Loki-Fögrufjöll
Encyclopedia
Loki-Fögrufjöll is a volcano
under the Vatnajökull
glacier.
The volcano is found within the Bárðarbunga
fissure system, but is independent of Bárðarbunga itself.
The last confirmed eruption was in 1910 when Tephra
was erupted, but may also have had subglacial eruptions in, 1986, 1991, 2006 and 2008
Volcano
2. Bedrock3. Conduit 4. Base5. Sill6. Dike7. Layers of ash emitted by the volcano8. Flank| 9. Layers of lava emitted by the volcano10. Throat11. Parasitic cone12. Lava flow13. Vent14. Crater15...
under the Vatnajökull
Vatnajökull
Vatnajökull is the largest glacier in Iceland. It is located in the south-east of the island, covering more than 8% of the country.-Size:With an area of 8,100 km², Vatnajökull is the largest ice cap in Europe by volume and the second largest in area Vatnajökull is the largest glacier in...
glacier.
The volcano is found within the Bárðarbunga
Bárðarbunga
Bárðarbunga is an Icelandic stratovolcano located under the ice cap of Vatnajökull glacier, rising to 2,009 m above sea level, making it the second highest mountain in Iceland, just about 101 m lower than Hvannadalshnjúkur....
fissure system, but is independent of Bárðarbunga itself.
The last confirmed eruption was in 1910 when Tephra
Tephra
200px|thumb|right|Tephra horizons in south-central [[Iceland]]. The thick and light coloured layer at center of the photo is [[rhyolitic]] tephra from [[Hekla]]....
was erupted, but may also have had subglacial eruptions in, 1986, 1991, 2006 and 2008