Further information: Fauna of Florida Miami Florida Business directory, 6.3 Seaports 7.4 Comprehensive Everglades Restoration Plan. . 4 Economy The Restudy came with a plan to stop the declining environmental quality and this proposal was to be the most expensive and comprehensive ecological repair project in history the Comprehensive Everglades Restoration Plan (CERP) proposed more than 60 construction projects over 30 years to store water that was being flushed into the ocean in reservoirs underground aquifers and abandoned quarries; add more Stormwater Treatment Areas to filter water that flowed into the lower Everglades; regulate water released from pumping stations into local waterways and improve water released to Everglades National Park and Water Conservation Areas; remove barriers to sheetflow by raising the Tamiami Trail and destroying the Miami Canal and reuse wastewater for urban areas the cost estimate for the entire plan was $7.8 billion and in a bipartisan show of cooperation CERP was voted through Congress with an overwhelming margin it was signed by President Bill Clinton on December 11 2000. Leisure City Agulhas Bank, Lighthouse Point Greater Downtown Miami is located in FloridaGreater Downtown Miami, Hollywood Silver Service Tri-Rail The Miami Seaquarium is a marine park on Virginia Key that has one of the world's largest collections of marine animals; some 10,000 specimens Open in 1955 the 38-acre (150,000-square-metre) park provides marine life exhibits and several daily marine mammal shows It is famous for its captive orcas dolphins and sea lions Manatee and shark exhibits are also present. The surface bedrock under the Miami area is called Miami oolite or Miami limestone This bedrock is covered by a thin layer of soil and is no more than 50 feet (15 m) thick Miami limestone formed as the result of the drastic changes in sea level associated with recent glacial periods or ice ages Beginning some 130,000 years ago the Sangamonian Stage raised sea levels to approximately 25 feet (8 m) above the current level All of southern Florida was covered by a shallow sea Several parallel lines of reef formed along the edge of the submerged Florida plateau stretching from the present Miami area to what is now the Dry Tortugas the area behind this reef line was in effect a large lagoon and the Miami limestone formed throughout the area from the deposition of oolites and the shells of bryozoans Starting about 100,000 years ago the Wisconsin glaciation began lowering sea levels exposing the floor of the lagoon by 15,000 years ago the sea level had dropped 300 to 350 feet (90 to 110 m) below the current level the sea level rose quickly after that stabilizing at the current level about 4,000 years ago leaving the mainland of South Florida just above sea level. 1.5 2000s to 2010s 4.1 Water S?? 6.3 Water and Sewer Department Allapattah and Grapeland Heights Civil Rights Movement! Including its marginal seas the Atlantic covers an area of 106,460,000 km2 (41,100,000 sq mi) or 23.5% of the global ocean and has a volume of 310,410,900 km3 (74,471,500 cu mi) or 23.3% of the total volume of the earth's oceans Excluding its marginal seas the Atlantic covers 81,760,000 km2 (31,570,000 sq mi) and has a volume of 305,811,900 km3 (73,368,200 cu mi) the North Atlantic covers 41,490,000 km2 (16,020,000 sq mi) (11.5%) and the South Atlantic 40,270,000 km2 (15,550,000 sq mi) (11.1%) the average depth is 3,646 m (11,962 ft) and the maximum depth the Milwaukee Deep in the Puerto Rico Trench is 8,486 m (27,841 ft).
2.3 National protected areas Herbert Wertheim College of Medicine, Downtown/Inner Loop Museum Park. Star Island Opening of the Central Atlantic 200-170 Ma, Main article: Transportation in Florida An embryonic subduction margin is potentially developing west of Gibraltar the Gibraltar Arc in the western Mediterranean is migrating westward into the Central Atlantic where it joins the converging African and Eurasian plates Together these three tectonic forces are slowly developing into a new subduction system in the eastern Atlantic Basin Meanwhile the Scotia Arc and Caribbean Plate in the western Atlantic Basin are eastward-propagating subduction systems that might together with the Gibraltar system represent the beginning of the closure of the Atlantic Ocean and the final stage of the Atlantic Wilson cycle.
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