due to recent restoration efforts[ clarification needed ]. Restoration efforts are crucial to the reintroduction and/or survival of these particular species, with appropriate fire and hydrological regimes pertinent to restoration efforts.
For example, the Red Pitcher plant was reintroduced to the park in 2010 after multiple active efforts to locate it where it was previously recorded to exist, and its reintroduced vitality was only made possible through continued restoration of the seepage slope natural community. Many bog species within the park continue to increase in population as restoration efforts have helped expand their habitats.
Ponce de León Springs State Park falls under the protection of Florida's statutes on state parks and preserves. The parks' flora and fauna are protected from disruption by Statue 258.008, which deems the following a second-degree misdemeanor if done without permission:
(a) Cutting, carving, injuring, mutilating, moving, displacing, or breaking off any water-bottom formation or coral. [12]
(b) Capturing, trapping, or injuring a wild animal. [12]
(c) Collecting plant or animal specimens. [12]
(d) Leaving the designated public roads in a vehicle. [12]
(e) Hunting. [12]
Access to Ponce De León Springs is from north of Interstate 10 in Ponce de León, Florida, off Holmes County Road 181A, which is accessed by way of U.S. 90. [4] There are two self-guided nature tours—Spring Run and Sandy Creek—as well as seasonal park ranger-guided walks. [13] These tours are bike accessible, as well as walkable. [14]
The Everglades is a natural region of flooded grasslands in the southern portion of the U.S. state of Florida, comprising the southern half of a large drainage basin within the Neotropical realm. The system begins near Orlando with the Kissimmee River, which discharges into the vast but shallow Lake Okeechobee. Water leaving the lake in the wet season forms a slow-moving river 60 miles (97 km) wide and over 100 miles (160 km) long, flowing southward across a limestone shelf to Florida Bay at the southern end of the state. The Everglades experiences a wide range of weather patterns, from frequent flooding in the wet season to drought in the dry season. Throughout the 20th century, the Everglades suffered significant loss of habitat and environmental degradation.
Everglades National Park is a national park of the United States that protects the southern twenty percent of the original Everglades in Florida. The park is the largest tropical wilderness in the United States and the largest wilderness of any kind east of the Mississippi River. An average of one million people visit the park each year. Everglades is the third-largest national park in the contiguous United States after Death Valley and Yellowstone. UNESCO declared the Everglades & Dry Tortugas Biosphere Reserve in 1976 and listed the park as a World Heritage Site in 1979, and the Ramsar Convention included the park on its list of Wetlands of International Importance in 1987. Everglades is one of only three locations in the world to appear on all three lists.
A spring is a natural exit point at which groundwater emerges from the aquifer and flows onto the top of the Earth's crust (pedosphere) to become surface water. It is a component of the hydrosphere, as well as a part of the water cycle. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall.
The St. Johns River is the longest river in the U.S. state of Florida and it is the most significant one for commercial and recreational use. At 310 miles (500 km) long, it flows north and winds through or borders twelve counties. The drop in elevation from headwaters to mouth is less than 30 feet (9 m); like most Florida waterways, the St. Johns has a very slow flow speed of 0.3 mph (0.13 m/s), and is often described as "lazy".
The Choctawhatchee River is a 141-mile-long (227 km) river in the southern United States, flowing through southeast Alabama and the Panhandle of Florida before emptying into Choctawhatchee Bay in Okaloosa and Walton counties. The river, the bay and their adjacent watersheds collectively drain 5,350 square miles (13,900 km2).
The Floridan aquifer system, composed of the Upper and Lower Floridan aquifers, is a sequence of Paleogene carbonate rock which spans an area of about 100,000 square miles (260,000 km2) in the southeastern United States. It underlies the entire state of Florida and parts of Alabama, Georgia, Mississippi, and South Carolina.
The San Marcos River rises from the San Marcos Springs, the location of the Meadows Center for Water and the Environment, in San Marcos, Texas. The springs are home to several threatened or endangered species, including the Texas blind salamander, fountain darter, and Texas wild rice. The river is a popular recreational area, and is frequented for tubing, canoeing, swimming, and fishing.
The Edwards Aquifer is one of the most prolific artesian aquifers in the world. Located on the eastern edge of the Edwards Plateau in the U.S. state of Texas, it is the source of drinking water for two million people, and is the primary water supply for agriculture and industry in the aquifer's region. Additionally, the Edwards Aquifer feeds the Comal and San Marcos Springs, provides springflow for recreational and downstream uses in the Nueces, San Antonio, Guadalupe, and San Marcos river basins, and is home to several unique and endangered species.
Lake Jackson is a shallow, prairie lake on the north side of Leon County, Florida, United States, near Tallahassee, with two major depressions or sinkholes known as Porter Sink and Lime Sink.
Lake Miccosukee is a large swampy prairie lake in northern Jefferson County, Florida, located east of the settlement of Miccosukee. A small portion of the lake, its northwest corner, is located in Leon County. The small town of Miccosukee, Florida is located on the north eastern shore of the lake in Leon County.
The Florida Trail is one of eleven National Scenic Trails in the United States, created by the National Trails System Act of 1968. It runs 1,500 miles (2,400 km), from Big Cypress National Preserve to Fort Pickens at Gulf Islands National Seashore, Pensacola Beach. Also known as the Florida National Scenic Trail, the trail provides permanent non-motorized recreation for hiking and other compatible activities within an hour's drive of most Floridians.
Garald G. Parker Sr. (1905–2000) was a hydrologist and is known as the "Father of Florida groundwater hydrology." Parker also named the principal artesian aquifer the Floridan Aquifer.
Surficial aquifers are shallow aquifers typically less than 50 feet (15 m) thick, but larger surficial aquifers of about 60 feet (18 m) have been mapped. They mostly consist of unconsolidated sand enclosed by layers of limestone, sandstone or clay and the water is commonly extracted for urban use. The aquifers are replenished by streams and from precipitation and can vary in volume considerably as the water table fluctuates. Being shallow, they are susceptible to contamination by fuel spills, industrial discharge, landfills, and saltwater. Parts of southeastern United States are dependent on surficial aquifers for their water supplies.
The Chisca were a tribe of Native Americans living in present-day eastern Tennessee and southwestern Virginia in the 16th century. Their descendants, the Yuchi lived in present-day Alabama, Georgia, and Florida in the 17th, 18th, and early 19th centuries, and were removed to Indian Territory in the 1830s.
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An ongoing effort to remedy damage inflicted during the 20th century on the Everglades, a region of tropical wetlands in southern Florida, is the most expensive and comprehensive environmental repair attempt in history. The degradation of the Everglades became an issue in the United States in the early 1970s after a proposal to construct an airport in the Big Cypress Swamp. Studies indicated the airport would have destroyed the ecosystem in South Florida and Everglades National Park. After decades of destructive practices, both state and federal agencies are looking for ways to balance the needs of the natural environment in South Florida with urban and agricultural centers that have recently and rapidly grown in and near the Everglades.
The Ocala Limestone is a late Eocene geologic formation of exposed limestones near Ocala, Marion County, Florida.
Edward Ball Wakulla Springs State Park is a Florida State Park in Wakulla County, Florida, United States. This 6,000 acre (24 km2) wildlife sanctuary, located south of Tallahassee, is listed on the National Register of Historic Places, and designated a National Natural Landmark.
Kissingen Spring was a natural spring formerly flowing in Polk County, Southwest Florida. It was also a venue for recreation until it dried up in 1950. Hundreds of wells drilled into the Floridan Aquifer may have caused the demise of the springs. Its site is located near the northern end of Peace River, approximately 3/4 mile east of U.S. Highway 17 and 4 miles south of Florida SR 60 / south of Bartow.
Lake Barco is a lake in Putnam County, Florida, United States. It is within the Ordway-Swisher Biological Station of the Institute of Food and Agricultural Sciences. It is roughly circular, about 200 metres (660 ft) in diameter. The nearest settlement is Melrose, Florida, about 5 kilometres (3.1 mi) to the northwest.