Observations of Deformation

Volcano number:372050
Geodetic measurements?Yes
Deformation observation?Yes
Measurement method(s):InSAR, Tiltmeter
Duration of observation:Continuous
Inferred cause(s) of deformation:Faulting/tectonics
Characteristics of deformation:

Scheiber-Enslin et al. (2011) present GPS derived horizontal velocity field in southern Iceland covering the period 1994–2006, new InSAR analyses for the periods 1993–2000 and 2003–2007.
The authors results indicate a decrease in spreading rate from northeast (15 mm yr−1) to southwest (9 mm yr−1) across the Torfajökull caldera and the intersection of the South Iceland Seismic Zone and EVZ, consistent with the propagating ridge model. 

Reference(s):Scheiber-Enslin, S. E., LaFemina, P. C., Sturkell, E., Hooper, A. J., & Webb, S. J. (2011). Geodetic investigation of plate spreading along a propagating ridge: the Eastern Volcanic Zone, Iceland. Geophysical Journal International, 187(3), 1175-1194.
Smithsonian Institution Global Volcanism Program
Location:63.92, -19.17
REST API endpoint (JSON):

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