Microstructure of impure ice.

By far the most common form of ice covering a body of water is "sheet ice". Wilson Zumberge and Marshall (1) have recently done a classification of lake ice and reported that two basic structures were found: i) a coarsely crystalline columnar aggregate, ii) a finely crystalline granular ag...

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Bibliographic Details
Main Author: Perey, Francis. G.
Other Authors: Pounder, E. (Supervisor)
Format: Thesis
Language:English
Published: McGill University 1957
Subjects:
Physics
Zumberge
Ice Sheet
Online Access:http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111273
id ftcanadathes:oai:collectionscanada.gc.ca:QMM.111273
record_format openpolar
spelling ftcanadathes:oai:collectionscanada.gc.ca:QMM.111273 2023-05-15T16:40:37+02:00 Microstructure of impure ice. Perey, Francis. G. Pounder, E. (Supervisor) Master of Science. (Department of Physics.) 1957 application/pdf http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111273 en eng McGill University alephsysno: NNNNNNNNN Theses scanned by McGill Library. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111273 All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated. Physics Electronic Thesis or Dissertation 1957 ftcanadathes 2014-02-16T00:53:25Z By far the most common form of ice covering a body of water is "sheet ice". Wilson Zumberge and Marshall (1) have recently done a classification of lake ice and reported that two basic structures were found: i) a coarsely crystalline columnar aggregate, ii) a finely crystalline granular aggregate. This crystalline granular aggregate is produced by the affects of heavy snow fall at the time of freeze-up or by snow fall on the ice surface which, by a process of wet and dry snow metamorphism, changes into the granular aggregate, forming a miner portion of the ice sheet. Thesis Ice Sheet Theses Canada/Thèses Canada (Library and Archives Canada) Zumberge ENVELOPE(-69.707,-69.707,-76.233,-76.233)
institution Open Polar
collection Theses Canada/Thèses Canada (Library and Archives Canada)
op_collection_id ftcanadathes
language English
topic Physics
spellingShingle Physics
Perey, Francis. G.
Microstructure of impure ice.
topic_facet Physics
description By far the most common form of ice covering a body of water is "sheet ice". Wilson Zumberge and Marshall (1) have recently done a classification of lake ice and reported that two basic structures were found: i) a coarsely crystalline columnar aggregate, ii) a finely crystalline granular aggregate. This crystalline granular aggregate is produced by the affects of heavy snow fall at the time of freeze-up or by snow fall on the ice surface which, by a process of wet and dry snow metamorphism, changes into the granular aggregate, forming a miner portion of the ice sheet.
author2 Pounder, E. (Supervisor)
format Thesis
author Perey, Francis. G.
author_facet Perey, Francis. G.
author_sort Perey, Francis. G.
title Microstructure of impure ice.
title_short Microstructure of impure ice.
title_full Microstructure of impure ice.
title_fullStr Microstructure of impure ice.
title_full_unstemmed Microstructure of impure ice.
title_sort microstructure of impure ice.
publisher McGill University
publishDate 1957
url http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111273
op_coverage Master of Science. (Department of Physics.)
long_lat ENVELOPE(-69.707,-69.707,-76.233,-76.233)
geographic Zumberge
geographic_facet Zumberge
genre Ice Sheet
genre_facet Ice Sheet
op_relation alephsysno: NNNNNNNNN
Theses scanned by McGill Library.
http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=111273
op_rights All items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
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