Bulletin of Volcanology

, 75:717 | Cite as

From feeder dykes to scoria cones: the tectonically controlled plumbing system of the Rauðhólar volcanic chain, Northern Volcanic Zone, Iceland

  • Nadine FrieseEmail author
  • Frithjof A. Bense
  • David C. Tanner
  • Lúðvík E. Gústafsson
  • Siegfried Siegesmund
Research Article


The Rauðhólar volcanic chain, located in the Northern Volcanic Zone of Iceland, has been variably eroded such that, in the northern part, the original scoria cones are preserved, while the central and southern parts expose their shallow feeders. The chain thus offers insight into the inner workings of the near-surface feeder system of scoria cones. The volcanic chain was mapped in 3D using GPS. The en echelon-arranged volcanic chain can be divided into three parts: The southernmost part contains only plugs and necks with a thin pyroclastic cover as well as multi-tiered lava flows. The central part combines partially eroded scoria cones, (feeder) dyke intersections, and welded scoria interbedded within rootless and clastogenic lava flows; the welded scoria is composed of different kinds of lithics and bombs. The northern part preserves almost intact, overlapping scoria cones with voluminous lapilli-sized scoriaceous deposits. The overall dyke trend is orthogonal but shows radial patterns in individual cone complexes. Feeder dykes observed to depths of about 200 m below the volcanic chain are up to 8 m thick and flare in to conduits in the uppermost 20–50 m. The exposed shallow plumbing system shows that magma pathways through the volcanic edifice are very complex with incremental, repeated intrusions. We interpret the arcuate shape to be the result of a local change in the orientation of the stress field because the Rauðhólar volcanic chain is located within a major relay structure between volcanoes on the eastern Fremrinámur rift arm and a rift extension with grabens on the western periphery.


Scoria cone row Hljóðaklettar Rauðhólar Northeast Iceland Stress localization Accommodation zone Plumbing system 



We are grateful to the National Park managers Sigþrúður Stella Jóhannsdóttir and Þorsteinn Hymer and the staff of the Jökulsárgljúfur Park for the work permission and their support during our field studies. The rangers Jóna and Kristin are especially thanked for their company in the ranger house and introducing us to cultural highlights in Asbyrgi. Árman Höskuldsson is acknowledged for the help with the literature research and Sigurður Steinþórsson for the support with formalities at the beginning of the field work. We thank Steffi Burchardt, University of Uppsala, and Matteo Lupi, University of Bonn, for the very helpful discussions. We are grateful for the financial support from the Structural Geology and Geodynamics Department of the University of Göttingen. Midland Valley is acknowledged for providing a free educational license for their software Move 2008.1. We thank the journal reviewers Greg Valentine and José Jorge Aranda Gómez for their constructive reviews and Pierre-Simon Ross for the editorial work. The authors thank two anonymous reviewers for the helpful comments of an earlier version of the manuscript.

Supplementary material


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Copyright information

© Springer-Verlag Berlin Heidelberg 2013

Authors and Affiliations

  • Nadine Friese
    • 1
    • 4
    Email author
  • Frithjof A. Bense
    • 1
  • David C. Tanner
    • 2
  • Lúðvík E. Gústafsson
    • 3
  • Siegfried Siegesmund
    • 1
  1. 1.Department of Structural Geology and Geodynamics, Geoscience CentreUniversity of GöttingenGöttingenGermany
  2. 2.Leibniz Institute for Applied GeophysicsHannoverGermany
  3. 3.Icelandic Association of Local AuthoritiesReykjavíkIceland
  4. 4.Wintershall Norge ASStavangerNorway

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