Travels in North America, From Modern Writers: With Remarks and Observations; Exhibiting a Connected View of the Geography and Present State of that Quarter of the GlobeBingley, William
History
Travels in North America, From Modern Writers: With Remarks and Observations; Exhibiting a Connected View of the Geography and Present State of that Quarter of the Globe
Bingley, William
Canada -- Description and travel; Mexico -- Description and travel; United States -- Description and travel
Geographical writers have divided the United States into three regions:
the _lowlands_ or flat country; the highlands, and the mountains. Of
these, the first extend from the Atlantic ocean to the falls of the
great rivers. The _highlands_ reach from the falls to the foot of the
mountains; and the _mountains_ stretch nearly through the whole country,
in a direction from south-west to north-east. Their length is about 900
miles, and their breadth from 60 to 200. They may be considered as
separated into two distinct chains; of which the eastern chain has the
name of _Blue Mountains_, and the western is known, at its southern
extremity, by the name of _Cumberland_ and _Gauley Mountains_, and
afterwards by that of the _Alleghany Mountains_. The Alleghanies are
about 250 miles distant from the shore of the Atlantic. Towards the
north there are other eminences, called the _Green Mountains_ and the
_White Mountains_. The loftiest summits of the whole are said to be
about 7000 feet in perpendicular height above the level of the sea.
Few countries can boast a greater general fertility of _soil_ than North
America. The soil of the higher lands consists, for the most part, of a
brown loamy earth, and a yellowish sandy clay. Marine shells, and other
substances, in a fossil state, are found at the depth of eighteen or
twenty feet below the surface of the ground. Some of these are of very
extraordinary description. In the year 1712, several bones and teeth of
a vast nondescript quadruped, were dug up at Albany in the state of New
York. By the ignorant inhabitants these were considered to be the
remains of gigantic human bodies. In 1799 the bones of other individuals
of this animal, which has since been denominated the _Mastodon_ or
_American Mammoth_, were discovered beneath the surface of the ground,
in the vicinity of Newburgh, on the river Hudson. Induced by the hope of
being able to obtain a perfect skeleton, a Mr. Peale, of Philadelphia,
purchased these bones, with the right of digging for others. He was
indefatigable in his exertions, but was unable, for some time, to
procure any more. He made an attempt in a morass about twelve miles
distant from Newburgh, where an entire set of ribs was found, but
unaccompanied by any other remains. In another morass, in Ulster county,
he found several bones; among the rest a complete under jaw, and upper
part of the head. From the whole of the fragments that he obtained, he
was enabled to form two skeletons. One of these, under the name of
mammoth, was exhibited in London, about a year afterwards. Its height at
the shoulder was eleven feet; its whole length was fifteen feet; and its
weight about one thousand pounds. This skeleton was furnished with large
and curved ivory tusks, different in shape from those of an elephant,
but similar in quality. In 1817 another skeleton was dug up, from the
depth of only four feet, in the town of _Goshen_, near Chester. The
tusks of this were more than nine feet in length.
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