James's Account of S. H. Long's Expedition, 1819-1820, part 4James, Edwin
History
James's Account of S. H. Long's Expedition, 1819-1820, part 4
James, Edwin
Indians of North America; Rocky Mountains; United States -- Discovery and exploration; West (U.S.) -- Description and travel
These concussions are felt through a great extent of country, from the
settlements on Red river and the Washita to the falls of Ohio, and from
the mouth of the Missouri to New Orleans. Their great extent, and the
very considerable degree of violence with which they affect not only
a large portion of the valley of the Mississippi, but of the adjacent
hilly and mountainous country, appear to us most clearly to indicate
that they are produced by causes far more efficient and deep-seated
than "the decomposition of beds of lignite or wood-coal situated
near the level of the river, and filled with pyrites," according to
the suggestion of Mr. Nuttall.[76] It has been repeatedly asserted,
that volcanic appearances exist in the mountainous country between
Cape Girardeau and the hot springs of the Washita, particularly
at the latter place; but our observation has not tended to confirm
these accounts; and Hunter and Dunbar, who spent some time at the hot
springs, confidently deny the existence of any such appearances in
that quarter. Reports have been often circulated, principally on the
authority of hunters, of explosions, subterraneous fires, blowings and
bellowings of the mountains, and many other singular phenomena, said
to exist on the Little Missouri of Washita, and other parts of the
region of the hot springs; but it is easy to see that the combustion
of a coal-bed, or some other affair of equal insignificance, may have
afforded all the foundation on which these reports ever rested. But
though no traces of existing or of extinct volcanoes should be found
in any part of the country affected by these earthquakes, it is not
therefore necessary to go in search of some cause unlike those which in
{186} other parts of the earth are believed to produce similar effects.
On the morning following the earthquake above mentioned, a fall of snow
commenced, and continued during the day; towards evening it fell mixed
with hail and rain, and covered the ground to the depth of about six
inches.
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