THE MÚLAJÖKULL DRUMLIN FIELD - SEDIMENTOLOGY AND GEOMORPHOLOGY

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MARC

Jonsson, Sverrir (author)

THE MÚLAJÖKULL DRUMLIN FIELD - SEDIMENTOLOGY AND GEOMORPHOLOGY

Article/chapterEnglish2011

Publisher, publication year, extent ...

2011

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LIBRIS-ID:oai:gup.ub.gu.se/149055
https://gup.ub.gu.se/publication/149055URI

Supplementary language notes

Language:English

Part of subdatabase

SwePubSwePub

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Subject category:ref swepub-contenttype
Subject category:kon swepub-publicationtype

Notes

The drumlin field in front of Múlajökull, a surge-style, outlet glacier from Hofsjökull in Iceland, is the only known active drumlin field (Johnson et al., 2010). The aim of this study is to further explore the formation of drumlins in a modern glacial environment. We use data from geological sections, DEMs, aerial imagery and field mapping. Here we present preliminary results from section logging and geomorphological mapping in the summer of 2011. Geomorphological mapping of the drumlin field both with DEMs and ground proofing has revealed over 100 drumlins and a number of drumlinized ridges. The drumlins furthest from the present ice margin appear broader and have lower relief than those closer to the ice. We suggest that this reflects an evolution of the drumlin form during recurrent surging. The drumlins farther away from the ice have experienced fewer surges than those that have just been uncovered due to retreat of the ice margin. During successive surges, the drumlins become narrower and develop higher relief. In one section close to the present ice margin, we identified at least 9 till beds in the crest of a drumlin, each likely the product of a surge, representing approximately 1/3 of the drumlin relief. The top till bed parallels the drumlin form and truncates the older tills. The older units also dip parallel to the drumlin form, but at a slightly lower angle. We believe that this represents an earlier, broader shape of the drumlin prior to the more recent surges, implying an evolution of form similar to that seen in the evolution in form in the drumlin field. The Múlajökull drumlins have thus grown during surging by erosion on the proximal end and sides of the drumlin followed by accretion of till sheets concentrically on the resulting form.

Subject headings and genre

NATURVETENSKAP Geovetenskap och miljövetenskap Geologi hsv//swe
NATURAL SCIENCES Earth and Related Environmental Sciences Geology hsv//eng
Mulajökull drumlin

Added entries (persons, corporate bodies, meetings, titles ...)

Schomacker, Anders (author)
Benediktsson, Ivar Örn (author)
Johnson, Mark D.,1954Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences(Swepub:gu)xjohnm (author)
Brynolfsson, Skafti (author)
Ingolfsson, Olafur (author)
Göteborgs universitetInstitutionen för geovetenskaper (creator_code:org_t)

Related titles

In:Geological Society of America abstracts with programs Minneapolis 2011

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By the author/editor: Jonsson, Sverrir; Schomacker, Ande ...; Benediktsson, Iv ...; Johnson, Mark D. ...; Brynolfsson, Ska ...; Ingolfsson, Olaf ...

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NATURAL SCIENCES: NATURAL SCIENCES; and Earth and Relate ...; and Geology

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By the university: University of Gothenburg

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