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
“Buck ague,” answered Ben Lester, quietly; and then the old and young
hunters, around that fireside, laughed uproariously.
The barking of the hounds, like my pace, stopped for a moment at the
report of Kenswick’s gun. Ten minutes after, I was on the Long rock on
the bank of the Little Tennessee. This stand merits a description, for
from it probably more deer have been killed than at any other single
point in the mountains of Western North Carolina. It is at the Narrows.
Here, in the narrowest channel of its course, from below where it begins
to merit the name of a river, this stream, of an average width of 150
yards, pours the whole drainage of the counties of Swain, Jackson,
Macon, one-half of Graham and a small portion of Northern Georgia,
between banks eighty-five feet apart. The waters are those of the rivers
Tuckasege, Cullasaja, Nantihala, Ocona Lufta, and the large creeks Soco,
Scott’s, Caney Fork, Stecoah, Forney, and Hazel, heading in the
cross-chains of the Balsam, Cowee, Nantihala, and Valley River
mountains, and on the southern slope of the Great Smoky.
For 100 yards the stream shoots along like a mill-race. Brown boulders,
the size of horses, coaches and cabins, are piled at the edges of the
current. At the entrance to the Narrows, a line of rocks forms a broken
fall of several feet. Over it the waters are white, and the trees wet
with spray. Above its roar, no rifle shot, or hound’s bay can be heard a
few feet away. Long rock is a dark boulder projecting into the river,
at its very narrowest point, 100 yards below, and in full sight of the
white rapids. The hunter leaves the road, jumps and clambers over a
succession of immense boulders, and at length seats himself on Long
rock. The water, close at its edge, is forty feet deep. A steep
mountain, following the river round every bend, showing square, mossed
rocks under the heavy autumn-tinted forests on its front, rises close
along the river’s opposite edge. A few sand-bars, below the stand, reach
out from the mountain’s foot. There is one narrow band of sandy bank
directly opposite the stand. Projecting boulders shield it from the rush
of waters. On this sandy bank the deer, if frightened when swimming down
mid-stream, will climb out, affording just the shot desired by the
hunter. If not frightened, they will pass on to the smooth-water
sand-bars below, and then, leaving the water, disappear up the mountain.
The drive-way, for which Long rock is a stand, comes down to the river a
few yards above the fall described. There are no rapids on the
Tennessee, but what can be swum by the deer. In many instances, to cool
his body and baffle the hounds, he keeps the center of the stream for a
mile or more, sometimes stopping in the water for hours before resuming
his course. The hounds, when the deer is in sight, follow him in the
water, and generally succeed in drowning him before he reaches the bank.
Public-domain text, read in full here on John Shaqi.
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