Architecture and structural evolution of an early Little Ice Age terminal moraine at the surge-type glacier Múlajökull, Iceland

Author:

Benediktsson Ívar Örn1ORCID,Schomacker Anders23,Johnson Mark D.4,Geiger Alessa J.5,Ingólfsson Ólafur67,Guðmundsdóttir Esther Ruth7

Affiliation:

1. Department of Geology; Lund University; Lund Sweden

2. Department of Geology; Norwegian University of Science and Technology; Trondheim Norway

3. Centre for GeoGenetics, Natural History Museum of Denmark; University of Copenhagen; Copenhagen Denmark

4. Department of Earth Sciences; University of Gothenburg; Gothenburg Sweden

5. School of Geographical and Earth Sciences; University of Glasgow; Glasgow UK

6. University Centre in Svalbard; Longyearbyen Norway

7. Institute of Earth Sciences; University of Iceland; Reykjavík Iceland

Funder

Carlsberg Foundation

University of Iceland Research Fund

Energy Research Fund of Landsvirkjun

Icelandic Center for Research (RANNÍS)

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Reference60 articles.

1. Glaciotectonism. Elsevier, Amsterdam;Aber;Dev. Quat. Sci.,2007

2. Glaciotectonic Landforms and Structures

3. Benediktsson , Í. Ö. 2010 End moraine and ice marginal processes of surge-type glaciers-Brúarjökull and Eyjabakkajökull, Iceland

4. Polyphase structural evolution of a fine-grained, fold-dominated end moraine, Brúarjökull surge-type glacier;Benediktsson;Icel. Jökull,2012

5. Instantaneous end moraine and sediment wedge formation during the 1890 glacier surge of Brúarjökull, Iceland;Benediktsson;Quat. Sci. Rev.,2008

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