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....

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Published in:Geological Magazine
Main Author: Bulman, G. W.
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
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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
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