IV.—The “Great Submergence” Again: Clava, etc. Part II
Last month I glanced at some of the difficulties attaching to the theory of a “ great submergence ” during Glacial times, particularly in connection with the deposition of this shelly clay at Clava. In regard to the alternative theory of transport by land-ice, the following facts may be enumerated a...
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Cambridge University Press (CUP)
1897
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Online Access: | http://dx.doi.org/10.1017/s0016756800175156 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800175156 |
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crcambridgeupr:10.1017/s0016756800175156 2024-03-03T08:45:24+00:00 IV.—The “Great Submergence” Again: Clava, etc. Part II Bell, Dugald 1897 http://dx.doi.org/10.1017/s0016756800175156 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800175156 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 4, issue 2, page 63-68 ISSN 0016-7568 1469-5081 Geology journal-article 1897 crcambridgeupr https://doi.org/10.1017/s0016756800175156 2024-02-08T08:39:21Z Last month I glanced at some of the difficulties attaching to the theory of a “ great submergence ” during Glacial times, particularly in connection with the deposition of this shelly clay at Clava. In regard to the alternative theory of transport by land-ice, the following facts may be enumerated as so far in its favour:- (a) Evidences of ice-action are conspicuous all over the district. It is a region of intense glaciation, and this special locality is right in the tract of the ancient ice-sheet. (b) The traces of the movement show that, with a very small submergence, the ice-sheet must have passed over part of a former sea-bottom. (c) That in this neighbourhood it rose in its progress, carrying numerous boulders with it in its course, and leaving them at higher elevations than their parent beds of rock. Article in Journal/Newspaper Ice Sheet Cambridge University Press Geological Magazine 4 2 63 68 |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Bell, Dugald IV.—The “Great Submergence” Again: Clava, etc. Part II |
topic_facet |
Geology |
description |
Last month I glanced at some of the difficulties attaching to the theory of a “ great submergence ” during Glacial times, particularly in connection with the deposition of this shelly clay at Clava. In regard to the alternative theory of transport by land-ice, the following facts may be enumerated as so far in its favour:- (a) Evidences of ice-action are conspicuous all over the district. It is a region of intense glaciation, and this special locality is right in the tract of the ancient ice-sheet. (b) The traces of the movement show that, with a very small submergence, the ice-sheet must have passed over part of a former sea-bottom. (c) That in this neighbourhood it rose in its progress, carrying numerous boulders with it in its course, and leaving them at higher elevations than their parent beds of rock. |
format |
Article in Journal/Newspaper |
author |
Bell, Dugald |
author_facet |
Bell, Dugald |
author_sort |
Bell, Dugald |
title |
IV.—The “Great Submergence” Again: Clava, etc. Part II |
title_short |
IV.—The “Great Submergence” Again: Clava, etc. Part II |
title_full |
IV.—The “Great Submergence” Again: Clava, etc. Part II |
title_fullStr |
IV.—The “Great Submergence” Again: Clava, etc. Part II |
title_full_unstemmed |
IV.—The “Great Submergence” Again: Clava, etc. Part II |
title_sort |
iv.—the “great submergence” again: clava, etc. part ii |
publisher |
Cambridge University Press (CUP) |
publishDate |
1897 |
url |
http://dx.doi.org/10.1017/s0016756800175156 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800175156 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geological Magazine volume 4, issue 2, page 63-68 ISSN 0016-7568 1469-5081 |
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https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800175156 |
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Geological Magazine |
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4 |
container_issue |
2 |
container_start_page |
63 |
op_container_end_page |
68 |
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1792500963144105984 |