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Mount Guyot (Great Smoky Mountains) : ウィキペディア英語版
Mount Guyot (Great Smoky Mountains)

Mount Guyot is a mountain in the eastern Great Smoky Mountains, located in
the southeastern United States. At above sea level, Guyot is the fourth-highest
summit in the eastern U.S., and the second-highest in the Great Smoky Mountains National Park(). While the mountain is remote, the Appalachian Trail crosses its south slope,
passing to within of the summit.
Mount Guyot lies on the Tennessee-North Carolina border, between Sevier County and
Haywood County. There are two peaks atop the mountain, appx. one-half mile apart,
with the southwestern peak being the true summit. The mountain rises above its
eastern base near Walnut Bottom () and above its western base near Greenbrier Cove. Ramsey Cascades, one of the park's most spectacular waterfalls, spills down a sandstone cliff near the bottom of Guyot's western
slope.
A dense stand of Southern Appalachian spruce-fir forest coats the summit and upper slopes of Guyot. Human settlement never expanded deep into the eastern Smokies, so the area around Guyot and adjacent
peaks suffered substantially less disturbance than the mountains in the western or
central parts of the range. A long hike and a challenging bushwhack are required
to reach the summit.
== Geology ==

Mount Guyot is composed of Precambrian rocks of the Ocoee Supergroup, formed
from ocean sediments approximately one billion years ago.〔Harry Moore, ''A Roadside Guide to the Geology of the Great Smoky Mountains National Park'' (Knoxville: University of Tennessee
Press, 1988), 32.〕 The mountain is underlain by
Thunderhead sandstone, which is common throughout the Smokies. The Thunderhead sandstone
was thrust over Roaring Fork sandstone several hundred million years ago.〔Harry Moore, ''A Roadside Guide to the Geology of the Great Smoky Mountains National Park'' (Knoxville: University of Tennessee Press, 1988), 66.〕 Mt. Guyot itself
was formed during the Appalachian orogeny over 200 million years ago, when the North American and African plates collided, thrusting the rock upward.〔Harry Moore,
''A Roadside Guide to the Geology of the Great Smoky Mountains National Park'' (Knoxville:
University of Tennessee Press, 1988), 23-27.〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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