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

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


Titill: 2021–2023 Unrest and Geodetic Observations at Askja Volcano, Iceland
Höfundur: Parks, Michelle M.
Sigmundsson, Freysteinn   orcid.org/0000-0001-9052-4665
Drouin, Vincent   orcid.org/0000-0002-5340-0484
Hreinsdóttir, Sigrún
Hooper, Andrew
Yang, Yilin
Ófeigsson, Benedikt G.
Sturkell, Erik
Hjartardóttir, Ásta R.
Grapenthin, Ronni
... 7 fleiri höfundar Sýna alla höfunda
Útgáfa: 2024-02-28
Tungumál: Enska
Umfang: 1944600
Svið: Engineering and Natural Sciences
Deild: Faculty of Earth Sciences
Science Institute
Birtist í: Geophysical Research Letters; 51(4)
ISSN: 0094-8276
DOI: 10.1029/2023GL106730
Efnisorð: Askja volcano; GNSS; InSAR; volcanic unrest; volcano geodesy; volcano monitoring; Geophysics; General Earth and Planetary Sciences
URI: https://hdl.handle.net/20.500.11815/4974

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Tilvitnun:

Parks , M M , Sigmundsson , F , Drouin , V , Hreinsdóttir , S , Hooper , A , Yang , Y , Ófeigsson , B G , Sturkell , E , Hjartardóttir , Á R , Grapenthin , R , Geirsson , H , Trasatti , E , Barsotti , S , Pedersen , R , Einarsson , P , Óladóttir , B A & Friðriksdóttir , H M 2024 , ' 2021–2023 Unrest and Geodetic Observations at Askja Volcano, Iceland ' , Geophysical Research Letters , vol. 51 , no. 4 , e2023GL106730 . https://doi.org/10.1029/2023GL106730

Útdráttur:

Unrest 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.

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Publisher Copyright: © 2024. The Authors.

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