V.—On the South of England Ice-Sheet

In the Reader , 14th October, 1865, and afterwards more fully in my papers on the “Boulder-clay of Caithness,” and on the “ Transport of the Wastdale Crag Blocks,” 2 the following were shown from physical considerations to be necessary results, viz.:— 1. That were the ice of Greenland much thicker t...

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Published in:Geological Magazine
Main Author: Croll, James
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1874
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800168037
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800168037
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spelling crcambridgeupr:10.1017/s0016756800168037 2024-03-03T08:44:59+00:00 V.—On the South of England Ice-Sheet Croll, James 1874 http://dx.doi.org/10.1017/s0016756800168037 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800168037 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 1, issue 6, page 257-257 ISSN 0016-7568 1469-5081 Geology journal-article 1874 crcambridgeupr https://doi.org/10.1017/s0016756800168037 2024-02-08T08:39:02Z In the Reader , 14th October, 1865, and afterwards more fully in my papers on the “Boulder-clay of Caithness,” and on the “ Transport of the Wastdale Crag Blocks,” 2 the following were shown from physical considerations to be necessary results, viz.:— 1. That were the ice of Greenland much thicker than it is at present, which it evidently was during the Glacial Epoch, it would not float in Davis Straits and Baffin's Bay, and consequently, would not break up into icebergs, but would move over upon the North American continent in one continuous mass, and pursue its course southwards, until it gradually melted away under the influence of the Sun's heat. Article in Journal/Newspaper Greenland Ice Sheet Cambridge University Press Greenland Geological Magazine 1 6 257 257
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Croll, James
V.—On the South of England Ice-Sheet
topic_facet Geology
description In the Reader , 14th October, 1865, and afterwards more fully in my papers on the “Boulder-clay of Caithness,” and on the “ Transport of the Wastdale Crag Blocks,” 2 the following were shown from physical considerations to be necessary results, viz.:— 1. That were the ice of Greenland much thicker than it is at present, which it evidently was during the Glacial Epoch, it would not float in Davis Straits and Baffin's Bay, and consequently, would not break up into icebergs, but would move over upon the North American continent in one continuous mass, and pursue its course southwards, until it gradually melted away under the influence of the Sun's heat.
format Article in Journal/Newspaper
author Croll, James
author_facet Croll, James
author_sort Croll, James
title V.—On the South of England Ice-Sheet
title_short V.—On the South of England Ice-Sheet
title_full V.—On the South of England Ice-Sheet
title_fullStr V.—On the South of England Ice-Sheet
title_full_unstemmed V.—On the South of England Ice-Sheet
title_sort v.—on the south of england ice-sheet
publisher Cambridge University Press (CUP)
publishDate 1874
url http://dx.doi.org/10.1017/s0016756800168037
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800168037
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source Geological Magazine
volume 1, issue 6, page 257-257
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800168037
container_title Geological Magazine
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container_issue 6
container_start_page 257
op_container_end_page 257
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