Abstract
The island of Jan Mayen in the North Atlantic Ocean is home to the world’s northernmost active subaerial volcano, Beerenberg. Of the five known historical eruptions on the island, the locations of two eruptions (1732 and 1818) have not been accurately located. It is known that the 1732 and 1818 eruptions occurred on the south flank of Beerenberg, and several eruption sites have been proposed for these events. Here we show that the tuff cone of Eggøya on the SW flank of Beerenberg was the site of the 1732 eruption, based on interpretation of the deposits, field relations and historical sources. We further describe the deposits from the eruption and show that Eggøya is the largest explosive eruption described from Jan Mayen, emplacing at least at least 0.3–0.4 km3 (VEI 4) of basanitic tephra up to distances of at least 111 km from Jan Mayen and covering a minimum area of around 500 km2 within the 2-cm isopach. We also present our eruption scenario and show that this was an emergent Surtseyan eruption with activity shifting between tephra jetting, continuous uprush and more magmatic phases.
| Original language | English |
|---|---|
| Journal | Bulletin of Volcanology |
| Volume | 77 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - Feb 2015 |
Bibliographical note
Funding Information: This study was part of E. Gjerløw’s Ph.D. project and was financed by the Centre for Geobiology at the University of Bergen and the Nordic Volcanological Center at the University of Iceland. We want to acknowledge the Jan Mayen personnel for their hospitality and assistance during fieldwork, Chris Hayward for assistance with microprobing and the Norwegian Polar Institute for supplying aerial photos and map data. Thanks are given to associate editor P.-S. Ross and reviewers Y.K. Sohn and D. Pedrazzi whose comments helped to improve this paper. Publisher Copyright: © 2015, Springer-Verlag Berlin Heidelberg.Other keywords
- Jan Mayen
- Surtseyan eruptions
- Tephra
- Volcanic hazards