Ponce De Leon Springs State Recreation Area
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Ponce De Leon Springs State Recreation Area
Ponce de Leon Springs State Recreation Area is a Florida State Park in Holmes County, Florida, USA. It is located in the town of Ponce de Leon. The park, which was created to provide public outdoor recreation and other park-related uses, was initially acquired on September 4, 1970, using funds from the Land Acquisition Trust Fund. Its self-proclaimed purpose is to develop, operate and maintain the property for outdoor recreation, park, historic, and related purposes, offering abundant opportunity for nature appreciation and wildlife viewing. Its primary recreational activities include swimming in the spring and hiking 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 powerful Floridan Aquifer. The spring was named in honor of Juan Ponce de Leon, an explorer who, in 1513, led the first Spanish expedition to Florida. Legend has it that the objective of Ponce de Leon's expedition was to sear ...
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Holmes County, Florida
Holmes County is a county located in the northwestern part of the U.S. state of Florida, in the Panhandle. As of the 2020 census, the population was 19,653. Its county seat is Bonifay. History Holmes County was created in 1848. The county's namesake is a point of debate. Holmes Creek – the county's eastern boundary – bore that name before the county was created, but it was originally named Weekaywehatchee (a Creek Indian name meaning "spring creek"). One claim is that the county was named for Thomas J. Holmes, who came from North Carolina to settle in the area about 1830. Another is that it is named after Holmes, an American Indian chief who settled in the area with his band of Red Stick Creek Indians after 1814. He was subsequently killed in 1818 by a raiding party sent by Andrew Jackson during the First Seminole War. Holmes County has had four county seats in its history. The first was Hewett's Bluff (later renamed Bear Pen, then Cerro Gordo), then Pittman's Fer ...
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Choctawhatchee River
The Choctawhatchee River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map , accessed 15 April 2011 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 . Overview The Choctawhatchee originates as two separate forks (East Fork and West Fork) in Barbour County, Alabama; the East Fork flows through Henry County and joins the West Fork in eastern Dale County about four miles (6 km) above Newton. The unified river then flows southwest through Dale and Geneva counties into Florida, collecting tributaries along the way: the Little Choctawhatchee River in Dale County, and the Pea River near Geneva. It then flows south into Florida, terminating at Choctawhatchee Bay. Other Alabama tributaries are Claybank Creek and Tight Eye Creek. On ...
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Rhododendron Calendulaceum
''Rhododendron calendulaceum'', the flame azalea, is a species of '' Rhododendron'' native to North America. All parts of this plant are poisonous to humans. Description It is a deciduous shrub, 120–450 cm tall. The leaves are simple, 3–7 cm long, slightly dull green above and villous below. The arrangement is generally alternate, however they appear whorled towards the tips of the branches. The flowers are 4–5 cm long, usually bright orange, but can vary from pastel orange to dark reddish-orange. These non-fragrant flowers have 4-5 lobes and grow in clusters of 5–10. It typically blooms in late May and early June. Distribution This species of ''Rhododendron'' is native to the Appalachian Mountains in the eastern United States, ranging from southern Pennsylvania and Ohio to northern Georgia. It has been reported historically in New York and Maryland, however its current native status in these states is undetermined. However, it can occur as an int ...
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Pitcher Plant
Pitcher plants are several different carnivorous plants which have modified leaves known as pitfall traps—a prey-trapping mechanism featuring a deep cavity filled with digestive liquid. The traps of what are considered to be "true" pitcher plants are formed by specialized leaves. The plants attract and drown their prey with nectar. Types The term "pitcher plant" generally refers to members of the Nepenthaceae and Sarraceniaceae families, but similar pitfall traps are employed by the monotypic Cephalotaceae and some members of the Bromeliaceae. The families Nepenthaceae and Sarraceniaceae are the most species-rich families of pitcher plants. The Nepenthaceae contains a single genus, '' Nepenthes'', containing over 100 species and numerous hybrids and cultivars. In this genus of Old World pitcher plants, the pitchers are borne at the end of tendrils that extend from the midrib of an otherwise unexceptional leaf. Old World pitcher plants are typically characterized as havin ...
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Fossiliferous Limestone
Fossiliferous limestone is any type of limestone, made mostly of calcium carbonate (CaCO3) in the form of the minerals calcite or aragonite, that contains an abundance of fossils or fossil traces. The fossils in these rocks may be of macroscopic or microscopic size. The sort of macroscopic fossils often include crinoid stems, brachiopods, gastropods, and other hard shelled mollusk remains. In some cases, microfossils such as siliceous diatom shells in deposition may convert over time to opal and chert, providing the only inferred evidence of bioactivity preserved in limestone. Fossiliferous limestone is termed biosparite limestone under the Folk classification of sedimentary rocks. Lagerstätte are a class of fossil bearing rocks that includes fossiliferous limestone. Use Fossils in general provide geologic clues to the environment of deposition, rock formation, and the types of biological activities present at the time. Index fossils are more helpful in providing geologic r ...
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Ocala, Florida
Ocala ( ) is a city in and the county seat of Marion County within the northern region of Florida, United States. As of the 2020 United States Census, the city's population was 63,591, making it the 54th most populated city in Florida. Home to over 400 thoroughbred farms and training centers, Ocala was officially named the Horse Capital of the World in 2007. Notable attractions include the Ocala National Forest, Silver Springs State Park, Rainbow Springs State Park, and the College of Central Florida. Ocala is the principal city of the Ocala, Florida Metropolitan Statistical Area, which had an estimated 2017 population of 354,353. History Ocala is located near what is thought to have been the site of ''Ocale'' or Ocali, a major Timucua village and chiefdom recorded in the 16th century. The modern city takes its name from the historical village, the name of which is believed to mean "Big Hammock" in the Timucua language. The Spaniard Hernando de Soto's expedition recorded Ocal ...
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Groundwater Contamination
Groundwater pollution (also called groundwater contamination) occurs when pollutants are released to the ground and make their way into groundwater. This type of water pollution can also occur naturally due to the presence of a minor and unwanted constituent, contaminant, or impurity in the groundwater, in which case it is more likely referred to as contamination rather than pollution. Groundwater pollution can occur from on-site sanitation systems, landfill leachate, effluent from wastewater treatment plants, leaking sewers, petrol filling stations, hydraulic fracturing (fracking) or from over application of fertilizers in agriculture. Pollution (or contamination) can also occur from naturally occurring contaminants, such as arsenic or fluoride. Using polluted groundwater causes hazards to public health through poisoning or the spread of disease (water-borne diseases). The pollutant often creates a contaminant plume within an aquifer. Movement of water and dispersion within the ...
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Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Ocala Limestone
The Ocala Limestone is a late Eocene geologic formation of exposed limestones near Ocala, Marion County, Florida. Age Period: Paleogene Epoch: Late Eocene Faunal stage: Late Clarkforkian through early Orellan Absolute Age: ~55.8 to ~33.9 mya, calculates to a period of approximately Location The Ocala Limestone is at or near the surface within the Ocala Karst District located in west-central to the northwestern part of the peninsula. It is also within the Dougherty Plain District in the north-central panhandle where it easily forms karsts. These karsts often have several feet (meters) of relief which dramatically influence the topography of the Ocala Karst District and the Dougherty Plain District. The area is abundant with disappearing streams and springs. Composition Formerly a geologic group, Ocala Limestone was downgraded to formation status by T.M. Scott in 1991.Scott, T.M, Lloyd, J.M, and Maddox, G., A Geological overview of Florida: Florida's Ground Water Quality Mon ...
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Walton County, Florida
Walton County is located on the Emerald Coast in the northwestern part of the U.S. state of Florida, with its southern border on the Gulf of Mexico. As of the 2020 census, the population was 75,305. Its county seat is DeFuniak Springs. The county is home to the highest natural point in Florida: Britton Hill, at . Walton County is included in the Crestview–Fort Walton Beach–Destin Metropolitan Statistical Area. History Walton County was organized by European Americans in 1824. It was named for Colonel George Walton Jr., secretary of the Florida Territory from 1821 to 1826. Walton, the son of George Walton, a signer of the Declaration of Independence, was born 15 August 1786 in Augusta, Georgia, and died 20 March 1859 in Petersburg, Virginia. Between 1763 and 1783 the territory that has since become Walton County was part of the colony of British West Florida. During this time British settlers permanently settled in the area, becoming the first English-speaking people ...
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