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...

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Bibliographic Details
Published in:The Holocene
Main Author: Krüger, Johannes
Format: Article in Journal/Newspaper
Language:English
Published: SAGE Publications 1995
Subjects:
Online Access:http://dx.doi.org/10.1177/095968369500500404
http://journals.sagepub.com/doi/pdf/10.1177/095968369500500404