Háskóli Íslands

An intense seismic swarm is currently taking place under the eastern part of Bárðarbunga. Between 03:04 and 13:00 on August 16th a total of 189 earthquakes occurred (max. M2.9).  The seismic swarm continues and continuous GPS stations have detected deformation that confirm magma movements associated with intrusive activity. No indications of surface magma extrusion beneath the ice cap have been observed. If the activity progresses towards an eruption, a scenario could involve a subglacial, or partly subglacial eruption, at the northwestern part or edge of Vatnajökull, with a jökulhlaup in the Jökulsá á Fjöllum river towards the north.

This is the largest seismic swarm seen in Bárðarbunga since the end of September 1996, in the days leading to the Gjálp eruption.  The area is covered by Vatnajökull and the ice thickness varies from 100-200 at  the caldera rims of Bárðarbunga to over 800 m within the Bárðarbunga caldera. IMO, IES and Civil Protection are monitoring the situation – the seismic activity can be observed at www.vedur.is.

A direct link to the Vatnajökull seismic map is: http://www.vedur.is/skjalftar-og-eldgos/jardskjalftar/vatnajokull/#view=map


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