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A South Appalachian Mississippian single mound and village site located on the northern bank of the Tugaloo River 1,200 feet (370 m) north of the mouth of the Chauga River in Oconee County, South Carolina now inundated by Lake Hartwell.The site is a Walls Phase Mississippian site dating back to the 15th century, located in the city of Memphis in West Tennessee and was occupied, abandoned and reoccupied several times throughout its history, spanning from 1000 to 1550 CE.To its northeast is Mound C, another platform mound with a height of 15 feet (4.6 m).A South Appalachian Mississippian culture multimound and village site located near the confluence of the Tallapoosa and Coosa rivers in modern Montgomery County, Alabama and likely occupied from 1400–1550 CE. The Mississippian culture was a mound-building Native American culture that flourished in what is now the Midwestern, inland-Eastern, and Southeastern United States from approximately 800 CE to 1500 CE, varying regionally.Its core area, along the Mississippi River, stretched from sites such as Cahokia in modern Illinois, to Mound Bottom in Tennessee, to the Winterville site in the state of Mississippi.Temple mound complexes further extend from Aztalan in Wisconsin to Crystal River in Florida, and from Fort Ancient now in Ohio to Spiro in Oklahoma, while Mississippian cultural influences extended as far north and west, as modern North Dakota.

It is located at mile 106.9 on the old Natchez Trace, now the Natchez Trace Parkway.

The site was a satellite village associated with the Nixon polity, remnants of the Coosa chiefdom encountered by de Soto in 1540.

It was occupied during the mid to late 1500s Type site for the Lamar Phase, located on the banks of the Ocmulgee River in Bibb County, Georgia and several miles to the southeast of the Ocmulgee Mound Site.

In addition to its Mississippian-era Shine I-phase, it is the largest settlement associated with the Shine II-phase of the lower Tallapoosa River.

A village site occupied during the local Duvall Phase and Bell Phases of the South Appalachian Mississippian period and located south of the mouth of the Apalachee River on the western bank of the Oconee River and now submerged under Lake Oconee.) protohistoric Barnett Phase village located on the western bank of the Coosa River in Floyd County, Georgia.

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