UNSTOPPABLE LAVA BREAKS DOWN INTO NÁTTHAGI! Rapid lava flows at 01:35 am, .
“Why is Fagradalsfajall so different? The first sign that the eruption was special was the deep origin and primitiveness of its magma composition. Scientists who have studied the lava erupted from the volcano have reported its remarkable characteristics. It rises up from a depth of 15-20 km in the mantle. Several markers of how primitive the magma was turned out to be remarkably high.
Additionally this eruption has broken a very long volcanic dormancy of ~800 years in the entire area of the Rekyjanes Peninsula and the Western Volcanic Zone of Iceland, since the Reyjanes Fires and the massive Hallmundarhraun eruptions took place. This could have consequences regarding the amount of magma available in the area.
The most striking aspect of the eruption is Ragnar, the name that some have been using for the currently active vent. Its size is enormous, over 100 meters tall. Typical eruptions of the Rekjanes Peninsula make cones that are 10-20 meters high, some may perhaps reach up to 50 meters, b
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UNSTOPPABLE LAVA BREAKS DOWN INTO NÁTTHAGI! Rapid lava flows at 01:35 am, .