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Health Launch of Space Shuttle Columbia from the Kennedy Space Center Miramar 122,041 72,739 Broward CR 9823 Northwest 67th Avenue. Five geologic formations form the surface of the southern portion of Florida: the Tamiami Formation Caloosahatchee Formation Anastasia Formation Miami Limestone and the Fort Thompson Formation the Tamiami Formation is a compression of highly permeable light colored fossiliferous sands and pockets of quartz 150 feet (46 m) thick It is named for the Tamiami Trail that follows the upper bedrock of the Big Cypress Swamp and underlies the southern portion of the Everglades Between the Tamiami Formation and Lake Okeechobee is the Caloosahatchee Formation named for the river over it Much less permeable this formation is highly calcitic and is composed of sandy shell marl clay and sand Water underneath the Caloosahatchee Formation is typically very mineralized Both the Tamiami and Caloosahatchee Formations developed during the Pliocene Epoch, 1870 85 2.4% Asian 1.0% 1.5% 2.4% 1.4 1980s to 1990s, See also: List of tallest buildings in Miami. . Contents Metrorail has stops throughout Miami with connections to Miami International Airport all Metrobus lines Tri-Rail and Amtrak the main bus station in Downtown is located next to the Arsht Center at the Adrienne Arsht Center Station, Dade County Courthouse built in 1928 is the tallest building built in the 1920s, Miami International Airport MIA Miami-Dade Large Hub View from one of the higher points in Miami west of downtown the highest natural point in the city of Miami is in Coconut Grove near the bay along the Miami Rock Ridge at 24 feet (7.3 m) above sea level. ! . .

2 Geography Miami FC became the first professional soccer team based in the city to win a national soccer title after winning the 2018 NPSL Championship. Air Europa Madrid Francis X Suarez Mayor of the City of Miami, 12.3 Libraries Rum-runners used the Everglades as a hiding spot during Prohibition; it was so vast there were never enough law enforcement officers to patrol it the arrival of the railroad and the discovery that adding trace elements like copper was the remedy for crops sprouting and dying quickly soon created a population boom New towns such as Moore Haven Clewiston and Belle Glade sprouted like the crops Sugarcane became the primary crop grown in South Florida Miami experienced a second real estate boom that earned a developer in Coral Gables $150 million Undeveloped land north of Miami sold for $30,600 an acre in 1925 Miami newspapers published editions weighing over 7 pounds (3.2 kg) most of it in real estate advertising Waterfront property was the most highly valued Mangrove trees were cut down and replaced with palm trees to improve the view Acres of South Florida slash pine were cleared Some of the pine was for lumber but most of the pine forests in Dade County were cleared for development, Miami Florida Business directory (23.3) 78.2 5.1 Personal income! The 2010 US Census reported that the Latino population in Miami accounted for 70% of its total population with 34.4% of city residents being of Cuban origin 15.8% had a Central American background (7.2% Nicaraguan 5.8% Honduran 1.2% Salvadoran and 1.0% Guatemalan) 8.7% were of South American descent (3.2% Colombian 1.4% Venezuelan 1.2% Peruvian 1.2% Argentinean and 0.7% Ecuadorian) 4.0% had other Hispanic or Latino origins (0.5% Spaniard) 3.2% descended from Puerto Ricans 2.4% were Dominican and 1.5% had Mexican ancestry. Richard Blanco Ice hockey: Miami Matadors (ECHL) Miami Screaming Eagles (WHA) Miami Manatees (WHA2), Initial attempts at developing agriculture near Lake Okeechobee were successful but the nutrients in the peat were rapidly removed In a process called soil subsidence oxidation of peat causes loss of volume Bacteria decompose dead sawgrass slowly underwater without oxygen When the water was drained in the 1920s and bacteria interacted with oxygen an aerobic reaction occurred Microorganisms degraded the peat into carbon dioxide and water Some of the peat was burned by settlers to clear the land Some homes built in the areas of early farms had to have their foundations moved to stilts as the peat deteriorated; other areas lost approximately 8 feet (2.4 m) of soil depth. .