The Heart of the Alleghanies; or, Western North CarolinaZeigler, Wilbur Gleason
History
The Heart of the Alleghanies; or, Western North Carolina
Zeigler, Wilbur Gleason
Allegheny Mountains; North Carolina -- Description and travel
The mountain men were divided in sentiment and action during the war.
Most of the property holders joined the Confederate forces, while the
poorer classes refused to volunteer, and, when conscripted into the
service, deserted at the first opportunity. There were exceptions, of
course, with respect to both classes--some of the larger freeholders
being Union men, and some of the poor people in the coves being
enthusiastically loyal to the state.
The Southern Alleghanies, though “the oldest in the world,” have not yet
settled down to a state of absolute rest. Shocks and noises in several
localities have frequently been felt and heard, much to the discomfort
of inhabitants of the vicinity. There are reminiscences in the northern
part of Haywood county of shocks as early as 1812, and from time to time
ever since. The restless mountain is in a spur of the New Found range,
near the head of Fine’s creek. General Clingman was the first to call
public attention to it, which he did in an elaborate paper in 1848.
There are cracks in the solid granite of which the ridge is composed,
and towards its foot, chasms four feet wide, extending at places in all
directions, like the radiating cracks made in a rock by a light blast of
gunpowder. There are evidences of trees having been thrown violently
down, and a trustworthy gentleman declares that a huge oak was split
from root to top by the opening of a chasm under it. General Clingman
says:
“I observed a large poplar tree which had been split through its
center so as to leave one-half of it standing 30 or 40 feet high.
The crack or opening under it was not an inch wide, but could be
traced for hundreds of yards, making it evident that there had been
an opening wide enough to split the tree, and that then the sides
of the chasm had returned to their original position without having
split so as to prevent the contact of broken rocks.”
A great mass of granite was broken into fragments, and after one of
these shocks every loose stone and piece of wood was moved from its
original place. These jars, accompanied with noise, used to occur at
intervals of two or three years, but none have been felt for some time.
About the year 1829 occurred a violent earthquake, covering a limited
area, in Cherokee county. One of the Valley River mountains was cleft
open for several hundred yards, making a chasm which is still visible.
Silas McDowell, a careful observer, late of Macon county, stated, in a
paper, that there was a violent shock on the divide between Ellijay and
Cullasaja many years ago. A chasm opened in the north side of the
mountain, accompanied with crashing sounds. Satoola mountain, bounding
the Highlands plateau, it has been stated, has crevices from which smoke
issues at intervals.
Public-domain text, read in full here on John Shaqi.
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