Origin, chronology and climatological significance of annual-moraine ridges at Myrdalsjökull, Iceland
Minor, transverse moraine ridges have formed annually at the retreating north margin of Myrdalsjökull, 550-600 m a.s.l., in south Iceland during the period 1928-1981. They are composed of slabs of clast-paved lodgement till and their formation at the glacier edge results from subglacial freezing-on...
Published in: | The Holocene |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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SAGE Publications
1995
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Online Access: | http://dx.doi.org/10.1177/095968369500500404 http://journals.sagepub.com/doi/pdf/10.1177/095968369500500404 |