Trölladyngja
Template:Short description Template:For Template:Infobox mountain Situated in the Ódáðahraun lava field, Trölladyngja ({{#invoke:IPA|main}}) is the biggest of the Icelandic shield volcanoes,<ref name="GTI">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> reaching a height of Template:Convert above sea level, and rising almost Template:Cvt above the surrounding desert and lava fields.<ref name=kortasja /> It part of the Bárðarbunga volcanic system and has a volume of Template:Cvt with some extensive lava flows to the north of Bárðarbunga.<ref name=CIV>{{#invoke:citation/CS1|citation |CitationClass=web }}Template:Rp</ref>
It is about Template:Cvtin diameter and its inclination is 4 to 5° in the lower slopes, but 6 to 8° at higher elevations.<ref name="AJS">Template:Cite journalTemplate:Rp</ref> Its oblong crater is about Template:Cvt in length, Template:Cvt broad, and about Template:Cvt deep.<ref name=kortasja />
Most of its tholeiitic basalt lava fields have flowed in a northerly direction, and the definite lava field has been dated at less than 4500 years old.<ref name=CIVm>{{#invoke:citation/CS1|citation |CitationClass=web }}Template:Rp</ref> Composition studies allow the separation of Trölladyngja lavas with their Bárðarbunga associations from other nearby older and younger Bárðarbunga basaltic lavas.<ref>Template:Cite thesisTemplate:Rp</ref> This includes a Bárðarbunga volcanic system origin lava field branch, that possibly erupted from the fissure swarm south of Trölladyngja before 8000 years ago, that reached the valley of Bárðardalur, a distance of roughly Template:Cvt and quite close to the northern Iceland sea coast.<ref name=CIVm /> The shield volcano itself is situated north of latitude 64.7° where the strike direction of the fissure swarms formed in the last 10 million years and the 2014 dyke intrusion from Bárðarbunga towards the north have the orientation of the Northern volcanic zone.<ref>Template:Cite journalTemplate:Rp</ref> The Bárðarbunga central volcano to the south is definitely in the Eastern volcanic zone.
Reports of an eruption in 1961 at Trölladyngja are most likely attributed to nearby Askja Caldera, which erupted the same year.<ref name="GTI" /><ref name="AJS" /> A potential confusion also exists geographically as in the distant past the name Trölladyngja had been used by some when writing about the Askja (Dynjufjöll, Dyngjufjall) volcanic system <ref>Template:Cite gvp</ref> The volcano can now be definitely assigned to the Bárðarbunga volcanic system.<ref name=GVP>Template:Cite gvp</ref><ref name=CIV /> The volcano and its lava flows overlay older lava that is about 8000 years old.<ref>Template:Cite journal</ref>