Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones
Abstract Attention is drawn to resemblances between two contrasted styles of mosaic crystallization—tessellate and equigranular as compared with irregularly interlocking (sutured) and inequigranular—that characterize ice in alpine glaciers and quartz in dynamically metamorphosed sandstones of the Mo...
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Language: | English |
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Cambridge University Press (CUP)
1951
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Online Access: | http://dx.doi.org/10.1017/s0022143000026289 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000026289 |
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crcambridgeupr:10.1017/s0022143000026289 2024-09-15T18:15:39+00:00 Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones MacGregor, A. G. 1951 http://dx.doi.org/10.1017/s0022143000026289 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000026289 en eng Cambridge University Press (CUP) Journal of Glaciology volume 1, issue 10, page 564-571 ISSN 0022-1430 1727-5652 journal-article 1951 crcambridgeupr https://doi.org/10.1017/s0022143000026289 2024-07-31T04:04:10Z Abstract Attention is drawn to resemblances between two contrasted styles of mosaic crystallization—tessellate and equigranular as compared with irregularly interlocking (sutured) and inequigranular—that characterize ice in alpine glaciers and quartz in dynamically metamorphosed sandstones of the Moinian area of the northern Scottish Highlands. It is suggested that in both environments the contrasted types of mosaic are due to crystallization under conditions of shearing stress that were respectively minimal and maximal. Similarities are also pointed out between the orientation of the principal crystallographic axes of crystals in ice subjected to shearing stress, and the “girdle” arrangement of the principal crystallographic axes of quartz in Moinian metamorphic sandstones. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 1 10 564 571 |
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Open Polar |
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Cambridge University Press |
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language |
English |
description |
Abstract Attention is drawn to resemblances between two contrasted styles of mosaic crystallization—tessellate and equigranular as compared with irregularly interlocking (sutured) and inequigranular—that characterize ice in alpine glaciers and quartz in dynamically metamorphosed sandstones of the Moinian area of the northern Scottish Highlands. It is suggested that in both environments the contrasted types of mosaic are due to crystallization under conditions of shearing stress that were respectively minimal and maximal. Similarities are also pointed out between the orientation of the principal crystallographic axes of crystals in ice subjected to shearing stress, and the “girdle” arrangement of the principal crystallographic axes of quartz in Moinian metamorphic sandstones. |
format |
Article in Journal/Newspaper |
author |
MacGregor, A. G. |
spellingShingle |
MacGregor, A. G. Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones |
author_facet |
MacGregor, A. G. |
author_sort |
MacGregor, A. G. |
title |
Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones |
title_short |
Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones |
title_full |
Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones |
title_fullStr |
Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones |
title_full_unstemmed |
Ice Crystals in Glaciers Compared with Quartz Crystals in Dynamically MetaMorphosed Sandstones |
title_sort |
ice crystals in glaciers compared with quartz crystals in dynamically metamorphosed sandstones |
publisher |
Cambridge University Press (CUP) |
publishDate |
1951 |
url |
http://dx.doi.org/10.1017/s0022143000026289 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000026289 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 1, issue 10, page 564-571 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000026289 |
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Journal of Glaciology |
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1 |
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10 |
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564 |
op_container_end_page |
571 |
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1810453583781429248 |