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The Florida counties of Miami-Dade and Broward had a system of 40 year structural inspections from the mid-1970s, created in response to the DEA building collapse of August 1974 that claimed the lives of seven DEA agents. In Broward County, the recertification scheme was introduced in 2005 and became operative in January 2006. Some structures ...
Devil's Millhopper is unique in Florida in terms of its scale; over 100 feet (30 m) of rock layers are exposed. [2] The cutaway, limestone sides of the sinkhole provide an easily visible geological record of the area. Twelve springs, some more visible than others, feed the pond at the bottom of the sinkhole. In the summer, the bottom of the ...
The tremor was felt as far south as Tampa and as far north as Savannah, Georgia. In January 1880, Cuba was the center of two strong earthquakes that sent severe shock waves through the city of Key West, Florida. [8] Another earthquake centered outside Florida was the 1886 Charleston earthquake. The shock was felt throughout northern Florida ...
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The Page–Ladson archaeological and paleontological site is a deep sinkhole in the bed of the karstic Aucilla River (between Jefferson and Taylor counties in the Big Bend region of Florida) that has stratified deposits of late Pleistocene and early Holocene animal bones and human artifacts.
The Leon Sinks offer three hiking trails to the different sinkholes in the park including an observation platform at Big Dismal Sink. The trails feature over 20 species of trees and 75 different plants along with wildlife ranging from Carolina chickadees to gopher tortoises. [4] Trails: Sinkhole Trail – 3.1 miles; Gumswamp Trail – 2.3 miles
Sinkholes of Florida (9 P) Pages in category "Sinkholes of the United States" The following 26 pages are in this category, out of 26 total.
Little Salt Spring is a feature of the karst topography of Florida, specifically an example of a sinkhole.It is classified as a third magnitude spring. [4] The numerous deep vents at the bottom of the sinkhole feed oxygen-depleted groundwater into it, producing an anoxic environment below a depth of about 5 m (16.4 ft). [4]