III.—On Drift
In a letter to Nature for 14th May, 1874, Mr. Belt has expressed his belief that the presence of shells in glacial deposits, at whatever elevation they may be found, does not necessarily constitute a proof that the land has been depressed to that extent relatively to the level of the sea; but that i...
| Published in: | Geological Magazine |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1874
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0016756800169808 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800169808 |
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crcambridgeupr:10.1017/s0016756800169808 |
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openpolar |
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crcambridgeupr:10.1017/s0016756800169808 2024-03-03T08:45:25+00:00 III.—On Drift Goodchild, J. G. 1874 http://dx.doi.org/10.1017/s0016756800169808 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800169808 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 1, issue 11, page 496-510 ISSN 0016-7568 1469-5081 Geology journal-article 1874 crcambridgeupr https://doi.org/10.1017/s0016756800169808 2024-02-08T08:30:58Z In a letter to Nature for 14th May, 1874, Mr. Belt has expressed his belief that the presence of shells in glacial deposits, at whatever elevation they may be found, does not necessarily constitute a proof that the land has been depressed to that extent relatively to the level of the sea; but that in such cases as those of the drifts of the basin of the Irish Sea the shells occur in their present positions because they were thrust thither out of the bed of the sea by the ice-sheet which was advancing from the North. Article in Journal/Newspaper Ice Sheet Cambridge University Press Geological Magazine 1 11 496 510 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
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English |
| topic |
Geology |
| spellingShingle |
Geology Goodchild, J. G. III.—On Drift |
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Geology |
| description |
In a letter to Nature for 14th May, 1874, Mr. Belt has expressed his belief that the presence of shells in glacial deposits, at whatever elevation they may be found, does not necessarily constitute a proof that the land has been depressed to that extent relatively to the level of the sea; but that in such cases as those of the drifts of the basin of the Irish Sea the shells occur in their present positions because they were thrust thither out of the bed of the sea by the ice-sheet which was advancing from the North. |
| format |
Article in Journal/Newspaper |
| author |
Goodchild, J. G. |
| author_facet |
Goodchild, J. G. |
| author_sort |
Goodchild, J. G. |
| title |
III.—On Drift |
| title_short |
III.—On Drift |
| title_full |
III.—On Drift |
| title_fullStr |
III.—On Drift |
| title_full_unstemmed |
III.—On Drift |
| title_sort |
iii.—on drift |
| publisher |
Cambridge University Press (CUP) |
| publishDate |
1874 |
| url |
http://dx.doi.org/10.1017/s0016756800169808 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800169808 |
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Ice Sheet |
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Ice Sheet |
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Geological Magazine volume 1, issue 11, page 496-510 ISSN 0016-7568 1469-5081 |
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https://www.cambridge.org/core/terms |
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https://doi.org/10.1017/s0016756800169808 |
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Geological Magazine |
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1 |
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11 |
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496 |
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510 |
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1792500980136280064 |