On the unity of geological phenomena in the solar system
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Abstract
This depth is deduced from the comparison oC the relative areas oC land and water which are taken as 1: 3, the elevation and depression oC the surface being assumed as proportional to the square roots of their surfaces.(Saigey, Physique du
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| Reference Key |
openalex_W2316388050
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|---|---|
| Authors | L. Saemann |
| Journal | american journal of science |
| Year | 1862 |
| DOI |
10.2475/ajs.s2-33.97.36
|
| URL | |
| Keywords | Keywords not found |
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