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St. Johns National Wildlife Refuge

Central Florida geography stubsFlorida protected area stubsIUCN Category VNational Wildlife Refuges in FloridaProtected areas established in 1971
Protected areas of Brevard County, Florida
Fairfield fire 022711 (5613157678)
Fairfield fire 022711 (5613157678)

The St. Johns National Wildlife Refuge is part of the United States National Wildlife Refuge System, located off SR 50 just west of Titusville. The 6,255 acre (25 km2) refuge was established in 1971 to protect the now extinct dusky seaside sparrow, Ammodramus maritimus nigrescens. It is administered as part of Merritt Island National Wildlife Refuge.

Excerpt from the Wikipedia article St. Johns National Wildlife Refuge (License: CC BY-SA 3.0, Authors, Images).

St. Johns National Wildlife Refuge

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N 28.558333333333 ° E -80.8875 °
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Brevard County (Brevard)



Florida, United States
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Fairfield fire 022711 (5613157678)
Fairfield fire 022711 (5613157678)
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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.