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Port St. John, Florida

Census-designated places in Brevard County, FloridaCensus-designated places in FloridaPopulated places on the Intracoastal Waterway in Florida
Brevard County Florida Incorporated and Unincorporated areas Port St. John Highlighted
Brevard County Florida Incorporated and Unincorporated areas Port St. John Highlighted

Port St. John is a census-designated place located between Titusville and Cocoa in Brevard County, Florida. The population was 12,267 at the 2010 United States Census. It is part of the Palm Bay–Melbourne–Titusville Metropolitan Statistical Area.

Excerpt from the Wikipedia article Port St. John, Florida (License: CC BY-SA 3.0, Authors, Images).

Port St. John, Florida
Bermuda Avenue,

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Wikipedia: Port St. John, FloridaContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 28.476944444444 ° E -80.788611111111 °
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Address

Bermuda Avenue 6734
32927
Florida, United States
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Brevard County Florida Incorporated and Unincorporated areas Port St. John Highlighted
Brevard County Florida Incorporated and Unincorporated areas Port St. John Highlighted
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Nearby Places

Windover Archeological Site
Windover Archeological Site

The Windover Archeological Site is a Middle Archaic (6000 to 5000 BC) archaeological site and National Historic Landmark in Brevard County near Titusville, Florida, United States on the central east coast of the state. Windover is a muck pond where skeletal remains of 168 individuals were found buried in the peat at the bottom of the pond. The skeletons were well preserved because of the peat. In addition, remarkably well-preserved brain tissue has been recovered from 91 skulls from the site. DNA from the brain tissue has been sequenced. The collection of human skeletal remains and artifacts recovered from Windover Pond represent among the largest finds of each type from the Archaic Period. It is considered one of the most important archeological sites ever excavated. The Windover dig site is a small pond, about 0.25 acres (1,000 m2) in area, that has held water continuously since sometime between 9000 and 8000 BC. It is next to the Atlantic coastal ridge about 5 miles (8 km) from Cape Canaveral. As the sea level was considerably lower 7,000 to 8,000 years ago than it is today, the pond originally sat above the water table, and was filled only by rainfall and runoff from the surrounding land. At that time the pond had a relatively thin layer of peat under a thin layer of water. The subsequent rise in sea level raised the local water table and in more recent times the pond has been fed by groundwater as well as rainfall. In 1984 the pond had a thick layer of peat, with five strata described by the archaeologists who excavated the pond. The peat in the center of the pond was covered by 6 feet (2 m) of water.