Skip to main content
Log in

Earthquake swarms at Upptyppingar, north-east Iceland: A sign of magma intrusion?

  • Published:
Studia Geophysica et Geodaetica Aims and scope Submit manuscript

Abstract

In 2007, intense swarms of deep, tectonic earthquakes, amounting to at least 5 300 epicentres, were detected near to Mount Upptyppingar, which forms part of the Kverkfjöll volcano system in Iceland’s Northern Volcanic Zone. Although micro-seismicity is common within such volcanic regions, the Upptyppingar swarms have been more intensive and persistent than any other deep-seated seismicity observed in Iceland. Here we outline the spatial and temporal changes in ongoing seismicity that began in February 2007; in addition, we document enhanced levels of GPS-derived crustal deformation, recorded within 25 km of the area of swarming. Besides displaying spatial clustering, the Upptyppingar micro-earthquakes are noteworthy because: (i) they concentrate at focal depths of 14–22 km; (ii) the swarms comprise brittle-type earthquakes < 2 in magnitude, yielding a b-value of 2.1; and (iii) several of the swarms originate at focal depths exceeding 18 km. Additionally, different parts of the affected region have exhibited seismicity at different times, with swarm sites alternating between distinct areas. The activity moved with time towards east-north-east and to shallower depths. Linear regression approximates the seismicity on a southward-dipping, ∼41° plane. Alongside sustained earthquake activity, significant horizontal displacement was registered at two permanent GPS stations in the region. High strain rates are required to explain brittle fracturing under visco-elastic conditions within the Earth’s crust; similarly, intense, localised deformation at considerable depth is necessary to reconcile the measured surface deformation. Such remarkable seismicity and localised deformation suggests that magma is ascending into the base of the crust.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Arnadottir T., Lund B., Jiang W., Geirsson H., Sturkell E., Sigmundsson F., Einarsson P. and Sigurdsson T., 2007. Rapid uplift and plate spreading observed by GPS in Iceland. EGU General Assembly 2007, Vienna, Austria. Geophysical Research Abstracts, 9, EGU2007-A-07053.

  • Ágústsson, K. and Flóvenz, Ó.G., 2005. The thickness of the seismogenic crust in Iceland and its implications for geothermal systems. Proceedings of the World Geothermal Congress 2005, 24–29 April 2005, Antalya, Turkey (http://iga.igg.cnr.it/geoworld/pdf/WGC/2005/0743.pdf).

  • Ágústsson K. and Halldórsson P., 2005. Seismic hazard in the Hengill area based on the SIL earthquake catalogue — first results. Report 05015, Icelandic Meteorological Office, 39 pp.

  • Björnsson A., Eysteinsson H. and Beblo M., 2005. Crustal formation and magma genesis beneath Iceland: Magnetotelluric constraints. Plates, Plumes and Paradigms, Special Paper 388, Geological Society of America, 665–686.

  • Böðvarsson R., Rögnvaldsson S.T., Jakobsdóttir S.S., Slunga R. and Stefánsson R., 1996. The SIL data acquisition and monitoring system. Seismol. Res. Lett., 67, 35–46.

    Google Scholar 

  • Boettcher M.S., Hirth G. and Evans B., 2007. Olivine friction at the base of oceanic seismogenic zones. J. Geophys. Res., 112, B01205, doi: 10.1029/2006JB004301.

    Article  Google Scholar 

  • Davidson C., Schmid S.M. and Hollister L.S., 1994. Role of melt during deformation in the deep crust. Terra Nova, 6, 133–142.

    Article  Google Scholar 

  • Dell’Angelo L.N. and Tullis J., 1988. Experimental deformation of partially melted granitic aggregates. J. Metamorph. Geol., 6, 6495–6515.

    Google Scholar 

  • DeMets C., Gordon R.G., Argus D.F. and Stein S., 1994. Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions. Geophys. Res. Lett., 21, 2191–2194.

    Article  Google Scholar 

  • De Zeeu-van Dalfsen E., Pedersen R. and Sigmundsson F., 2004. Satellite radar interferometry 1993–1999 suggests deep accumulation of magma near the crust-mantle boundary at the Krafla volcanic system. Geophys. Res. Lett., 31, L13611, doi: 10.1029/2004GL020059.

    Article  Google Scholar 

  • Einarsson P. and Sæmundsson K., 1987. Earthquake epicenters 1982–1985 and volcanic systems in Iceland (map). In: Sigfússon Th.I. (Ed.), Í Hlutarins Eðli. Festschrift for Thorbjörn Sigurgeirsson, Menningarsjóður, Reykjavík.

    Google Scholar 

  • Flóvenz O.G. and Sæmundsson K., 1993. Heat flow and geothermal processes in Iceland. Tectonophysics, 225, 123–138.

    Article  Google Scholar 

  • Geirsson H., Árnadóttir T., Bennett R., LaFemina P., Jónsson S., Hreinsdóttir S., Holland A., Deutscher J., Ingvarsson T., Sturkell E. and Villemin T., 2007. A high-rate continuous GPS network in Iceland for crustal deformation research. Eos Trans. AGU, 88, 1228.

    Google Scholar 

  • Geirsson H., Árnadóttir T., Völksen C., Jiang W., Sturkell E., Villemin T., Einarsson P., Sigmundsson F. and Stefánsson R., 2006. Current plate movements across the Mid-Atlantic Ridge determined from 5 years of continuous GPS measurements in Iceland. J. Geophys. Res., 111, B09407, doi: 10.1029/2005JB003717.

    Article  Google Scholar 

  • Grapenthin R., Sigmundsson F., Geirsson H., Árnadóttir T. and Pinel V., 2006. Icelandic rhythmics: annual modulation of land elevation and plate spreading by snow load. Geophys Res. Lett., 33, L24305, doi: 10.1029/2006GL028081.

    Article  Google Scholar 

  • Jakobsdóttir S.S., 2008. Seismicity in Iceland: 1994–2007. Jökull, 58, 75–100.

    Google Scholar 

  • Jurewics S.R. and Watson E.B., 1985. The distribution of partial melt in a granitic system: The application of liquid phase sintering theory. Geochim. Cosmochim. Acta, 49, 1109–1121.

    Article  Google Scholar 

  • McKenzie D., Jackson J. and Priestley K., 2005. Thermal structure of oceanic and continental lithosphere. Earth Planet. Sci. Lett., 233, 337–349.

    Article  Google Scholar 

  • Mogi K., 1962. Magnitude-frequency relations for elastic shocks accompanying fractures of various materials and some related problems in earthquakes. Bull Earthquake Res. Inst. Univ. Tokyo, 40, 831–853.

    Google Scholar 

  • Needleman A. and Tvergaard V., 2000. Numerical modeling of the ductile-brittle transition. Int. J. Fract., 101, 73–97.

    Article  Google Scholar 

  • Ófeigsson B.G., 2008. Crustal Movements 2005–2007 in the Kárahnjúkar Area, NE-Iceland, in Relation to Formation of the Hálslón Water Reservoir. Report 0801, Nordic Volcanological Center, Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland.

    Google Scholar 

  • Pagli C., Sigmundsson F., Árnadóttir T., Einarsson P. and Sturkell E., 2006. Deflation of the Askja volcanic system: constraints on the deformation source from combined inversion of satellite radar interferograms and GPS measurements. J. Volcanol. Geotherm. Res., 152, 97–108.

    Article  Google Scholar 

  • Pedersen R. and Sigmundsson F., 2004. InSAR based sill model links spatially offset areas of deformation and seismicity for the 1994 unrest episode at Eyjafjallajökull volcano, Iceland. Geophys. Res. Lett., 31, L14610, doi: 10.1029/2004GL020368.

    Article  Google Scholar 

  • Pedersen R. and Sigmundsson F., 2006. Temporal development of the 1999 intrusive episode in the Eyjafjallajökull volcano, Iceland, derived from InSAR images. Bull. Volcanol., 68, 377–393.

    Article  Google Scholar 

  • Pinel V., Sigmundsson F., Sturkell E., Geirsson H., Einarsson P., Gudmundsson M.T. and Högnadóttir T., 2007. Discriminating volcano deformation due to magma movements and variable surface loads: application to Katla subglacial volcano, Iceland. Geophys. J. Int., 169, 325–338.

    Article  Google Scholar 

  • R Development Core Team, 2008. R: A Language and Environment for Statistical Computing. R Foundation for Statistical Computing, Vienna, Austria (http://www.R-project.org).

    Google Scholar 

  • Roman D.C., De Angelis S., Latchman J.L. and White R., 2008. Patterns of volcanotectonic seismicity and stress during the ongoing eruption of the Soufrière Hills Volcano, Montserrat (1995–2007). J. Volcanol. Geotherm. Res., 173, 230–244.

    Article  Google Scholar 

  • Rögnvaldsson S.T. and Slunga R., 1993. Routine fault plane solutions for local and regional networks: a test with synthetic data. Bull. Seismol. Soc. Amer., 11, 1247–1250.

    Google Scholar 

  • Sánchez J.J., Gomez D.M., Torres R.A., Calvache M.L., Ortega A., Ponce A.P., Acevedo A.P., Gil-Cruz F., Londono J.M., Rodriguez S.P., Patino J.J. and Bohórquez O.P., 2005. Spatial mapping of the b-value at Galeras volcano, Colombia, using earthquakes recorded from 1995 to 2002. Earth Sci. Res. J., 9, 30–36.

    Google Scholar 

  • Sánchez J.J., McNutt S.R., Power J.A. and Wyss M., 2004. Spatial variations in the frequency-magnitude distribution of earthquakes at Mount Pinatubo volcano. Bull. Seismol. Soc. Amer., 94, 430–438.

    Article  Google Scholar 

  • Scholz C.H., 1968. The frequency-magnitude relation of microfracturing in rock and its relation to earthquakes. Bull. Seismol. Soc. Amer., 58, 399–415.

    Google Scholar 

  • Schorlemmer D., Weimer S. and Wyss M., 2005. Variations in earthquake-size distribution across different stress regimes. Nature, 437, 539–542.

    Article  Google Scholar 

  • Sella G.F., Dixon T. and Mao A., 2002. REVEL: A model for recent plate velocities from space geodesy. J. Geophys. Res., 107, Art.No. 2081, doi: 10.1029/2000JB00033.

  • Sigbjarnarson G., 1993. Northern Vatnajökull II. Stratigraphy and geological map (Norðan Vatnajökuls II. Jarðlagaskipan og jarðfræðikort). Náttúrufræðingurinn, 63, 201–217 (in Icelandic with English summary).

    Google Scholar 

  • Sigmundsson F., Einarsson P., Rögnvaldsson S.T., Foulger G.R., Hodgkinson K.M. and Thorbergsson G., 1997. The 1994–1995 seismicity and deformation at the Hengill triple junction, Iceland: Triggering of earthquakes by minor magma injection in a zone of horizontal shear stress. J. Geophys. Res., 102, 15151–15161.

    Article  Google Scholar 

  • Sigurbjarnarson G., 1988. Description of geological map units (Krepputunga og Brúardalir). Lýsing á korteiningum jarðfræðikorts. Orkustofnun, OS-88038/VOD-06 (in Icelandic).

  • Slunga R. 1981. Earthquake source mechanism determination by use of body-wave amplitudes — an application to Swedish earthquakes. Bull. Seismol. Soc. Amer., 71, 25–35.

    Google Scholar 

  • Slunga R., Rögnvaldsson S.T. and Böðvarsson R., 1995. Absolute and relative locations of similar events with application to microearthquakes in southern Iceland. Geophys. J. Int., 123, 409–419.

    Article  Google Scholar 

  • Soosalu H., White R.S., Key A.J., Knox C., Einarsson P. and Jakobsdóttir S., 2008. Lower-crustal earthquakes reflect magma movements beneath the north Iceland rift near Askja. EGU General Assembly 2008, Vienna, Austria. Geophysical Research Abstracts, 10, EGU2008-A-07323.

  • Stefánsson R., Bergerat F., Bonafede M., Böðvarsson R., Crampin S., Einarsson P., Feigl K.L., Goltz C., Guðmundsson Á., Roth F., Sigbjörnsson R., Sigmundsson F., Suhadolc P., Wyss M., Angelier J., Árnadóttir Th., Belardinelli M.E., Clifton A., Dubois L., Guðmundsson G.B., Halldórsson P., Hjaltadóttir S., Lund B., Ólafsson S., Richwalski S., Sens-Schönfelder C., Slunga R., Tryggvason A., Vogfjörð K.S. and Thorkelsson B., 2005. PREPARED — Second Periodic Report. February 1, 2004–January 31, 2005. Report 05007, Icelandic Meteorological Office, Reykjavik, Iceland, 107 pp.

    Google Scholar 

  • Sturkell E., Sigmundsson F. and Slunga R., 2006. 1983–2003 decaying rate of deflation at Askja caldera: Pressure decrease in an extensive magma plumbing system at a spreading plate boundary. Bull. Volcanol., 68, 727–735.

    Article  Google Scholar 

  • Sæmundsson K., 1979. Outline of the geology of Iceland. Jökull, 29, 7–28.

    Google Scholar 

  • Thorarinsson S. and Sigvaldason G.E., 1962. The eruption in Askja, 1961; a preliminary report. Am. J. Sci., 260, 641–651.

    Google Scholar 

  • Vilhjálmsson A.M., Flóvenz Ó.G., Karlsdóttir R., Árnason K., Eysteinsson H. and Sæmundsson K., 2008. Resistivity survey supports magmatic activity at Upptyppingar N-Iceland. IAVCEI 2008 General Assembly, Reykjavík, Iceland, Abstract 2-f P07 (http://www.iavcei.org/IAVCEI.htm).

  • Warren N.W. and Latham G.V., 1970. An experimental study of thermally induced microfracturing and its relation to volcanic seismicity. J. Geophys. Res., 75, 4455–4464.

    Article  Google Scholar 

  • Wessel P. and Smith W.H.F., 1998. New, improved version of Generic Mapping Tools released. EOS Trans. AGU, 79, 579.

    Article  Google Scholar 

  • Wiemer S. and Benoit J., 1996. Mapping the b-value anomaly at 100 km depth in the Alaska and new Zealand subduction zones. Geophys. Res. Lett., 23, 1557–1560.

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to S. S. Jakobsdóttir.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Jakobsdóttir, S.S., Roberts, M.J., Guđmundsson, G.B. et al. Earthquake swarms at Upptyppingar, north-east Iceland: A sign of magma intrusion?. Stud Geophys Geod 52, 513–528 (2008). https://doi.org/10.1007/s11200-008-0035-x

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s11200-008-0035-x

Keywords

Navigation