The Blue-Grass Region of Kentucky, and Other Kentucky ArticlesAllen, James Lane
General
The Blue-Grass Region of Kentucky, and Other Kentucky Articles
Allen, James Lane
Kentucky -- Description and travel; Kentucky -- Social life and customs
This mountain pass not being in Kentucky, it might be asked why in a
series of articles on Kentucky it should deserve a place. The answer is
plain: not because a Kentuckian selected it as the site of a hoped for
city, or because Kentuckians have largely developed it, or because
Kentuckians largely own it, and have stamped upon it a certain excellent
social tone; but for the reason that if the idea of its development is
carried out, it will gather towards itself a vast net-work of railways
from eastern Kentucky, the Atlantic seaboard, the South, and the Ohio
and Mississippi valleys, which will profoundly affect the inner life of
Kentucky, and change its relations to different parts of the Union.
Big Stone Gap! It does not sound very big. What is it? At a certain
point of this continuation of Cumberland Mountain, called Stone
Mountain, the main fork of Powell's River has in the course of ages worn
itself a way down to a practical railroad pass at water-level, thus
opening connection between the coking coal on the north and the iron
ores on the south of the mountain. No pass that I have ever seen--except
those made by the Doe River in the Cranberry region of North
Carolina--has its wild, enrapturing loveliness; towering above on each
side are the mountain walls, ancient and gray and rudely disordered; at
every coign of vantage in these, grasping their precipitous buttresses
as the claw of a great eagle might grasp the uttermost brow of a cliff,
enormous trees above trees, and amid the trees a green lace-work of
undergrowth. Below, in a narrow, winding channel piled high with
bowlders, with jutting rocks and sluice-like fissures--below and against
these the river hurls itself, foaming, roaring, whirling, a long cascade
of white or lucent water. This is Big Stone Gap, and the valley into
which the river pours its full strong current is the site of the town. A
lofty valley it is, having an elevation of 1600 feet above the sea, with
mountains girdling it that rise to the height of 4000--a valley the
surface of which gently rolls and slopes towards these encircling bases
with constant relief to the eye, and spacious enough, with those opening
into it, to hold a city of the population of New York.
Public-domain text, read in full here on John Shaqi.
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