Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway

Abstract Sorted circles and nets formed on the surface of the principal medial moraine on Storbreen, Jotunheimcn, Norway, are described. These consist of “islands” of coarse sand, granules, and small pebbles, surrounded by pebbles and cobbles and underlain by small domes of glacier ice. It is sugges...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Ballantyne, C. K.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1979
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000014386
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014386
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spelling crcambridgeupr:10.1017/s0022143000014386 2024-03-03T08:44:38+00:00 Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway Ballantyne, C. K. 1979 http://dx.doi.org/10.1017/s0022143000014386 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014386 en eng Cambridge University Press (CUP) Journal of Glaciology volume 22, issue 87, page 396-401 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1979 crcambridgeupr https://doi.org/10.1017/s0022143000014386 2024-02-08T08:40:37Z Abstract Sorted circles and nets formed on the surface of the principal medial moraine on Storbreen, Jotunheimcn, Norway, are described. These consist of “islands” of coarse sand, granules, and small pebbles, surrounded by pebbles and cobbles and underlain by small domes of glacier ice. It is suggested that patterned ground formation on the moraine results from differential ablation in areas of thin (<200 mm) debris cover near the glacier snout, where melting is relatively rapid. It is unlikely that supraglacial patterned ground could survive deposition. Article in Journal/Newspaper glacier Journal of Glaciology Cambridge University Press Norway Storbreen ENVELOPE(8.269,8.269,62.521,62.521) Journal of Glaciology 22 87 396 401
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Ballantyne, C. K.
Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway
topic_facet Earth-Surface Processes
description Abstract Sorted circles and nets formed on the surface of the principal medial moraine on Storbreen, Jotunheimcn, Norway, are described. These consist of “islands” of coarse sand, granules, and small pebbles, surrounded by pebbles and cobbles and underlain by small domes of glacier ice. It is suggested that patterned ground formation on the moraine results from differential ablation in areas of thin (<200 mm) debris cover near the glacier snout, where melting is relatively rapid. It is unlikely that supraglacial patterned ground could survive deposition.
format Article in Journal/Newspaper
author Ballantyne, C. K.
author_facet Ballantyne, C. K.
author_sort Ballantyne, C. K.
title Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway
title_short Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway
title_full Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway
title_fullStr Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway
title_full_unstemmed Patterned Ground on an Active Medial Moraine, Jotunheimen, Norway
title_sort patterned ground on an active medial moraine, jotunheimen, norway
publisher Cambridge University Press (CUP)
publishDate 1979
url http://dx.doi.org/10.1017/s0022143000014386
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000014386
long_lat ENVELOPE(8.269,8.269,62.521,62.521)
geographic Norway
Storbreen
geographic_facet Norway
Storbreen
genre glacier
Journal of Glaciology
genre_facet glacier
Journal of Glaciology
op_source Journal of Glaciology
volume 22, issue 87, page 396-401
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000014386
container_title Journal of Glaciology
container_volume 22
container_issue 87
container_start_page 396
op_container_end_page 401
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