Mechanical weathering rates on Signy Island, maritime Antarctic
By means of re‐evaluating a number of properties of rock tablets left in the field for varying time periods, an estimation of rock breakdown rates is attained. From data obtained during the last five years, it would appear that rates are very slow, only of the order of 2% mass loss per 100 years. Th...
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Online Access: | http://nora.nerc.ac.uk/id/eprint/520404/ https://doi.org/10.1002/ppp.3430010108 |
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ftnerc:oai:nora.nerc.ac.uk:520404 2023-05-15T13:49:35+02:00 Mechanical weathering rates on Signy Island, maritime Antarctic Hall, Kevin 1990 http://nora.nerc.ac.uk/id/eprint/520404/ https://doi.org/10.1002/ppp.3430010108 unknown Wiley Hall, Kevin. 1990 Mechanical weathering rates on Signy Island, maritime Antarctic. Permafrost and Periglacial Processes, 1 (1). 61-67. https://doi.org/10.1002/ppp.3430010108 <https://doi.org/10.1002/ppp.3430010108> Publication - Article PeerReviewed 1990 ftnerc https://doi.org/10.1002/ppp.3430010108 2023-02-04T19:46:47Z By means of re‐evaluating a number of properties of rock tablets left in the field for varying time periods, an estimation of rock breakdown rates is attained. From data obtained during the last five years, it would appear that rates are very slow, only of the order of 2% mass loss per 100 years. These rates refer to omnidirectionally frozen, relatively wet samples and, on the basis of laboratory simulation results, are over 50 times greater than for unidirectionally frozen bedrock. It is suggested that mechanical weathering rates in the maritime Antarctic are very slow. Article in Journal/Newspaper Antarc* Antarctic Permafrost and Periglacial Processes Signy Island Natural Environment Research Council: NERC Open Research Archive Antarctic Signy Island ENVELOPE(-45.595,-45.595,-60.708,-60.708) Permafrost and Periglacial Processes 1 1 61 67 |
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Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
unknown |
description |
By means of re‐evaluating a number of properties of rock tablets left in the field for varying time periods, an estimation of rock breakdown rates is attained. From data obtained during the last five years, it would appear that rates are very slow, only of the order of 2% mass loss per 100 years. These rates refer to omnidirectionally frozen, relatively wet samples and, on the basis of laboratory simulation results, are over 50 times greater than for unidirectionally frozen bedrock. It is suggested that mechanical weathering rates in the maritime Antarctic are very slow. |
format |
Article in Journal/Newspaper |
author |
Hall, Kevin |
spellingShingle |
Hall, Kevin Mechanical weathering rates on Signy Island, maritime Antarctic |
author_facet |
Hall, Kevin |
author_sort |
Hall, Kevin |
title |
Mechanical weathering rates on Signy Island, maritime Antarctic |
title_short |
Mechanical weathering rates on Signy Island, maritime Antarctic |
title_full |
Mechanical weathering rates on Signy Island, maritime Antarctic |
title_fullStr |
Mechanical weathering rates on Signy Island, maritime Antarctic |
title_full_unstemmed |
Mechanical weathering rates on Signy Island, maritime Antarctic |
title_sort |
mechanical weathering rates on signy island, maritime antarctic |
publisher |
Wiley |
publishDate |
1990 |
url |
http://nora.nerc.ac.uk/id/eprint/520404/ https://doi.org/10.1002/ppp.3430010108 |
long_lat |
ENVELOPE(-45.595,-45.595,-60.708,-60.708) |
geographic |
Antarctic Signy Island |
geographic_facet |
Antarctic Signy Island |
genre |
Antarc* Antarctic Permafrost and Periglacial Processes Signy Island |
genre_facet |
Antarc* Antarctic Permafrost and Periglacial Processes Signy Island |
op_relation |
Hall, Kevin. 1990 Mechanical weathering rates on Signy Island, maritime Antarctic. Permafrost and Periglacial Processes, 1 (1). 61-67. https://doi.org/10.1002/ppp.3430010108 <https://doi.org/10.1002/ppp.3430010108> |
op_doi |
https://doi.org/10.1002/ppp.3430010108 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
1 |
container_issue |
1 |
container_start_page |
61 |
op_container_end_page |
67 |
_version_ |
1766251789832683520 |