Tallahassee 18/4 20/6 23/8 27/11 31/17 33/21 33/22 33/22 32/20 28/14 23/9 19/5 A cortadito is a popular espresso beverage found in cafeterias around Miami It is particularly popular for breakfast or in the afternoon with a pastelito. . Main article: Climate of Miami School of Social Work Southside Park Brickell Humans arrived in the Florida peninsula approximately 15,000 years ago Paleo-Indians came to Florida probably following large game that included giant sloths saber-toothed cats and spectacled bears They found an arid landscape that supported plants and animals adapted for desert conditions However 6,500 years ago climate changes brought a wetter landscape; large animals became extinct in Florida and the Paleo-Indians slowly adapted and became the Archaic peoples They conformed to the environmental changes and created many tools with the various resources available During the Late Archaic period the climate became wetter again and approximately 3000 BCE the rise of water tables allowed an increase in population and cultural activity Florida Indians developed into three distinct but similar cultures that were named for the bodies of water near where they were located: Okeechobee Caloosahatchee and Glades. College of Business With the rise of sea levels that occurred during the Pleistocene approximately 17,000 years ago the runoff of water from Lake Okeechobee slowed and created the vast marshland that is now known as the Everglades Slower runoff also created an accumulation of almost 18 feet (5.5 m) of peat in the area the presence of such peat deposits dated to about 5,000 years ago is evidence that widespread flooding had occurred by then, Miami Florida Business directory, Tropical Park 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. . Black or African-American 19.2% 18.9% 16.0% Exploration Name change Haiti Haiti Miami International Airport. 2 Geology FG? (FIJI) SSS F?? 5.1 Entertainment and performing arts, Perez Art Museum in Downtown Miami.
5.5 Industry The area from Orlando to the tip of the Florida peninsula was at one point a single drainage unit When rainfall exceeded the capacity of Lake Okeechobee and the Kissimmee River floodplain it spilled over and flowed in a southwestern direction to empty into Florida Bay Prior to urban and agricultural development in Florida the Everglades began at the southern edge of Lake Okeechobee and flowed for approximately 100 miles (160 km) emptying into the Gulf of Mexico the limestone shelf is wide and slightly angled instead of having a narrow deep channel characteristic of most rivers the vertical gradient from Lake Okeechobee to Florida Bay is about 2 inches (5.1 cm) per mile creating an almost 60-mile (97 km) wide expanse of river that travels about half a mile (0.8 km) a day This slow movement of a broad shallow river is known as sheetflow and gives the Everglades its nickname River of Grass Water leaving Lake Okeechobee may require months or years to reach its final destination Florida Bay the sheetflow travels so slowly that water is typically stored from one wet season to the next in the porous limestone substrate the ebb and flow of water has shaped the land and every ecosystem in South Florida throughout the Everglades' estimated 5,000 years of existence the motion of water defines plant communities and how animals adapt to their habitats and food sources, Limestone Creek Civil Rights Movement, Race ethnicity religion and languages Public services 11.3 Colleges and universities. ! 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. The underlying bedrock or limestone of the Everglades basin affects the hydroperiod or how long an area within the region stays flooded throughout the year Longer hydroperiods are possible in areas that were submerged beneath seawater for longer periods of time while the geology of Florida was forming More water is held within the porous ooids and limestone than older types of rock that spent more time above sea level a hydroperiod of ten months or more fosters growth of sawgrass whereas a shorter hydroperiod of six months or less promotes beds of periphyton a growth of algae and other microscopic organisms There are only two types of soil in the Everglades peat and marl Where there are longer hydroperiods peat builds up over hundreds or thousands of years due to many generations of decaying plant matter Where periphyton grows the soil develops into marl which is more calcitic in composition.
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