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
In several parts of the Arkansa territory we were shewn dollars, which
were believed to have been coined in some of the upper settlements of
White river; and it has been currently reported, that mines of silver
exist, and are wrought there. It appears, however, upon examination,
that much spurious coin is here in circulation; and it is probable that
the White river country owes its present reputation for mineral wealth
to the successful labours of some manufacturer of imitation dollars.
Since the time of De Soto, it has been confidently asserted by many
who have written concerning Louisiana, that mines of gold and silver
exist in that part of the country of which we are speaking. In an old
map, by Du Pratz, a gold mine is placed somewhere near the confluence
of the Illinois and the Arkansa; a silver mine on the Merameg, and he
says, "I myself saw a rivulet whose waters rolled down gold dust."[22]
We are informed by Schoolcraft, that granite exists about the sources
of the St. Francis, which are near those of White river.[23] Of the
extent and character of this formation of granite, we have not yet
been able to form any very definite ideas; it is, however, by no means
improbable, that to its plates of yellow and white mica, we are to
look for the origin of the fabulous accounts of the precious metals in
those regions. Like the country of the gilded king, the El Dorado of
South America, it is probable the gold and silver mines of the Arkansa
territory will recede, before the progress of examination, first into
the wildest and most inaccessible parts, and at length disappear
entirely. We by no means intend to assert, that the region in question
will not prove of immense importance, on account of its mineral
treasures; valuable mines of lead and iron are certainly frequent in
many parts of it. And we can assign no reason why silver {139} and
other metals should not be found in the argillite with quartzy veins,
and in the other rocks of the transition period, which we know to
exist in these mountains. We only intend to give it as our opinion,
that there has as yet been no foundation in actual discovery for the
belief that such mines do exist.
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