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Gregory Bald - Wikipedia, the free encyclopedia

Gregory Bald

From Wikipedia, the free encyclopedia

Gregory Bald

Gregory Bald, snow-capped, looking south from Foothills Parkway
Elevation 4,949 feet (1,508 metres)
Location Tennessee, USA
Range Great Smoky Mountains
Prominence 1107 feet (337 metres) [1]
Coordinates 35.520536, -83.866317
Topo map USGS Gregory Bald
Easiest route Gregory Ridge Trail + Gregory Bald Trail
Looking east from the summit of Gregory Bald, with ruts of Elkmont sandstone on the lower left.
Looking east from the summit of Gregory Bald, with ruts of Elkmont sandstone on the lower left.
View from the summit of Gregory Bald, looking northeast.  Cades Cove is the strip of land in the valley below.
View from the summit of Gregory Bald, looking northeast. Cades Cove is the strip of land in the valley below.
The Gregory Bald Trail approaching the summit.
The Gregory Bald Trail approaching the summit.

Gregory Bald is a mountain on the western fringe of the Great Smoky Mountains. It has an elevation of 4,949 feet (1,508 meters) above sea level. The mountain's majestic summit makes it a popular hiking destination.

Gregory Bald is located along the Tennessee-North Carolina border, between Blount County and Swain County. It rises appx. 3,000 feet above its northern base in Cades Cove, and appx. 3,300 feet above its southern base at Fontana Lake. The mountain is located entirely within the Great Smoky Mountains National Park.

Gregory Bald is a type of mountain known as a grassy bald. Unlike most summits in the Appalachians, which are heavily-forested or culminate in jagged peaks, grassy balds are covered by a thick layer of wild grass. Trees and other foliage are sparse. How and why a summit develops into a grassy bald is unknown. While there is evidence that Gregory Bald was a natural grassy bald, the National Park Service must currently work to prevent the summit from becoming forested.[1]

Contents

[edit] Geology

Gregory Bald is composed of a precambrian rock known as Elkmont sandstone.[2] In a few places atop the mountain, sandstone ruts actually erupt through the thick grass. The Elkmont sandstone is part of the Ocoee Supergroup, which was formed from ancient ocean sediments between 500 million and one billion years ago. Gregory Bald, along with most mountains in the area, was formed appx. 200 million years ago during the Appalachian orogeny.[3]

[edit] History

The Cherokee name for Gregory Bald was "Tsistu'yi," or "Rabbit Place." According to tribal lore, the chief of all rabbits— known simply as the Great Rabbit— lived at the summit.[4] The rabbit, considered by the Cherokee to be sly and mischievous, was a key figure in tribal legends, showing the importance the tribe placed upon the mountain.[5]

The mountain was listed by Arnold Guyot in his 1856 survey of the Smokies, although Guyot gave it the name "Great Bald's Central Peak", and measured its elevation at 4,922 feet.[6] The name "Gregory Bald" was given to the mountain by Cades Cove residents in honor of Russell Gregory (1805-1863), a prominent Cades Cove settler. Gregory used the mountain to graze cattle during the spring and summer, when the fields in the cove were needed for growing crops. He lived atop the mountain during this part of the year in a circular stone house near the mountain's summit (the house is no longer standing).[7] Gregory, who (like most Cades Covers) supported the Union during the U.S. Civil War, was murdered by Confederate guerillas in 1863.[8]

[edit] Access

The summit of Gregory Bald can be reached via several well-maintained hiking trails. From Cades Cove, the summit can be reached via the Gregory Ridge Trail (5.5 miles). This trail begins at the end of Forge Creek Road, which is a gravel road on the Cades Cove Loop just past the Cable Mill area. From Fontana, the summit is reached via the Appalachian Trail and a two-mile connector trail (7.3 miles). From Twentymile, the summit is reached via the Wolf Ridge Trail (7.3 miles).

From the summit, one can see Cades Cove and Rich Mountain to the north, and the Nantahala and Yellow Creek Mountains to the south. Visible to the east is the crest of the Smokies, including Thunderhead Mountain and Clingman's Dome. Fontana Lake and Shuckstack are discernible to the southeast.

[edit] References

  1. ^ Durwood Dunn, Cades Cove: The Life and Death of an Appalachian Community (Knoxville: University of Tennessee Press, 1988), 33.
  2. ^ Harry Moore, A Roadside Guide to the Geology of the Great Smoky Mountains National Park (Knoxville: University of Tennessee Press, 1988), 150.
  3. ^ Harry Moore, A Roadside Guide to the Geology of the Great Smoky Mountains National Park (Knoxville: University of Tennessee Press, 1988), 26-27.
  4. ^ James Mooney, Myths of the Cherokee and Sacred Formulas of the Cherokee (Nashville: Charles Elder, 1972), 407.
  5. ^ James Mooney, Myths of the Cherokee and Sacred Formulas of the Cherokee (Nashville: Charles Elder, 1972), 231.
  6. ^ Robert Mason, The Lure of the Great Smokies (Boston and New York: Houghton-Mifflen, 1927), 55-56.
  7. ^ Durwood Dunn, Cades Cove: The Life and Death of an Appalachian Community (Knoxville: University of Tennessee Press, 1988), 44.
  8. ^ Durwood Dunn, Cades Cove: The Life and Death of an Appalachian Community (Knoxville: University of Tennessee Press, 1988), 136.


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