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Another volcanic clap could take place in Iceland in a matter of twenty-four hour period or weeks , authority have warned .
agree to experts with the Icelandic Met Office ( IMO ) , 230 million three-dimensional foot ( 6.5 million three-dimensional meters ) of magma has now participate the chamber sit beneath Svartsengi , around 2.5 miles ( 4 klick ) magnetic north of the township of Grindavík — mean the bulk is fast set about levels seen before the bam on Jan. 14 , when two scissure opened on the outskirts of the Ithiel Town .
The last eruption on Iceland’s Reykjanes Peninsula took place on Jan. 14, with two fissures opening near Grindavík.
According to atranslated statementfrom the IMO , the bulk of magma in the sleeping room will accomplish the same point seen in the last volcanic eruption within the next two workweek .
Unlike the previous eruptions , the warning time this time could be as little as one minute due to few earthquakes in the progress - up , IMO representative drop a line . " In case of repeated magma flow , it is likely that the path for the magma will be easier and this will be accompanied by less seismal activity , " they drop a line in the assertion .
Benedikt Ófeigsson , foreland of deformation mensuration at the IMO , toldIceland ’s internal broadcaster RUVthat the most likely station a crack will come out is between Stóra - skógafell and Hagafell — 3.7 miles and 1.2 mile ( 5.9 km and 2 km ) , severally , nor'-east of Grindavík .
An updated map shows the risk zones for another eruption on the Reykjanes Peninsula.
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" It is not likely that it will take fire inside the Ithiel Town and in fact the geological data does not indicate that , but nothing is out of the interrogative sentence so we have to keep it in as a opening , " he say . " mayhap it ’s fourth dimension for magma not to get this far in the south again . However , we do not have any measure that tell us when enough is enough , so we have to take that the magma can go south again in the guidance of Grindavík . "
A 9.3 naut mi ( 15 km ) magma dike — a near - vertical tunnel run from the magma chamber beneath — formed beneath the Reykjanes Peninsula in October and November last year . Iterupted on Dec. 18 , witha wall of lavaflowing from a 2.5 - mile ( 4 km ) fissure .
Lava flows from a fissure that opened on Jan. 14 near the town of Grindavík destroyed three houses.
After a period of quiet , the vent erupted again on Jan. 14 , whentwo fissures opened up just northwards of Grindavík . Lava course from the lowly eruption entered the Ithiel Town and destroy houses . Since then , the land around Svartsengihas continued to rise up , indicating magma is still accumulate beneath the open and that this wave of volcanic activity is not over .
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— Tonga volcano bam was fueled by 2 merging sleeping room that are still brim with magma
It ’s not possible to anticipate on the button where an eruption could take topographic point . Carmen Solana , associate prof of volcanology and hazard communication at the University of Portsmouth in the U.K.,previously tell Live Sciencethat magma will rise to the surface through the weak points in Earth ’s impertinence . " We do n’t fuck where the next one is going to bechance and we do n’t know how large it will be , " she said . " That ’s the sad part of vulcanology — we know that something is going to happen and you know around where , but you’re able to not nail with that preciseness . "
An update hazard map from the IMO shows the area running north - northwestern United States of Grindavík is likely at great jeopardy from a crack opening without poster . The town of Grindavík is view to be at " considerable hazard , " with lava flows and land collapse possible .
