Háskóli Íslands

Eruption at Grímsvötn Volcano, 18 - 28 December 1998

An eruption began within the caldera of the subglacial Grimsvötn volcano, Vatnajökull ice cap in Central Iceland, at 09:20 on December 18.  Ten minuets later, around 9:30, an eruption plume was observed.  The eruption penetrated through the Grimvötn subglacial caldera lake and its ice shelf, however not from great depth.  The eruption vents were on a 1300 m long east-west eruptive fissure located on the southern caldera fault, similar as eruption in 1934 and 1983. On the initial day of the eruption, a continuous eruption plume extended to elevation of 10 km. On that day, the eruption plume could be seen from large distances.  It was well observed from Reykjavik, the capital of Iceland, located 200 km from the eruptive site.
 Photo: Freysteinn Sigmundsso


 Photo: Freysteinn Sigmundsson
The eruption was preceded by a mild increase in seismic activity during the last few weeks. A small earthquake swarm occurred at 22 h on December 17, and a sharp increase in earthquake activity began at 03:30 on December 18. This activity was replaced by continuous tremor at 09:20 marking the beginning of the eruption.
Eruption tremor stopped around 14:00 on December 28, and this is considered to mark the end of the eruption. No activity was observed after that.

The eruption occurred 10 km south of the 1996 eruption in Vatnajökull (Gudmundsson et al., 1997) that caused a catastrophic outburst flood from the Vatnajökull glacier.  This time no major flood occurred, because water was not flowing towards the Grimsvötn caldera lake; rather a small amount of the Grimsvötn ice shelf near the eruption site melted

 

 

Map source:
Björnsson, H., Pálsson, F. and Guðmundsson, M.T. 1992
Vatnajökull, northwestern part, 1:100.000
Glacier surface.
Science Institute, University of Iceland

Location of eruption:
64°24.06´ North
17°20.19´ Wes


 

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