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In Tennessee, Prehistoric is generally defined as the time between the appearance of the first people in the region (c. 12,000 BC) and the arrival of the first European explorers (c. 1540 AD). The Historic period begins after the arrival of those Europeans and continues to the present.
Geology of the Older Precambrian Rocks of the Grand Canyon: Part I. Petrology and Structure of the Vishnu Complex. Part II. The Zoroaster Plutonic Complex and Related Rocks. Part III. Petrology of Mafic Schists and Amphibolites. Precambrian Research, 8, pp. 219–302. Babcock, R.S. (1990). The Precambrian Crystalline Core (of the Grand Canyon).
The Tennessee River Gorge is a 26-mile (42 km) canyon formed by the Tennessee River known locally as Cash Canyon. It is the fourth largest river gorge in the Eastern United States. The gorge is cut into the Cumberland Plateau as the river winds its way into Alabama from Tennessee. The Tennessee River Gorge was also known as Walden Gorge.
Following is a list of sites and structures in Tennessee that have been designated National Historic Landmarks. There are 31 National Historic Landmarks located entirely in the state, and one that includes elements in both Tennessee and Mississippi. All National Historic Landmarks are listed on the National Register of Historic Places.
Video and images from four residents and obtained by the The Times appeared to show that before the Eaton fire exploded — scorching more than 14,100 acres, damaging and destroying more than ...
The Caney Fork rises in Cumberland County about 6 miles (10 km) west-northwest of Crossville before flowing southwest and crossing into White County.In southeastern White County it descends off the Cumberland Plateau through a deep and steep gorge known as Scott's Gulf in a remote area west of Scott Pinnacle, a locally-known mountain.
After 100 years serving the local Jewish community, the Pasadena Jewish Temple & Center was destroyed in the Eaton Fire. The congregation says it will rebuild. This Pasadena Temple burned in the ...
Grand Canyon, Arizona, at the confluence of the Colorado River and Little Colorado River.. A canyon (from Spanish: cañón; archaic British English spelling: cañon), [1] gorge or chasm, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. [2]