Note upon the origin of the phosphatic formation
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1869
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Abstract
CONCERNING the origin of this extensive formation, several explanations suggest themselves.Among these thl~ best answering the purpose at preRent is perhaps the supposition, that the great Carolina Eocene bed. of shell-marl on which it rests, formerly, and for a long period, protruded IIHtny feet above the present sea-level, giving rise to a luxUl'iant soil (analogous to that now existing over portion~ of some of the guano islands and shores) and which was then depressed beneath the sea, where it nnder-
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| Reference Key |
openalex_W2312822957
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|---|---|
| Authors | C. U. Shepard |
| Journal | american journal of science |
| Year | 1869 |
| DOI |
10.2475/ajs.s2-47.141.338
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| URL | |
| Keywords | Keywords not found |
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