2021–2023 Unrest and Geodetic Observations at Askja Volcano, Iceland

Author:

Parks Michelle M.1ORCID,Sigmundsson Freysteinn2ORCID,Drouin Vincent1ORCID,Hreinsdóttir Sigrún3ORCID,Hooper Andrew4ORCID,Yang Yilin2ORCID,Ófeigsson Benedikt G.1,Sturkell Erik5ORCID,Hjartardóttir Ásta R.2ORCID,Grapenthin Ronni6ORCID,Geirsson Halldór2,Trasatti Elisa7ORCID,Barsotti Sara1,Pedersen Rikke2,Einarsson Páll2ORCID,Óladóttir Bergrún A.1,Friðriksdóttir Hildur M.1

Affiliation:

1. Icelandic Meteorological Office Reykjavik Iceland

2. Nordic Volcanological Center Institute of Earth Sciences University of Iceland Reykjavik Iceland

3. GNS Science Lower Hutt New Zealand

4. COMET School of Earth and Environment University of Leeds Leeds UK

5. Department of Earth Sciences University of Gothenburg Goteborg Sweden

6. Geophysical Institute University of Alaska Fairbanks Fairbanks AK USA

7. Istituto Nazionale di Geofisica e Vulcanologia Rome Italy

Abstract

AbstractUnrest began in July 2021 at Askja volcano in the Northern Volcanic Zone (NVZ) of Iceland. Its most recent eruption, in 1961, was predominantly effusive and produced ∼0.1 km3 lava field. The last plinian eruption at Askja occurred in 1875. Geodetic measurements between 1983 and 2021 detail subsidence of Askja, decaying in an exponential manner. At the end of July 2021, inflation was detected at Askja volcano, from GNSS observations and Sentinel‐1 interferograms. The inflationary episode can be divided into two periods from the onset of inflation until September 2023. An initial period until 20 September 2021 when geodetic models suggest transfer of magma (or magmatic fluids) from within the shallowest part of the magmatic system (comprising an inflating and deflating source), potentially involving silicic magma. A following period when one source of pressure increase at shallow depth can explain the observations.

Funder

Natural Environment Research Council

National Science Foundation

Publisher

American Geophysical Union (AGU)

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