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The Pisgah phase (1000 to 1450/1500 CE) is an archaeological phase of the South Appalachian Mississippian culture (a regional variation of the Mississippian culture) in Southeast North America. [1] It is associated with the Appalachian Summit area of southeastern Tennessee , Western North Carolina , and northwestern South Carolina in what is ...
Dallas peoples moved into what is now southwest Virginia from northeastern Tennessee in the early 13th century. [3] Dallas phase settlements ranged from along the Holston River to Cobb Island, and up the Nolichucky River and Little Pigeon Creek in Tennessee, and along the Clinch River in Virginia.
The Mississippian culture village and mound complex is located on the eastern bank of the Tennessee River and is covered by the modern city of Savannah, Tennessee. [1] The 16 mounds [2] form a zig-zag line of nearly a mile along the Tennessee River. The largest of the platform mounds is located at the center of the site, and was 30 feet (9.1 m ...
The Cumberland Plateau is a deeply dissected plateau, with topographic relief commonly of about 400 feet (120 metres), and frequent sandstone outcroppings and bluffs.. At Kentucky's Pottsville Escarpment, which is the transition from the Cumberland Plateau to the Bluegrass in the north and the Pennyrile in the south, there are many spectacular cliffs, gorges, rockhouses, natural bridges, and ...
The Cumberland Gap is one of many passes in the Appalachian Mountains, but one of the few in the continuous Cumberland Mountain ridgeline. [2] It lies within Cumberland Gap National Historical Park and is located on the border of present-day Kentucky and Virginia, approximately 0.25 miles (0.40 km) northeast of the tri-state marker with Tennessee.
The Museum of Appalachia, located in Norris, Tennessee, 20 miles (32 km) north of Knoxville, is a living history museum that interprets the pioneer and early 20th-century period of the Southern Appalachian region of the United States.
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Continental collisions raised the Appalachian-Ouachita chain to a lofty mountain range on the scale of the present-day Himalayas. The massive bulk of Pangea was completed near the end of the Paleozoic era (the Permian period) when Africa plowed into the continental agglomeration, with the Appalachian-Ouachita mountains near the middle. [10]