5.4 Cypress Education: in 2005 83% of people 25 years and over had at least graduated from high school and 30% had a bachelor's degree or higher Among people 16 to 19 years old 7% were dropouts; they were not enrolled in school and had not yet graduated from high school the total school enrollment in the Miami Metro Area was 1.4 million in 2005 Nursery school and kindergarten enrollment was 170,000 and elementary or high school enrollment was 879,000 children College or graduate school enrollment was 354,000. Vizcaya Museum and Gardens Miami, Later years Pompano Beach 99,845 78,191 Broward, The metropolitan areas of Miami Fort Lauderdale and West Palm Beach are located on a rise in elevation along the eastern coast of Florida called the Eastern Coastal Ridge that was formed as waves compressed ooids into a single formation Along the western border of the Big Cypress Swamp is the Immokolee Ridge (or Immokolee Rise) a slight rise of compressed sand that divides the runoff between the Caloosahatchee River and the Big Cypress This slight rise in elevation on both sides of the Everglades creates a basin and forces water that overflows Lake Okeechobee to creep toward the southwest Under both the Miami Limestone formation and the Fort Thompson limestone lies the Biscayne Aquifer a surface aquifer that serves as the Miami metropolitan area's fresh water source Rainfall and stored water in the Everglades replenish the Biscayne Aquifer directly. . The remainder of the ridge was discovered in the 1920s by the German Meteor expedition using echo-sounding equipment the exploration of the MAR in the 1950s led to the general acceptance of seafloor spreading and plate tectonics; American flamingos in South Florida, The geology of South Florida together with a warm wet subtropical climate provides conditions well-suited for a large marshland ecosystem Layers of porous and permeable limestone create water-bearing rock and soil that affect the climate weather and hydrology of South Florida the properties of the rock underneath the Everglades can be explained by the geologic history of the state the crust underneath Florida was at one point part of the African region of the supercontinent Gondwana About 300 million years ago North America merged with Africa connecting Florida with North America Volcanic activity centered on the eastern side of Florida covered the prevalent sedimentary rock with igneous rock Continental rifting began to separate North America from Gondwana about 180 million years ago When Florida was part of Africa it was initially above water but during the cooler Jurassic Period the Florida Platform became a shallow marine environment in which sedimentary rocks were deposited Through the Cretaceous Period most of Florida remained a tropical sea floor of varying depths the peninsula has been covered by seawater at least seven times since the bedrock formed, After Eastern's shutdown in 1991 it was used by a variety of European and Latin American airlines; by the 2000s (decade) American Airlines was its sole tenant the concourse was closed in 2004 and torn down the following year as part of the North Terminal Development project the immigration and customs hall remained open until 2007 when it was closed along with Concourse A. .
. U.S Representative 2.2 Hydrology Calusa and Tequesta 5 References 6.1 Fire Rescue 8 See also Miami Wind Symphony. .
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