Bulletin of Volcanology

, 71:961

The fissure swarm of the Askja volcanic system along the divergent plate boundary of N Iceland


  • Ásta Rut Hjartardóttir
    • Institute of Earth SciencesUniversity of Iceland
    • Institute of Earth SciencesUniversity of Iceland
  • Haraldur Sigurdsson
    • Graduate School of OceanographyUniversity of Rhode Island
Research Article

DOI: 10.1007/s00445-009-0282-x

Cite this article as:
Hjartardóttir, Á.R., Einarsson, P. & Sigurdsson, H. Bull Volcanol (2009) 71: 961. doi:10.1007/s00445-009-0282-x


Divergent plate boundaries, such as the one crossing Iceland, are characterized by a high density of subparallel volcanic fissures and tectonic fractures, collectively termed rift zones, or fissure swarms when extending from a specific volcano. Volcanic fissures and tectonic fractures in the fissure swarms are formed during rifting events, when magma intrudes fractures to form dikes and even feeds fissure eruptions. We mapped volcanic fissures and tectonic fractures in a part of the divergent plate boundary in northern Iceland. The study area is ~1,800 km2, located within and north of the Askja central volcano. The style of fractures changes with distance from Askja. Close to Askja the swarm is dominated by eruptive fissures. The proportion of tectonic fractures gets larger with distance from Askja. This may indicate that magma pressure is generally higher in dikes close to Askja than farther away from it. Volcanic fissures and tectonic fractures are either oriented away from or concentric with the 3–4 identified calderas in Askja. The average azimuth of fissures and fractures in the area deviates significantly from the azimuth perpendicular to the direction of plate velocity. As this deviation decreases gradually northward, we suggest that the effect of the triple junction of the North American, Eurasian and the Hreppar microplate is a likely cause for this deviation. Shallow, tectonic earthquakes in the vicinity of Askja are often located in a relatively unfractured area between the fissure swarms of Askja and Kverkfjöll. These earthquakes are associated with strike-slip faulting according to fault plane solutions. We suggest that the latest magma intrusions into either the Askja or the Kverkfjöll fissure swarms rotated the maximum stress axis from being vertical to horizontal, causing the formation of strike-slip faults instead of the dilatational fractures related to the fissure swarms. The activity in different parts of the Askja fissure swarm is uneven in time and switches between subswarms, as shown by a fissure swarm that is exposed in an early Holocene lava NW of Herðubreið but disappears under a younger (3500–4500 BP) lava flow. We suggest that the location of inflation centres in Askja central volcano controls into which part of the Askja fissure swarm a dike propagates. The size and amount of fractures in the Kollóttadyngja lava shield decrease with increasing elevation. We suggest that this occurred as the depth to the propagating dike(s) was greater under central Kollóttadyngja than under its flanks, due to topography.


Askja volcanoFissure swarmMid-Atlantic plate boundaryIcelandRift zoneNorthern volcanic zoneRifting

Supplementary material

445_2009_282_Fig1_ESM.tif (15 mb)
High resolution image (TIFF 15376 kb)
445_2009_282_Fig2_ESM.tif (17.3 mb)
High resolution image (TIFF 17664 kb)
445_2009_282_MOESM3_ESM.doc (38 kb)
Table S1The width of fractures (in meters) found by inspection on ground in the northeastern subswarm of the Askja fissure swarm, across a given profile. The profile is located east of Mt. Eggert and is perpendicular to the fissure swarm. The area is situated within UTM zone 27. (DOC 38 kb)

Copyright information

© Springer-Verlag 2009