VII.—Glacier Lake Channels
In 1902 I published a paper, the outcome of several years' observation, on certain phenomena associated with the glacial deposits of the Cleveland area, which I attributed to the former presence of a series of temporary lakes and lakelets upheld in the recesses of the hills by the margin of a g...
Published in: | Geological Magazine |
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Language: | English |
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Cambridge University Press (CUP)
1916
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Online Access: | http://dx.doi.org/10.1017/s0016756800190909 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800190909 |
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crcambridgeupr:10.1017/s0016756800190909 2024-03-03T08:45:26+00:00 VII.—Glacier Lake Channels Kendall, Percy Fry 1916 http://dx.doi.org/10.1017/s0016756800190909 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800190909 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 3, issue 1, page 26-29 ISSN 0016-7568 1469-5081 Geology journal-article 1916 crcambridgeupr https://doi.org/10.1017/s0016756800190909 2024-02-08T08:32:02Z In 1902 I published a paper, the outcome of several years' observation, on certain phenomena associated with the glacial deposits of the Cleveland area, which I attributed to the former presence of a series of temporary lakes and lakelets upheld in the recesses of the hills by the margin of a great ice-sheet occupying the greater part of the North Sea. This interpretation met with so wide an acceptance, even by those geologists familiar with the district who had previously attributed the glacial deposits to a marine origin, that during the succeeding thirteen years I have steadfastly refrained from replying to criticism, hoping by this abstention to keep the issues unclouded by a controversy that might at any stage develop an acerbity not always lacking in earlier discussions. Article in Journal/Newspaper Ice Sheet Cambridge University Press Geological Magazine 3 1 26 29 |
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Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Kendall, Percy Fry VII.—Glacier Lake Channels |
topic_facet |
Geology |
description |
In 1902 I published a paper, the outcome of several years' observation, on certain phenomena associated with the glacial deposits of the Cleveland area, which I attributed to the former presence of a series of temporary lakes and lakelets upheld in the recesses of the hills by the margin of a great ice-sheet occupying the greater part of the North Sea. This interpretation met with so wide an acceptance, even by those geologists familiar with the district who had previously attributed the glacial deposits to a marine origin, that during the succeeding thirteen years I have steadfastly refrained from replying to criticism, hoping by this abstention to keep the issues unclouded by a controversy that might at any stage develop an acerbity not always lacking in earlier discussions. |
format |
Article in Journal/Newspaper |
author |
Kendall, Percy Fry |
author_facet |
Kendall, Percy Fry |
author_sort |
Kendall, Percy Fry |
title |
VII.—Glacier Lake Channels |
title_short |
VII.—Glacier Lake Channels |
title_full |
VII.—Glacier Lake Channels |
title_fullStr |
VII.—Glacier Lake Channels |
title_full_unstemmed |
VII.—Glacier Lake Channels |
title_sort |
vii.—glacier lake channels |
publisher |
Cambridge University Press (CUP) |
publishDate |
1916 |
url |
http://dx.doi.org/10.1017/s0016756800190909 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800190909 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geological Magazine volume 3, issue 1, page 26-29 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800190909 |
container_title |
Geological Magazine |
container_volume |
3 |
container_issue |
1 |
container_start_page |
26 |
op_container_end_page |
29 |
_version_ |
1792500990612602880 |