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Space Coast Junior/Senior High School

Florida school stubsHigh schools in Brevard County, FloridaPublic high schools in FloridaPublic middle schools in Florida

Space Coast Junior/Senior High School is located in Brevard County, Florida, in the community of Port St. John, Florida, United States. It is part of the Brevard County School District. The school name comes from its location, on the Space Coast. The high school graduated its first class in 2006. Dual enrollment is also offered, which allows students to take college classes at Eastern Florida State College to earn college credit; some of these students receive their associate degree at the same time as their high school diploma. In 1994 the school opened as a middle school and later became a Jr/Sr high in 2001. In 2014, it contained 320,474 square feet (29,773.0 m2).The campus shares the same design as Central Middle School, a middle school in West Melbourne, Florida.

Excerpt from the Wikipedia article Space Coast Junior/Senior High School (License: CC BY-SA 3.0, Authors).

Space Coast Junior/Senior High School
Banyan Street,

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N 28.47678 ° E -80.82736 °
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Banyan Street
32927
Florida, United States
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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.