Scientific American Supplement, No. 433, April 19, 1884Various
Science
Scientific American Supplement, No. 433, April 19, 1884
Various
Science -- Periodicals
Topographically considered as a whole, the Cumberland range has its
southern terminus in Alabama, and its northern in Pennsylvania. It
is almost wholly composed of coal-bearing rocks, resting on Devonian
strata, which are visible in many places in the valleys.
But a small portion of the Cumberland lies above a plane of 2,000 feet.
Walden's Ridge and Lookout Mountain vary in height from 2,000 to 2,500
feet.
North of Grassy Cove, after the ridges are united, the variation from
2,000 feet is but little throughout the remainder of the State, and
the general character of the table changes but little. The great and
important difference is in the climate, the winters being much more
severe in these mountains in the northern part of the State than in the
southern, and the summers much more liable to sudden changes of weather.
Scott, Fentress, and Morgan counties comprise this portion of the table,
and these have not been included in my examination, excepting as to
general features.
In all our southern country, and I may say in our whole country, there
is no other large extent of elevated territory which offers mankind
a pleasant living place, a comfortable climate--none too cold or too
hot--and productive lands. We have east of the upper waters of the great
Tennessee River, in our State, and in North Carolina and Georgia, the
great Blue Ridge range of mountains, known as the Unaka, or Smoky,
Chilhowee, Great and Little Frog, Nantahala, etc., all belonging to the
same family of hills. This chain has the same general course as the
Cumberlands. It is a much bolder range of mountains, but it is vastly
less inhabitable, productive, or convenient of access. The winters there
are severely cold, and the nights in summer are too cold and damp for
health and comfort, as I know by personal experience of two summers on
Nantahala River. But the trout fishing is beyond comparison, and that
is one inducement of great value for a stout consumptive _who is a good
fellow_. These mountains are much more broken up into branches, peaks,
and spurs than the Cumberlands. They afford no table terrritory of
any extent. There are some excellent places there for hot summer
visits--Ashville, Warm Springs, Franklin, and others.
The Cumberland Mountains, as a whole, are flat, in broad level spaces,
broken only by the "divides," or "gulfs," as they are called by the
inhabitants, where the streams flow out into the valleys.
Public-domain text, read in full here on John Shaqi.
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