Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island
Abstract Sorted stripes found on the volcanic scoria and glacial deposits of sub‐Antarctic Marion Island indicate a distinct preferred orientation. Despite uniformity of slope and material, the stripes are predominantly aligned parallel to the wind. It is suggested that melting of needle ice by the...
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crwiley:10.1002/esp.3290040309 2024-09-15T17:48:12+00:00 Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island Hall, Kevin 1979 http://dx.doi.org/10.1002/esp.3290040309 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.3290040309 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.3290040309 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Earth Surface Processes volume 4, issue 3, page 281-289 ISSN 0360-1269 1931-8065 journal-article 1979 crwiley https://doi.org/10.1002/esp.3290040309 2024-07-25T04:21:55Z Abstract Sorted stripes found on the volcanic scoria and glacial deposits of sub‐Antarctic Marion Island indicate a distinct preferred orientation. Despite uniformity of slope and material, the stripes are predominantly aligned parallel to the wind. It is suggested that melting of needle ice by the early morning sun is of only limited importance in the sub‐Antarctic owing to the almost continual overcast conditions. The effect of the wind is so great that in exposed situations stripes are formed on horizontal surfaces. Article in Journal/Newspaper Antarc* Antarctic Marion Island Wiley Online Library Earth Surface Processes 4 3 281 289 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract Sorted stripes found on the volcanic scoria and glacial deposits of sub‐Antarctic Marion Island indicate a distinct preferred orientation. Despite uniformity of slope and material, the stripes are predominantly aligned parallel to the wind. It is suggested that melting of needle ice by the early morning sun is of only limited importance in the sub‐Antarctic owing to the almost continual overcast conditions. The effect of the wind is so great that in exposed situations stripes are formed on horizontal surfaces. |
format |
Article in Journal/Newspaper |
author |
Hall, Kevin |
spellingShingle |
Hall, Kevin Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island |
author_facet |
Hall, Kevin |
author_sort |
Hall, Kevin |
title |
Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island |
title_short |
Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island |
title_full |
Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island |
title_fullStr |
Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island |
title_full_unstemmed |
Sorted stripes orientated by wind action: Some observations from sub‐antarctic marion island |
title_sort |
sorted stripes orientated by wind action: some observations from sub‐antarctic marion island |
publisher |
Wiley |
publishDate |
1979 |
url |
http://dx.doi.org/10.1002/esp.3290040309 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.3290040309 https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.3290040309 |
genre |
Antarc* Antarctic Marion Island |
genre_facet |
Antarc* Antarctic Marion Island |
op_source |
Earth Surface Processes volume 4, issue 3, page 281-289 ISSN 0360-1269 1931-8065 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/esp.3290040309 |
container_title |
Earth Surface Processes |
container_volume |
4 |
container_issue |
3 |
container_start_page |
281 |
op_container_end_page |
289 |
_version_ |
1810289338020265984 |