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Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland.

Nature

Sigmundsson F, Hooper A, Hreinsdóttir S, Vogfjörd KS, Ófeigsson BG, Heimisson ER, Dumont S, Parks M, Spaans K, Gudmundsson GB, Drouin V, Árnadóttir T, Jónsdóttir K, Gudmundsson MT, Högnadóttir T, Fridriksdóttir HM, Hensch M, Einarsson P, Magnússon E, Samsonov S, Brandsdóttir B, White RS, Ágústsdóttir T, Greenfield T, Green RG, Hjartardóttir ÁR, Pedersen R, Bennett RA, Geirsson H, La Femina PC, Björnsson H, Pálsson F, Sturkell E, Bean CJ, Möllhoff M, Braiden AK, Eibl EP.
PMID: 25517098
Nature. 2015 Jan 08;517(7533):191-5. doi: 10.1038/nature14111. Epub 2014 Dec 15.

Crust at many divergent plate boundaries forms primarily by the injection of vertical sheet-like dykes, some tens of kilometres long. Previous models of rifting events indicate either lateral dyke growth away from a feeding source, with propagation rates decreasing...

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Sigmundsson F, Hooper A, Hreinsdóttir S, et al. Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland. Nature. 2014;517(7533):191-5doi: 10.1038/nature14111.
Sigmundsson, F., Hooper, A., Hreinsdóttir, S., Vogfjörd, K. S., Ófeigsson, B. G., Heimisson, E. R., Dumont, S., Parks, M., Spaans, K., Gudmundsson, G. B., Drouin, V., Árnadóttir, T., Jónsdóttir, K., Gudmundsson, M. T., Högnadóttir, T., Fridriksdóttir, H. M., Hensch, M., Einarsson, P., Magnússon, E., Samsonov, S., Brandsdóttir, B., White, R. S., Ágústsdóttir, T., Greenfield, T., Green, R. G., Hjartardóttir, �. �. R., Pedersen, R., Bennett, R. A., Geirsson, H., La Femina, P. C., Björnsson, H., Pálsson, F., Sturkell, E., Bean, C. J., Möllhoff, M., Braiden, A. K., & Eibl, E. P. (2015). Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland. Nature, 517(7533), 191-5. https://doi.org/10.1038/nature14111
Sigmundsson, Freysteinn, et al. "Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland." Nature vol. 517,7533 (2015): 191-5. doi: https://doi.org/10.1038/nature14111
Sigmundsson F, Hooper A, Hreinsdóttir S, Vogfjörd KS, Ófeigsson BG, Heimisson ER, Dumont S, Parks M, Spaans K, Gudmundsson GB, Drouin V, Árnadóttir T, Jónsdóttir K, Gudmundsson MT, Högnadóttir T, Fridriksdóttir HM, Hensch M, Einarsson P, Magnússon E, Samsonov S, Brandsdóttir B, White RS, Ágústsdóttir T, Greenfield T, Green RG, Hjartardóttir ÁR, Pedersen R, Bennett RA, Geirsson H, La Femina PC, Björnsson H, Pálsson F, Sturkell E, Bean CJ, Möllhoff M, Braiden AK, Eibl EP. Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland. Nature. 2015 Jan 08;517(7533):191-5. doi: 10.1038/nature14111. Epub 2014 Dec 15. PMID: 25517098.
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Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow.

Science (New York, N.Y.)

Gudmundsson MT, Jónsdóttir K, Hooper A, Holohan EP, Halldórsson SA, Ófeigsson BG, Cesca S, Vogfjörd KS, Sigmundsson F, Högnadóttir T, Einarsson P, Sigmarsson O, Jarosch AH, Jónasson K, Magnússon E, Hreinsdóttir S, Bagnardi M, Parks MM, Hjörleifsdóttir V, Pálsson F, Walter TR, Schöpfer MP, Heimann S, Reynolds HI, Dumont S, Bali E, Gudfinnsson GH, Dahm T, Roberts MJ, Hensch M, Belart JM, Spaans K, Jakobsson S, Gudmundsson GB, Fridriksdóttir HM, Drouin V, Dürig T, Aðalgeirsdóttir G, Riishuus MS, Pedersen GB, van Boeckel T, Oddsson B, Pfeffer MA, Barsotti S, Bergsson B, Donovan A, Burton MR, Aiuppa A.
PMID: 27418515
Science. 2016 Jul 15;353(6296):aaf8988. doi: 10.1126/science.aaf8988.

Large volcanic eruptions on Earth commonly occur with a collapse of the roof of a crustal magma reservoir, forming a caldera. Only a few such collapses occur per century, and the lack of detailed observations has obscured insight into...

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Gudmundsson MT, Jónsdóttir K, Hooper A, et al. Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow. Science. 2016;353(6296):aaf8988doi: 10.1126/science.aaf8988.
Gudmundsson, M. T., Jónsdóttir, K., Hooper, A., Holohan, E. P., Halldórsson, S. A., Ófeigsson, B. G., Cesca, S., Vogfjörd, K. S., Sigmundsson, F., Högnadóttir, T., Einarsson, P., Sigmarsson, O., Jarosch, A. H., Jónasson, K., Magnússon, E., Hreinsdóttir, S., Bagnardi, M., Parks, M. M., Hjörleifsdóttir, V., Pálsson, F., Walter, T. R., Schöpfer, M. P., Heimann, S., Reynolds, H. I., Dumont, S., Bali, E., Gudfinnsson, G. H., Dahm, T., Roberts, M. J., Hensch, M., Belart, J. M., Spaans, K., Jakobsson, S., Gudmundsson, G. B., Fridriksdóttir, H. M., Drouin, V., Dürig, T., Aðalgeirsdóttir, G., Riishuus, M. S., Pedersen, G. B., van Boeckel, T., Oddsson, B., Pfeffer, M. A., Barsotti, S., Bergsson, B., Donovan, A., Burton, M. R., & Aiuppa, A. (2016). Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow. Science (New York, N.Y.), 353(6296), aaf8988. https://doi.org/10.1126/science.aaf8988
Gudmundsson, Magnús T, et al. "Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow." Science (New York, N.Y.) vol. 353,6296 (2016): aaf8988. doi: https://doi.org/10.1126/science.aaf8988
Gudmundsson MT, Jónsdóttir K, Hooper A, Holohan EP, Halldórsson SA, Ófeigsson BG, Cesca S, Vogfjörd KS, Sigmundsson F, Högnadóttir T, Einarsson P, Sigmarsson O, Jarosch AH, Jónasson K, Magnússon E, Hreinsdóttir S, Bagnardi M, Parks MM, Hjörleifsdóttir V, Pálsson F, Walter TR, Schöpfer MP, Heimann S, Reynolds HI, Dumont S, Bali E, Gudfinnsson GH, Dahm T, Roberts MJ, Hensch M, Belart JM, Spaans K, Jakobsson S, Gudmundsson GB, Fridriksdóttir HM, Drouin V, Dürig T, Aðalgeirsdóttir G, Riishuus MS, Pedersen GB, van Boeckel T, Oddsson B, Pfeffer MA, Barsotti S, Bergsson B, Donovan A, Burton MR, Aiuppa A. Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow. Science. 2016 Jul 15;353(6296):aaf8988. doi: 10.1126/science.aaf8988. PMID: 27418515.
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Intrusion triggering of the 2010 Eyjafjallajökull explosive eruption.

Nature

Sigmundsson F, Hreinsdóttir S, Hooper A, Arnadóttir T, Pedersen R, Roberts MJ, Oskarsson N, Auriac A, Decriem J, Einarsson P, Geirsson H, Hensch M, Ofeigsson BG, Sturkell E, Sveinbjörnsson H, Feigl KL.
PMID: 21085177
Nature. 2010 Nov 18;468(7322):426-30. doi: 10.1038/nature09558.

Gradual inflation of magma chambers often precedes eruptions at highly active volcanoes. During such eruptions, rapid deflation occurs as magma flows out and pressure is reduced. Less is known about the deformation style at moderately active volcanoes, such as...

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Sigmundsson F, Hreinsdóttir S, Hooper A, et al. Intrusion triggering of the 2010 Eyjafjallajökull explosive eruption. Nature. 2010;468(7322):426-30doi: 10.1038/nature09558.
Sigmundsson, F., Hreinsdóttir, S., Hooper, A., Arnadóttir, T., Pedersen, R., Roberts, M. J., Oskarsson, N., Auriac, A., Decriem, J., Einarsson, P., Geirsson, H., Hensch, M., Ofeigsson, B. G., Sturkell, E., Sveinbjörnsson, H., & Feigl, K. L. (2010). Intrusion triggering of the 2010 Eyjafjallajökull explosive eruption. Nature, 468(7322), 426-30. https://doi.org/10.1038/nature09558
Sigmundsson, Freysteinn, et al. "Intrusion triggering of the 2010 Eyjafjallajökull explosive eruption." Nature vol. 468,7322 (2010): 426-30. doi: https://doi.org/10.1038/nature09558
Sigmundsson F, Hreinsdóttir S, Hooper A, Arnadóttir T, Pedersen R, Roberts MJ, Oskarsson N, Auriac A, Decriem J, Einarsson P, Geirsson H, Hensch M, Ofeigsson BG, Sturkell E, Sveinbjörnsson H, Feigl KL. Intrusion triggering of the 2010 Eyjafjallajökull explosive eruption. Nature. 2010 Nov 18;468(7322):426-30. doi: 10.1038/nature09558. PMID: 21085177.
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Unexpected large eruptions from buoyant magma bodies within viscoelastic crust.

Nature communications

Sigmundsson F, Pinel V, Grapenthin R, Hooper A, Halldórsson SA, Einarsson P, Ófeigsson BG, Heimisson ER, Jónsdóttir K, Gudmundsson MT, Vogfjörd K, Parks M, Li S, Drouin V, Geirsson H, Dumont S, Fridriksdottir HM, Gudmundsson GB, Wright TJ, Yamasaki T.
PMID: 32415105
Nat Commun. 2020 May 15;11(1):2403. doi: 10.1038/s41467-020-16054-6.

Large volume effusive eruptions with relatively minor observed precursory signals are at odds with widely used models to interpret volcano deformation. Here we propose a new modelling framework that resolves this discrepancy by accounting for magma buoyancy, viscoelastic crustal...

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Sigmundsson F, Pinel V, Grapenthin R, et al. Unexpected large eruptions from buoyant magma bodies within viscoelastic crust. Nat Commun. 2020;11(1):2403doi: 10.1038/s41467-020-16054-6.
Sigmundsson, F., Pinel, V., Grapenthin, R., Hooper, A., Halldórsson, S. A., Einarsson, P., Ófeigsson, B. G., Heimisson, E. R., Jónsdóttir, K., Gudmundsson, M. T., Vogfjörd, K., Parks, M., Li, S., Drouin, V., Geirsson, H., Dumont, S., Fridriksdottir, H. M., Gudmundsson, G. B., Wright, T. J., & Yamasaki, T. (2020). Unexpected large eruptions from buoyant magma bodies within viscoelastic crust. Nature communications, 11(1), 2403. https://doi.org/10.1038/s41467-020-16054-6
Sigmundsson, Freysteinn, et al. "Unexpected large eruptions from buoyant magma bodies within viscoelastic crust." Nature communications vol. 11,1 (2020): 2403. doi: https://doi.org/10.1038/s41467-020-16054-6
Sigmundsson F, Pinel V, Grapenthin R, Hooper A, Halldórsson SA, Einarsson P, Ófeigsson BG, Heimisson ER, Jónsdóttir K, Gudmundsson MT, Vogfjörd K, Parks M, Li S, Drouin V, Geirsson H, Dumont S, Fridriksdottir HM, Gudmundsson GB, Wright TJ, Yamasaki T. Unexpected large eruptions from buoyant magma bodies within viscoelastic crust. Nat Commun. 2020 May 15;11(1):2403. doi: 10.1038/s41467-020-16054-6. PMID: 32415105; PMCID: PMC7229005.
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Corrigendum: Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano.

Scientific reports

Spaans K, Hreinsdóttir S, Hooper A, Ófeigsson BG.
PMID: 27624911
Sci Rep. 2016 Sep 14;6:33010. doi: 10.1038/srep33010.

No abstract available.

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Spaans K, Hreinsdóttir S, Hooper A, et al. Corrigendum: Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano. Sci Rep. 2016;6:33010doi: 10.1038/srep33010.
Spaans, K., Hreinsdóttir, S., Hooper, A., & Ófeigsson, B. G. (2016). Corrigendum: Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano. Scientific reports, 633010. https://doi.org/10.1038/srep33010
Spaans, Karsten, et al. "Corrigendum: Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano." Scientific reports vol. 6 (2016): 33010. doi: https://doi.org/10.1038/srep33010
Spaans K, Hreinsdóttir S, Hooper A, Ófeigsson BG. Corrigendum: Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano. Sci Rep. 2016 Sep 14;6:33010. doi: 10.1038/srep33010. PMID: 27624911; PMCID: PMC5022027.
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Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano.

Scientific reports

Spaans K, Hreinsdóttir S, Hooper A, Ófeigsson BG.
PMID: 25992847
Sci Rep. 2015 May 20;5:10285. doi: 10.1038/srep10285.

Many volcanic systems around the world are located beneath, or in close proximity to, ice caps. Mass change of these ice caps causes surface movements, which are typically neglected when interpreting surface deformation measurements around these volcanoes. These movements...

Cite
Spaans K, Hreinsdóttir S, Hooper A, et al. Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano. Sci Rep. 2015;5:10285doi: 10.1038/srep10285.
Spaans, K., Hreinsdóttir, S., Hooper, A., & Ófeigsson, B. G. (2015). Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano. Scientific reports, 510285. https://doi.org/10.1038/srep10285
Spaans, Karsten, et al. "Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano." Scientific reports vol. 5 (2015): 10285. doi: https://doi.org/10.1038/srep10285
Spaans K, Hreinsdóttir S, Hooper A, Ófeigsson BG. Crustal movements due to Iceland's shrinking ice caps mimic magma inflow signal at Katla volcano. Sci Rep. 2015 May 20;5:10285. doi: 10.1038/srep10285. PMID: 25992847; PMCID: PMC4650818.
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Showing 1 to 6 of 6 entries