Tallulah Gorge

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View of Tallulah Gorge from an overlook 15-18-001, Tallulah Gorge - panoramio.jpg
View of Tallulah Gorge from an overlook

The Tallulah Gorge is a canyon in the southern Appalachian Mountains of the U.S. state of Georgia. Located near the town of Tallulah Falls in the northeastern part of the state, the gorge was formed by the Tallulah River as it cut through the Tallulah Dome rock formation. It measures approximately 2 miles (3 km) long and almost 1,000 feet (300 m) deep. [1] Georgia's Tallulah Gorge State Park protects much of the gorge and its waterfalls. The Tallulah Gorge has been dubbed one of the "Seven Natural Wonders of Georgia". [2]

Contents

Tallulah Falls Lake lies just above the gorge. It was created in 1913 by a hydroelectric dam built by Georgia Railway and Power (now Georgia Power) in order to run Atlanta's city streetcars. The dam still collects most of the water from the falls via a 6,666-foot (2,032 m) tunnel sluice or penstock around the falls. It then redirects the water to a 72 MW hydropower electricity generation station downstream. This station lies at an elevation 608 feet (185 m) below the lake, but a few days each year the dam releases water and the lake's water levels rise considerably. The days when water is released are especially popular for recreation, including kayaking and whitewater rafting. [3]

Tallulah Gorge, circa 1894 Tallulah Gorge (c, 1894)- USGS .jpg
Tallulah Gorge, circa 1894

History

Since the early 19th century, Tallulah Gorge and its waterfalls have been a tourist attraction. In 1882, Tallulah Falls Railway was built, increasing the accessibility of the area to visitors from Atlanta and elsewhere in Georgia, and the gorge became North Georgia's leading tourist attraction. Resort hotels and bars sprang up to serve the tourist trade, which, after the addition of the railway, swelled to as many as 2,000 people on any given Sunday. In 1883, tightrope walker Professor Bachman crossed the gorge as part of a publicity stunt for a local hotel. On July 18, 1970, Karl Wallenda became the second man to walk across the gorge on a tightrope.

In the 1910s, Georgia Railway and Power began building dams on the river. The town of Burton, Georgia was purchased and its residents relocated. The area was cleared and then flooded to become Lake Burton in 1919. Many nearby residents opposed the dams, including Helen Dortch Longstreet, widow of Confederate general James Longstreet, who led an unsuccessful campaign in 1911 to have Tallulah Gorge protected by the state. The Georgia Assembly was unable to raise the $1 million required to purchase the gorge, but Mrs. Longstreet's efforts are among the first recorded conservation movements in Georgia. Once the dam was completed in 1913, the roar of the Tallulah Falls (which could be heard for miles from the gorge) was quieted, and tourism dwindled. A state park was created by Georgia governor Zell Miller in cooperation with Georgia Power. [4]

Etymology

Georgians have long assumed that Tallulah was a Cherokee word, given the prominence of Cherokee history in the extreme northern part of the state. The word's etymology remains uncertain, and it does not clearly match either Cherokee or nearby Muscogean languages such as Creek. In his book Georgia Place-names, Kenneth K. Krakow cites John Mooney, an authority on the Cherokee language who traced the name from the Native American word talulu or taruri but concluded that both forms are untranslatable. Krakow also mentions that the American actress Tallulah Bankhead (19021968) was named for her grandmother, who was named after Tallulah Falls. [5]

Site marker at Tallulah Gorge State Park commemorating Karl Wallenda's 1970 high-wire walk Tower at site of Wallenda's crossing of Tallulah Gorge.JPG
Site marker at Tallulah Gorge State Park commemorating Karl Wallenda's 1970 high-wire walk

Geology and ecology

Persistent trillium Persistent Trillium Photo.jpg
Persistent trillium

Tallulah Dome is a rock formation caused by the double folding of the Earth's crust during the formation of Pangaea, about 500 to 250 million years ago. The dome is made up of mostly quartzite along with schist.

Because of the variation in sunlight, shade, and moisture caused by the steep cliffs, several different ecosystems exist in and around the canyon-like gorge. The persistent trillium, an endangered species of trillium, grows in this river basin and only few other parts of the South Carolina/Georgia area.

Additional photographs

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References

  1. "Tallulah Gorge State Park". Explore Georgia. Retrieved 3 March 2021.
  2. "Seven Natural Wonders of Georgia". New Georgia Encyclopedia. Retrieved 3 March 2021.
  3. "Tallulah Gorge reach description".
  4. Andrew B. McCallister (2009-02-19). "Tallulah Falls and Gorge". New Georgia Encyclopedia. Retrieved 25 July 2012.
  5. Kenneth K. Krakau. "Georgia Place-names" (PDF). Retrieved December 7, 2024.

Sources

34°43′30″N83°22′13″W / 34.72500°N 83.37028°W / 34.72500; -83.37028