To the top

Page Manager: Webmaster
Last update: 9/11/2012 3:13 PM

Tell a friend about this page
Print version

New insights into volcani… - University of Gothenburg, Sweden Till startsida
To content Read more about how we use cookies on

New insights into volcanic activity from strain and other deformation data for the Hekla 2000 eruption

Journal article
Authors Erik Sturkell
K. Ágústsson
A. T. Linde
S.I. Sacks
P. Einarsson
F. Sigmundsson
H. Geirsson
R. Pedersen
P.C. LaFemina
H. Ólafsson
Published in Journal of Volcanology and Geothermal Research
Volume 256
Pages 78–86
ISSN 0377-0273
Publication year 2013
Published at
Pages 78–86
Language en
Subject categories Earth and Related Environmental Sciences


Hekla is one of Iceland's most active volcanoes; its eruptions, characterized by surface fissuring and repeated lava flows during its post-glacial activity, have built up an 800 m high elongated mountain. Since 1970 it has erupted every ~ 10 years; the previous repose interval averaged ~ 60 years. For the last eruption in 2000 we constrain the magma geometry by using a wide variety of deformation data: campaign GPS; an InSAR interferogram; dry tilt data, and borehole strain data. The dike that causes surface fissuring extends no more than ~ 0.5 km in depth, and the reservoir depth is ~ 10 km. These are connected by a conduit of small lateral extent. Data for previous eruptions are consistent with this model. We propose that the marked change in eruption interval is because this conduit remains liquid during the short interval between recent eruptions; only a small pressure increase is required to rupture the thin crustal seal. Such a state is consistent with precursory seismicity being confined to very shallow depths and may be applicable to other volcanoes that undergo abrupt changes in eruption interval.

Page Manager: Webmaster|Last update: 9/11/2012

The University of Gothenburg uses cookies to provide you with the best possible user experience. By continuing on this website, you approve of our use of cookies.  What are cookies?