Vatnafjöll
Vatnafjöll (Script error: No such module "IPA".) is a Script error: No such module "convert". long, Script error: No such module "convert". wide basaltic fissure vent system that is south-east of Hekla, Iceland. It includes from the north towards the south the hills of Innri-Vatnafjöll at Template:Cvt high, Fremri-Vatnafjöll at Template:Cvt and Vatnafjallarani at Template:Cvt as the main Vatnafjöll edifice,[1] at a distance of about Template:Cvt from Hekla.[2]Template:Rp It is part of the same system as Hekla,[3] and the term Hekla-Vatnafjöll volcanic system has been used to describe it.[4] More than two dozen eruptions have occurred at Vatnafjöll during the Holocene Epoch. Vatnafjöll has not erupted during the last 1100 years.[5]Template:Rp While these eruptions were predominantly effusive some basaltic tephra deposits have been found up to Template:Cvt away.[6]
A Template:M with an epicenter near the main Vatnafjöll edifice occurred on 25th May, 1987,[5]Template:Rp where the transform South Iceland seismic zone meets the East volcanic zone of Iceland. Later analysis has suggested that initiation was from strain relief but a subsurface dyke intrusion then occurred over the next 3 days.[2]Template:Rp
See also
References
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