Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico
Abstract Neoglacial to historic and recent fluctuations of the firn field and one glacier on Popocatépetl, Mexico, include advance prior to 1519 to possible mid-Neoglaciation stadial position on gentle, north flanks at 4 150 m, then retreat up-valley to 4 335 m by 1906, and to 4 435 m by 1920 at 7 m...
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Cambridge University Press (CUP)
1981
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Online Access: | http://dx.doi.org/10.1017/s0022143000015434 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015434 |
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crcambridgeupr:10.1017/s0022143000015434 2024-03-03T08:46:09+00:00 Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico White, Sidney E. 1981 http://dx.doi.org/10.1017/s0022143000015434 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015434 en eng Cambridge University Press (CUP) Journal of Glaciology volume 27, issue 96, page 359-363 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1981 crcambridgeupr https://doi.org/10.1017/s0022143000015434 2024-02-08T08:40:23Z Abstract Neoglacial to historic and recent fluctuations of the firn field and one glacier on Popocatépetl, Mexico, include advance prior to 1519 to possible mid-Neoglaciation stadial position on gentle, north flanks at 4 150 m, then retreat up-valley to 4 335 m by 1906, and to 4 435 m by 1920 at 7 m/year. After volcanic eruptions and melting to about 4 800 m in 1921, growth of firn field and advance of a thin ice lobe before 1949 to 4 573 m by 1950, then retreat in next eight years at about 34 m/year, re-advance of the firn edge as an ice bulge to about 4 700 m by 1968, and as a thick double-lobed glacier to about 4 600 m by 1978 and 1979. A 37 year crevasse study shows continuous active firn-field movement on the north-west side of the cone. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 27 96 359 363 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes White, Sidney E. Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico |
topic_facet |
Earth-Surface Processes |
description |
Abstract Neoglacial to historic and recent fluctuations of the firn field and one glacier on Popocatépetl, Mexico, include advance prior to 1519 to possible mid-Neoglaciation stadial position on gentle, north flanks at 4 150 m, then retreat up-valley to 4 335 m by 1906, and to 4 435 m by 1920 at 7 m/year. After volcanic eruptions and melting to about 4 800 m in 1921, growth of firn field and advance of a thin ice lobe before 1949 to 4 573 m by 1950, then retreat in next eight years at about 34 m/year, re-advance of the firn edge as an ice bulge to about 4 700 m by 1968, and as a thick double-lobed glacier to about 4 600 m by 1978 and 1979. A 37 year crevasse study shows continuous active firn-field movement on the north-west side of the cone. |
format |
Article in Journal/Newspaper |
author |
White, Sidney E. |
author_facet |
White, Sidney E. |
author_sort |
White, Sidney E. |
title |
Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico |
title_short |
Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico |
title_full |
Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico |
title_fullStr |
Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico |
title_full_unstemmed |
Neoglacial to Recent Glacier Fluctuations on the Volcano Popocatépetl, Mexico |
title_sort |
neoglacial to recent glacier fluctuations on the volcano popocatépetl, mexico |
publisher |
Cambridge University Press (CUP) |
publishDate |
1981 |
url |
http://dx.doi.org/10.1017/s0022143000015434 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015434 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 27, issue 96, page 359-363 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000015434 |
container_title |
Journal of Glaciology |
container_volume |
27 |
container_issue |
96 |
container_start_page |
359 |
op_container_end_page |
363 |
_version_ |
1792502131939344384 |