Cave Regions of the Ozarks and Black Hills by Luella Agnes Owen
page 21 of 173 (12%)
page 21 of 173 (12%)
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In several other counties the pine is equally good, and other valuable timber everywhere abundant, although in a school geography published in 1838, the following descriptions of this region occur: "The lowlands of the Mississippi are bounded by the region of the Ozark Mountains. With the exception of the alluvial tracts on the borders of the streams, it is extremely hilly and broken. The mountains rise from eight hundred to eighteen hundred feet above the streams, with rounded summits and often perpendicular cliffs, and have a rocky surface, which admits only a scanty growth of timber." * * "Missouri is generally a region of prairies and table lands, much of which, as already described, is almost destitute of timber and water. It is crossed by the Ozark Mountains, which form a rugged tract of considerable extent. Earthquakes are not infrequent in some parts of this state. The soil is not generally productive." A comparison of these curious views with the latest official reports is highly amusing, as well as suggestive that early impressions are liable to require modification. In addition to the wonderful springs of pure water, there are numerous fine mineral springs, among which are a number of Epsom salt springs. At Jacksonville, in Randolph County, there is a large mineral spring from which it is said an over-heated horse may drink all he will without injury. Epsom-salts, or Epsomite, frequently occurs, as does the Niter, in a crystalline form of the pure mineral, as an efflorescence on rocks in many of the caves and in other sheltered positions. |
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