Oldest continuously occupied archaeological site in North America
A location that was ideal for catching fish on the Chattahoochee River was one of many amazing archaeological sites, discovered by Archaeologist Robert Wauchope in 1939. Wauchope gave it an official site number on the state registry, but soon after moved to Chapel Hill, NC. Because World War II intervened, the location was apparently forgotten by subsequent generations of archaeologists.
Site 9FO1 in Forsyth County, GA contains artifacts from the Ice Age to the late 1700s, when the land was secretly taken from the Creek Confederacy by the United States and given to the Cherokees. The area was on the extreme fringe of the short-lived Eastern Cherokee Nation and was never significantly re-occupied until white settlers arrived.
The land adjacent to shoals on the Chattahoochee River at Strickland Ferry, 2-2.4 miles south of Buford Dam, was occupied continuously and longer than any Native American archaeological site in North America. In 1939, in addition to a wide range of projectile points, Archaeologist Robert Wauchope found a continuous chain of pottery from the Early Woodland, Middle Woodland, Late Woodland, Early Mississippian, Middle Mississippian, Late Mississippian and Proto-Historic Periods. This is particularly amazing, since he was unaware of the multiple village sites containing mounds that are just upstream in the bottomlands of the Chattahoochee River.
Soapstone bowls and stone tools from the Middle and Late Archaic Periods have been found at a village site just upstream from the shoals. This suggests that the ancestors of the Uchees and Creeks lived here in permanent villages from at least 3500 BC to 1790 AD. That’s in the range of a whopping 5, 300 years!
Site 9FO1 should definitely be considered a Uchee and Creek Sacred Heritage Site, plus placed on the National Register of Historic Places. The land is owned by the federal government and in a natural state, but a locale with such a legacy deserves special recognition.
Public land, but a dangerous place to visit
The archaeological zone is in a booming section of Metro Atlanta, just north of GA Hwy. 20 that connects Cummings with Buford. It was saved from destruction by real estate development by the US Army Corps of Engineers. When Buford Dam was constructed upstream in the mid-1950s, the federal government quickly became aware that sudden releases of water from the dam would be a hazard downstream. The land was purchased from a local family and left in a natural state.
The shoals on the river were an ideal place to spear fish or to trap fish in nets and weirs. The bottom of the river was rich with freshwater mussels. That attracted bands and eventually permanent villages of indigenous peoples for at least 12,000 years. Still today huge trout teem above and below the shoals.
The fishing opportunities attract fishermen and young people, who like to lay on the rocks next to the shoals. That creates a problem. A siren goes off when water is released from the dam. Sometimes the visitors to the shoals have not heard the sound of the siren. There have been several drownings here as a result.
The terrace above the shoals is safe, however. Native peoples camped here, while fishing and gathering mussels from the river bottom. What remains a mystery, though, is the presence of large amounts of Late Woodland and Mississippian mound builder pottery shards on the banks below the terrace. It would make no sense for people to hauls these large bowls and jars downstream a half mile, just to fish.
One possibility is that apocalyptic floods in the past washed the ceramics downstream. During the Little Ice Age (Colonial Period) weather patterns were different in the Southeast. The Georgia Mountains received so much snow in the winter that there were often impassible and called by the Creeks, “The Snowy Mountains.” When the snow melted in late March and early April, the waters rushed down the Chattahoochee, Savannah and Oconee Rivers. Vast areas of southeast Georgia and north central Florida would flood. In 1776, explorer William Bartram stated that the Okefenokee Swamp would swell in the spring to cover most of Southeast Georgia after the snow melted in the Appalachian Mountains, 280 miles to the north.
The climate has changed, indeed.
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