II.—Ice and Ice-Work in Newfoundland
Aspect of Newfoundland .—It has been suggested that the so-called glacial effects which are universally seen in temperate, and even in tropical regions, may in many cases have been due to an ocean on which great icebergs floated. These, as they moved from point to point (like huge pepper-castors), s...
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Language: | English |
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Cambridge University Press (CUP)
1876
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Online Access: | http://dx.doi.org/10.1017/s0016756800154986 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800154986 |
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crcambridgeupr:10.1017/s0016756800154986 2024-03-03T08:46:40+00:00 II.—Ice and Ice-Work in Newfoundland Milne, John 1876 http://dx.doi.org/10.1017/s0016756800154986 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800154986 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 3, issue 8, page 345-350 ISSN 0016-7568 1469-5081 Geology journal-article 1876 crcambridgeupr https://doi.org/10.1017/s0016756800154986 2024-02-08T08:48:41Z Aspect of Newfoundland .—It has been suggested that the so-called glacial effects which are universally seen in temperate, and even in tropical regions, may in many cases have been due to an ocean on which great icebergs floated. These, as they moved from point to point (like huge pepper-castors), strewed broadcast boulders and detrital matter, such as are now to be seen over an area like that of Russia and parts of North America. The effect of the force of impact of these tremendous masses has also been dwelt on, and the way in which they could grind, smooth down, or rub up the surface of a submerged area, has also often been referred to. Article in Journal/Newspaper Newfoundland Cambridge University Press Geological Magazine 3 8 345 350 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Milne, John II.—Ice and Ice-Work in Newfoundland |
topic_facet |
Geology |
description |
Aspect of Newfoundland .—It has been suggested that the so-called glacial effects which are universally seen in temperate, and even in tropical regions, may in many cases have been due to an ocean on which great icebergs floated. These, as they moved from point to point (like huge pepper-castors), strewed broadcast boulders and detrital matter, such as are now to be seen over an area like that of Russia and parts of North America. The effect of the force of impact of these tremendous masses has also been dwelt on, and the way in which they could grind, smooth down, or rub up the surface of a submerged area, has also often been referred to. |
format |
Article in Journal/Newspaper |
author |
Milne, John |
author_facet |
Milne, John |
author_sort |
Milne, John |
title |
II.—Ice and Ice-Work in Newfoundland |
title_short |
II.—Ice and Ice-Work in Newfoundland |
title_full |
II.—Ice and Ice-Work in Newfoundland |
title_fullStr |
II.—Ice and Ice-Work in Newfoundland |
title_full_unstemmed |
II.—Ice and Ice-Work in Newfoundland |
title_sort |
ii.—ice and ice-work in newfoundland |
publisher |
Cambridge University Press (CUP) |
publishDate |
1876 |
url |
http://dx.doi.org/10.1017/s0016756800154986 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800154986 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Geological Magazine volume 3, issue 8, page 345-350 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800154986 |
container_title |
Geological Magazine |
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3 |
container_issue |
8 |
container_start_page |
345 |
op_container_end_page |
350 |
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1792502727086964736 |