On Taconic rocks and stratigraphy, with a geological map of the Taconic region
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Abstract
This southwestward direction is probably a consequence of the fact, already stated, that an Archrean area exists to the south and southeast in the hilly region of Sharon, Cornwall and Kent, which was a resisting mass when the uplifts and flexures of the later rocks took place.
| Reference Key |
openalex_W2332217313
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|---|---|
| Authors | J. D. Dana |
| Journal | american journal of science |
| Year | 1885 |
| DOI |
10.2475/ajs.s3-29.171.205
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| URL | |
| Keywords | Keywords not found |
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