Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica
Summary The weathering of a suite of basalt clasts, that have been transported by mass wasting downslope in the Cumulus Hills region of the Queen Maud Mountains, Antarctica, is examined from both geochemical and glacio-geomorphic viewpoints. Chemical weathering, predominantly oxidation and hydration...
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Cambridge University Press (CUP)
1982
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Online Access: | http://dx.doi.org/10.1017/s0016756800027047 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800027047 |
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crcambridgeupr:10.1017/s0016756800027047 2024-09-09T19:03:07+00:00 Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica Talkington, R. W. Mayewski, P. A. Gaudette, H. E. 1982 http://dx.doi.org/10.1017/s0016756800027047 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800027047 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 119, issue 6, page 553-566 ISSN 0016-7568 1469-5081 journal-article 1982 crcambridgeupr https://doi.org/10.1017/s0016756800027047 2024-06-19T04:04:31Z Summary The weathering of a suite of basalt clasts, that have been transported by mass wasting downslope in the Cumulus Hills region of the Queen Maud Mountains, Antarctica, is examined from both geochemical and glacio-geomorphic viewpoints. Chemical weathering, predominantly oxidation and hydration, increases in severity from clast core to rim for the suite. These weathering processes and concomitant formation of a weathering rind are suggested to be an accumulative process, culminating in the disaggregation of the rock due in part both to the chemical breakdown of the interstitial and intersertal basaltic glass and to physical weathering processes. Mass wasting rates in the range of 1.4 × 10 −3 −1.13 × 10 −1 cm. y −1 are estimated, assuming that the style of transport is dry creep. These transport rates suggest that the rock-surface/air-temperature differences in the study area may have been as little as 0.5 °C and heating and cooling cycles as few as 1 cy. y −1 for the last 4.2 Ma. Article in Journal/Newspaper Antarc* Antarctica Cambridge University Press Cumulus Hills ENVELOPE(-175.000,-175.000,-85.333,-85.333) Geological Magazine 119 6 553 566 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Summary The weathering of a suite of basalt clasts, that have been transported by mass wasting downslope in the Cumulus Hills region of the Queen Maud Mountains, Antarctica, is examined from both geochemical and glacio-geomorphic viewpoints. Chemical weathering, predominantly oxidation and hydration, increases in severity from clast core to rim for the suite. These weathering processes and concomitant formation of a weathering rind are suggested to be an accumulative process, culminating in the disaggregation of the rock due in part both to the chemical breakdown of the interstitial and intersertal basaltic glass and to physical weathering processes. Mass wasting rates in the range of 1.4 × 10 −3 −1.13 × 10 −1 cm. y −1 are estimated, assuming that the style of transport is dry creep. These transport rates suggest that the rock-surface/air-temperature differences in the study area may have been as little as 0.5 °C and heating and cooling cycles as few as 1 cy. y −1 for the last 4.2 Ma. |
format |
Article in Journal/Newspaper |
author |
Talkington, R. W. Mayewski, P. A. Gaudette, H. E. |
spellingShingle |
Talkington, R. W. Mayewski, P. A. Gaudette, H. E. Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica |
author_facet |
Talkington, R. W. Mayewski, P. A. Gaudette, H. E. |
author_sort |
Talkington, R. W. |
title |
Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica |
title_short |
Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica |
title_full |
Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica |
title_fullStr |
Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica |
title_full_unstemmed |
Geochemical and glacio-geomorphic implications of basalt weathering in the Queen Maud Mountains, Antarctica |
title_sort |
geochemical and glacio-geomorphic implications of basalt weathering in the queen maud mountains, antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
1982 |
url |
http://dx.doi.org/10.1017/s0016756800027047 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800027047 |
long_lat |
ENVELOPE(-175.000,-175.000,-85.333,-85.333) |
geographic |
Cumulus Hills |
geographic_facet |
Cumulus Hills |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
Geological Magazine volume 119, issue 6, page 553-566 ISSN 0016-7568 1469-5081 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0016756800027047 |
container_title |
Geological Magazine |
container_volume |
119 |
container_issue |
6 |
container_start_page |
553 |
op_container_end_page |
566 |
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1809817139809353728 |