The Volcanic Hazards of Jan Mayen Island (North-Atlantic)

• Published in: Frontiers in Earth Science
• Main Authors: Gjerløw, Eirik, Hoskuldsson, Armann, Bartolini, Stefania, Biass,Sebastien, Mossoux, Sophie, Gilbert, Jennie, Pedersen,Rolf B., Martí Molist, Joan
• Other Authors: University of Bergen, University of Iceland, European Commission
• Format: Article in Journal/Newspaper
• Language: English
• Published: Frontiers Media 2022
• Subjects: Hazard assesment; Volcano; Geohazard; Hazard models; Volcanic hazard; Eruptive Scenarios; Arctic; Beerenberg; Bergen; Jan Mayen; Norway; Iceland; Jan Mayen Island; North Atlantic; Arctic University of Norway; UiT The Arctic University of Norway
• Online Access: http://hdl.handle.net/10261/263460; https://doi.org/10.13039/501100005036; https://doi.org/10.13039/501100000780

Hazard assessment of remote volcanic islands provides many challenges compared to other volcanoes and volcanic fields. Here we present the first systematic volcanic hazard assessment of Jan Mayen Island, a remote island located in the North-Atlantic Ocean and home to the northernmost active subaerial volcano in the world (Beerenberg Volcano), and we discuss some of the challenges and characteristics of performing a volcanic hazard assessment of a remote volcanic island. Jan Mayen has had at least five eruptions since its discovery at the start of the 17th century. Its Holocene volcanism is mainly characterized by eruptions with styles ranging from Hawaiian to Strombolian, but also by lava domes and Surtseyan eruptions. Based on field data, remote images, topographic data, past data, and computer simulations, our study evaluates the spatial probability of new vents opening, estimates eruption recurrence rates, simulates various eruption scenarios, and produces hazard maps for the different scenarios. This work shows where the hazards of ash fall, and lava flows are more likely to affect the built infrastructure on Jan Mayen Island. This hazard assessment will assist emergency planning and the determination of future land use on the island. This study was part of EG’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. This paper has been written while the lead author has been employed at UiT the Arctic University of Norway. This study has also been part of the VeTools and EVE projects (EC ECHO Grants SI2.695524 and 826292). Peer reviewed