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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... "
Elements of Geology: Including Fossil Botany and Palaeontology : a Popular ... - หน้า 293
โดย John Lee Comstock - 1847 - 432 หน้า
มุมมองทั้งเล่ม - เกี่ยวกับหนังสือเล่มนี้

An Outline of Mineralogy and Geology,: Intended for the Use of Those who May ...

William Phillips - 1816 - 222 หน้า
...preservation as that their sharpest ridges are retained ; they are found in elevations far above the level of the ocean, and in places to which the sea could not be conveyed by any existing cause : they arc sometimes enclosed in loose sand, sometimes filled or...

The American Monthly Magazine and Critical Review, เล่มที่ 3

H. Biglow, Orville Luther Holley - 1818 - 500 หน้า
...and their finest and tenderest processes. They are found in elevations far above the level of evey part of the ocean, and in places to which the sea could not be conveyed by any existing cause. They are not only enclosed in loose sand, but are often incrusted...

A Dictionary of Chemistry: On the Basis of Mr. Nicholson's, in ..., เล่มที่ 2

Andrew Ure - 1821 - 512 หน้า
...sharpest ridges, and tenderest processes. They are found in elevations tar above the level of ever)- 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...

A Comparative Estimate of the Mineral and Mosaical Geologies

Granville Penn - 1822 - 480 หน้า
..." and their finest and tenderest processes. " They are found in elevations far above the PART in. " 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 en" closed in loose sand, but often incrusted...

The Christian Observer, เล่มที่ 23

1824 - 884 หน้า
...parts, their sharpest ridges, and 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...

The Christian observer [afterw.] The Christian observer and advocate

1824 - 890 หน้า
...their sharpest ridges, and 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...

A Comparative Estimate of the Mineral and Mosaical Geologies, เล่มที่ 2

Granville Penn - 1825 - 440 หน้า
...are almost 1 D'AUBUISSON, torn. ip 8. ' Ib. p. 252. CHAT. IV. MINERAL AND MOSAICAL GEOLOOIES. 47 " every where so completely preserved, that even " the...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...

A Dictionary of Chemistry ...

Andrew Ure - 1828 - 872 หน้า
...most delicate parts, their sharpest ridges, and tenderes! processes. They are found in elevations far above the level of every part of the ocean, and in places to which the sta could not be conveyed by any presently existing cause. They are not merely enclosed in loose sand,...

A Dictionary of Chemistry and Mineralogy: With Their Applications

Andrew Ure - 1831 - 980 หน้า
...most delicate parts, their 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...

Buffon's Natural history, corrected and enlarged by J. Wright. (To which are ...

Georges Louis Le Clerc (comte de Buffon.) - 1831 - 462 หน้า
...most delicate parts, their 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...




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