IV.—Was the Boulder-clay formed Beneath the Ice?
Geological opinion is still divided on the subject of the formation of the Boulder-clay. By some it is held to be the sole work of the ice, and accumulated beneath it; by others it is looked upon as a marine deposit, though deriving its materials from the grinding action of the ice-sheet or glacier....
Published in: | Geological Magazine |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1892
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0016756800145807 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800145807 |
id |
crcambridgeupr:10.1017/s0016756800145807 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0016756800145807 2024-03-03T08:45:25+00:00 IV.—Was the Boulder-clay formed Beneath the Ice? Bulman, G. W. 1892 http://dx.doi.org/10.1017/s0016756800145807 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800145807 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 9, issue 7, page 305-310 ISSN 0016-7568 1469-5081 Geology journal-article 1892 crcambridgeupr https://doi.org/10.1017/s0016756800145807 2024-02-08T08:41:38Z Geological opinion is still divided on the subject of the formation of the Boulder-clay. By some it is held to be the sole work of the ice, and accumulated beneath it; by others it is looked upon as a marine deposit, though deriving its materials from the grinding action of the ice-sheet or glacier. Some geologists, again, hold that the “Till”—as distinct from the Boulder-clay— was formed beneath the ice, but that the latter is a marine deposit laid down in glacial seas. Article in Journal/Newspaper Ice Sheet Cambridge University Press Geological Magazine 9 7 305 310 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Geology |
spellingShingle |
Geology Bulman, G. W. IV.—Was the Boulder-clay formed Beneath the Ice? |
topic_facet |
Geology |
description |
Geological opinion is still divided on the subject of the formation of the Boulder-clay. By some it is held to be the sole work of the ice, and accumulated beneath it; by others it is looked upon as a marine deposit, though deriving its materials from the grinding action of the ice-sheet or glacier. Some geologists, again, hold that the “Till”—as distinct from the Boulder-clay— was formed beneath the ice, but that the latter is a marine deposit laid down in glacial seas. |
format |
Article in Journal/Newspaper |
author |
Bulman, G. W. |
author_facet |
Bulman, G. W. |
author_sort |
Bulman, G. W. |
title |
IV.—Was the Boulder-clay formed Beneath the Ice? |
title_short |
IV.—Was the Boulder-clay formed Beneath the Ice? |
title_full |
IV.—Was the Boulder-clay formed Beneath the Ice? |
title_fullStr |
IV.—Was the Boulder-clay formed Beneath the Ice? |
title_full_unstemmed |
IV.—Was the Boulder-clay formed Beneath the Ice? |
title_sort |
iv.—was the boulder-clay formed beneath the ice? |
publisher |
Cambridge University Press (CUP) |
publishDate |
1892 |
url |
http://dx.doi.org/10.1017/s0016756800145807 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800145807 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geological Magazine volume 9, issue 7, page 305-310 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800145807 |
container_title |
Geological Magazine |
container_volume |
9 |
container_issue |
7 |
container_start_page |
305 |
op_container_end_page |
310 |
_version_ |
1792500980330266624 |