A note on biological weathering on nunataks of the juneau icefield, Alaska
Abstract Observations on a number of nunataks of the Juneau Icefield indicate that chasmolithic algae play a major role in the breakdown of granitic rock. Expansion and contraction of the algal mucilage, caused by wetting and drying episodes, results in the surface flaking of the rock. Available dat...
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Language: | English |
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crwiley:10.1002/ppp.3430010209 2024-09-15T18:30:16+00:00 A note on biological weathering on nunataks of the juneau icefield, Alaska Hall, Kevin Otte, Wulf 1990 http://dx.doi.org/10.1002/ppp.3430010209 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430010209 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430010209 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 1, issue 2, page 189-196 ISSN 1045-6740 1099-1530 journal-article 1990 crwiley https://doi.org/10.1002/ppp.3430010209 2024-07-25T04:22:04Z Abstract Observations on a number of nunataks of the Juneau Icefield indicate that chasmolithic algae play a major role in the breakdown of granitic rock. Expansion and contraction of the algal mucilage, caused by wetting and drying episodes, results in the surface flaking of the rock. Available data suggest that the average mass of material lost per year from 1 m 2 of rock could be as high as 562 g. It is suggested that biological weathering may be a major destructive mechanism of the granitic lithologies. Article in Journal/Newspaper Permafrost and Periglacial Processes Alaska Wiley Online Library Permafrost and Periglacial Processes 1 2 189 196 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Observations on a number of nunataks of the Juneau Icefield indicate that chasmolithic algae play a major role in the breakdown of granitic rock. Expansion and contraction of the algal mucilage, caused by wetting and drying episodes, results in the surface flaking of the rock. Available data suggest that the average mass of material lost per year from 1 m 2 of rock could be as high as 562 g. It is suggested that biological weathering may be a major destructive mechanism of the granitic lithologies. |
format |
Article in Journal/Newspaper |
author |
Hall, Kevin Otte, Wulf |
spellingShingle |
Hall, Kevin Otte, Wulf A note on biological weathering on nunataks of the juneau icefield, Alaska |
author_facet |
Hall, Kevin Otte, Wulf |
author_sort |
Hall, Kevin |
title |
A note on biological weathering on nunataks of the juneau icefield, Alaska |
title_short |
A note on biological weathering on nunataks of the juneau icefield, Alaska |
title_full |
A note on biological weathering on nunataks of the juneau icefield, Alaska |
title_fullStr |
A note on biological weathering on nunataks of the juneau icefield, Alaska |
title_full_unstemmed |
A note on biological weathering on nunataks of the juneau icefield, Alaska |
title_sort |
note on biological weathering on nunataks of the juneau icefield, alaska |
publisher |
Wiley |
publishDate |
1990 |
url |
http://dx.doi.org/10.1002/ppp.3430010209 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.3430010209 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.3430010209 |
genre |
Permafrost and Periglacial Processes Alaska |
genre_facet |
Permafrost and Periglacial Processes Alaska |
op_source |
Permafrost and Periglacial Processes volume 1, issue 2, page 189-196 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.3430010209 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
1 |
container_issue |
2 |
container_start_page |
189 |
op_container_end_page |
196 |
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1810471732751892480 |