The Windover dig site is a small pond, about in area, that has held water continuously since sometime between 9000 and 8000 BC. It is next to the Atlantic coastal ridge about 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 of water.