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" ... processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any existing cause. They are not only inclosed in loose sand, but are often incrusted and penetrated on... "
An Outline of Mineralogy and Geology,: Intended for the Use of Those who May ... - Page 72
by William Phillips - 1816 - 192 pages
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The Cyclopædia, Or, Universal Dictionary of Arts, Sciences, and ..., Volume 34

Abraham Rees - 1819 - 754 pages
...fmaUeft retain their mod delicate parts, their (harpeft ridges, and their fioeft and tendereft procefles. They are found in elevations far above the level of the ocean, and in places where the fea could not be conveyed by any exitting caufe. They are not only included in loofe fand,...
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A Dictionary of Chemistry, on the Basis of Mr. Nicholson's: In ..., Volume 2

Andrew Ure - 1821 - 418 pages
...sharpest ridges, and tenderest processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any presently existing cause. They are not merely enclosed in loose sand, but are often increased and penetrated...
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The Christian observer [afterw.] The Christian observer and advocate

1824 - 890 pages
...their finest and t ruderest processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any existing cause. They are not only inclosed in loose sand, but are often incrusted and penetrated on all sides by the hardest...
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The Christian Observer, Volume 23

1824 - 884 pages
...their finest and tenderest processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any existing cause. They are not only inclosed in loose sand, but are often incrusted and penetrated on all sides by the hardest...
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A Comparative Estimate of the Mineral and Mosaical Geologies, Volume 2

Granville Penn - 1825 - 440 pages
...processes, and their " finest points. They are found in elevations " above the level of every part of the ocean, and in " places to which the sea could not now be con" veyed by any existing causes. They are not " only enveloped in loose sands, but are incrusted...
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Buffon's Natural history, corrected and enlarged by J. Wright. (To which are ...

Georges Louis Le Clerc (comte de Buffon.) - 1831 - 462 pages
...sharpest ridges, and tenderest processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any previously existing cause. They are not merely enclosed in loose sand, but are often incrusted and...
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A Dictionary of Chemistry and Mineralogy: With Their Applications

Andrew Ure - 1831 - 980 pages
...sharpest ridges, and tenderest processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any presently existing cause. They are not merely enclosed in loose sand, but are often incrusted and penetrated...
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The British Critic, Quarterly Theological Review, and ..., Volume 12

1832 - 528 pages
...their finest and tenderest processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any existing cause. They are not only inclosed in loose sand, but are often encrusted and penetrated on all sides by the hardest...
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Leigh Hunt's London Journal, Volumes 1-2

Leigh Hunt - 1834 - 680 pages
...their finest and tenderest processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sea could not be conveyed by any existing cause. They are not only inclosed in loose sand, but are often incrusted and penetrated on all sides by the hardest...
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Outlines of Geology: Intended as a Popular Treatise on the Most Interesting ...

John Lee Comstock - 1836 - 396 pages
...slenderest processes, and their finest points. They are found in elevations, above the level of every part of the ocean, and in places to which the sea could not now be conveyed by any existing causes. They are not only enveloped in loose sands, but are encrusted...
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