The Initiation of Dirt Cones on Snow

Abstract Dirt cones develop where debris has been blown on to snow and has become concentrated into numerous small patches thick enough to protect the underlying snow from ablation. These striking accumulations of dirt, separated by virtually dirt-free snow, are produced by movement (both contractio...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Wilson, J. Warren
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1953
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000025478
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025478
id crcambridgeupr:10.1017/s0022143000025478
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000025478 2024-03-03T08:46:09+00:00 The Initiation of Dirt Cones on Snow Wilson, J. Warren 1953 http://dx.doi.org/10.1017/s0022143000025478 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025478 en eng Cambridge University Press (CUP) Journal of Glaciology volume 2, issue 14, page 281-287 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1953 crcambridgeupr https://doi.org/10.1017/s0022143000025478 2024-02-08T08:37:11Z Abstract Dirt cones develop where debris has been blown on to snow and has become concentrated into numerous small patches thick enough to protect the underlying snow from ablation. These striking accumulations of dirt, separated by virtually dirt-free snow, are produced by movement (both contraction and expansion) of the snow surface during ablation. Factors controlling this movement operate in such a way that local concentrations of dirt will be produced even when initial deposition of the dirt is almost uniform. The significance of these processes in relation to the development and structure of dirt cone fields is discussed, and certain experiments and observations on dirt cones are described. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 2 14 281 287
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Wilson, J. Warren
The Initiation of Dirt Cones on Snow
topic_facet Earth-Surface Processes
description Abstract Dirt cones develop where debris has been blown on to snow and has become concentrated into numerous small patches thick enough to protect the underlying snow from ablation. These striking accumulations of dirt, separated by virtually dirt-free snow, are produced by movement (both contraction and expansion) of the snow surface during ablation. Factors controlling this movement operate in such a way that local concentrations of dirt will be produced even when initial deposition of the dirt is almost uniform. The significance of these processes in relation to the development and structure of dirt cone fields is discussed, and certain experiments and observations on dirt cones are described.
format Article in Journal/Newspaper
author Wilson, J. Warren
author_facet Wilson, J. Warren
author_sort Wilson, J. Warren
title The Initiation of Dirt Cones on Snow
title_short The Initiation of Dirt Cones on Snow
title_full The Initiation of Dirt Cones on Snow
title_fullStr The Initiation of Dirt Cones on Snow
title_full_unstemmed The Initiation of Dirt Cones on Snow
title_sort initiation of dirt cones on snow
publisher Cambridge University Press (CUP)
publishDate 1953
url http://dx.doi.org/10.1017/s0022143000025478
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000025478
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 2, issue 14, page 281-287
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000025478
container_title Journal of Glaciology
container_volume 2
container_issue 14
container_start_page 281
op_container_end_page 287
_version_ 1792502116475994112