Wind Erosion By Snow
Abstract Calcite (Mohs hardness 3), fluorite (hardness 4) and periclase (hardness 5 1/2) have been eroded by snow blown at moderate wind velocities, at temperatures between —10 and —25°C. Future interpretations involving ventifacts and apparently wind-blasted rock exposures must take this informatio...
Published in: | Journal of Glaciology |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1977
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000021614 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021614 |
id |
crcambridgeupr:10.1017/s0022143000021614 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0022143000021614 2024-03-03T08:45:58+00:00 Wind Erosion By Snow Dietrich, R.V. 1977 http://dx.doi.org/10.1017/s0022143000021614 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021614 en eng Cambridge University Press (CUP) Journal of Glaciology volume 18, issue 78, page 148-149 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1977 crcambridgeupr https://doi.org/10.1017/s0022143000021614 2024-02-08T08:37:11Z Abstract Calcite (Mohs hardness 3), fluorite (hardness 4) and periclase (hardness 5 1/2) have been eroded by snow blown at moderate wind velocities, at temperatures between —10 and —25°C. Future interpretations involving ventifacts and apparently wind-blasted rock exposures must take this information into account. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 18 78 148 149 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Dietrich, R.V. Wind Erosion By Snow |
topic_facet |
Earth-Surface Processes |
description |
Abstract Calcite (Mohs hardness 3), fluorite (hardness 4) and periclase (hardness 5 1/2) have been eroded by snow blown at moderate wind velocities, at temperatures between —10 and —25°C. Future interpretations involving ventifacts and apparently wind-blasted rock exposures must take this information into account. |
format |
Article in Journal/Newspaper |
author |
Dietrich, R.V. |
author_facet |
Dietrich, R.V. |
author_sort |
Dietrich, R.V. |
title |
Wind Erosion By Snow |
title_short |
Wind Erosion By Snow |
title_full |
Wind Erosion By Snow |
title_fullStr |
Wind Erosion By Snow |
title_full_unstemmed |
Wind Erosion By Snow |
title_sort |
wind erosion by snow |
publisher |
Cambridge University Press (CUP) |
publishDate |
1977 |
url |
http://dx.doi.org/10.1017/s0022143000021614 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021614 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 18, issue 78, page 148-149 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000021614 |
container_title |
Journal of Glaciology |
container_volume |
18 |
container_issue |
78 |
container_start_page |
148 |
op_container_end_page |
149 |
_version_ |
1792501712077979648 |