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Potential Area of Eruption Larger than Before Fagradalsfjall mountain. Photo/Skúli Halldórsson Vala Hafstað Morgunblaðið . He believes that area to include Fagradalsfjall and vicinity, not the area south of the mountain. According to Benedikt Gunnar Ófeigsson, tectonics specialist at the Icelandic Met Office, the magma dyke may have reached a hindrance or constriction under the Nátthagi area, south of Fagradalsfjall. Constant expansion is being registered in the area, and magma continues to flow into the dyke. Benedikt deduces this from the latest satellite picture, analyzed yesterday. Geophysicist Freysteinn Sigmundsson. mbl.is/Kristinn Magnússon The comparison of satellite pictures taken in the past weeks shows tectonic divergence on both sides of the magma dyke, which has formed between the mountains Keilir and Fagradalsfjall, amounting to up to 10 cm on each side, Freysteinn tells

Kristinn magnFreysteinn sigmundssonIcelandic met officeUniversity of iceland institute earth sciencesSouthwest icelandIceland instituteEarth sciencesBenedikt gunnarIn depth iceland news coverageIceland weather forecast and informationஐஸ்லாந்து சந்தித்தார் அலுவலகம்பல்கலைக்கழகம் ஆஃப் ஐஸ்லாந்து நிறுவனம் பூமி அறிவியல்தென்மேற்கு ஐஸ்லாந்துஐஸ்லாந்து நிறுவனம்பூமி அறிவியல்இல் ஆழம் ஐஸ்லாந்து செய்தி பாதுகாப்பு