To the Editor of the Geological Magazine
are also some beds which may turn out to be altered limestones; a,nd then, this group is really an old mountain-chain, having an anticlinal line, which (if the beds had not been broken through and broken up at the same time) would have given a ridge of many thousand feet high.These features, I think...
保存先:
| 出版年: | Geological Magazine |
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| 第一著者: | |
| フォーマット: | 論文 |
| 言語: | 英語 |
| 出版事項: |
Cambridge University Press
1865
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| 主題: | |
| オンライン･アクセス: | https://doi.org/10.1017/s001675680016193x |
| タグ: |
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| 要約: | are also some beds which may turn out to be altered limestones; a,nd then, this group is really an old mountain-chain, having an anticlinal line, which (if the beds had not been broken through and broken up at the same time) would have given a ridge of many thousand feet high.These features, I think, distinguish this group of rocks from the Cambrians of Wales. |
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| DOI: | 10.1017/s001675680016193x |