Kverkfjöll
Kverkfjoll
Stratovolcano · Iceland · 1930m

- Type
- Stratovolcano
- Country
- Iceland
- Region
- Atlantic Ocean Volcanic Regions / Iceland Neovolcanic Rift Volcanic Province
- Elevation
- 1930m
- Coordinates
- 64.653, -16.647
- Last eruption
- 1968
- Tectonic setting
- Rift zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Basalt / Picro-Basalt
Geological summary
Kverkfjöll is a large subglacial volcano at the NE end of the Vatnajökull icecap. Two elliptical ice-filled calderas, each about 8 x 5 km in size, have been identified. An associated fissure swarm can be traced 60 km to the NE. A half dozen ridges of subglacially erupted pillow lavas are now exposed and extend beyond the glacial icecap to the NE. Subglacial historical eruptions have been recorded since the mid-17th century. Several other historical eruptions once attributed to Kverkfjöll are now thought to have originated from Bárdarbunga volcano to the west.
From Wikipedia
Kverkfjöll is a potentially active central volcano, fissure swarm, and associated mountain range situated on the northern border of the glacier Vatnajökull in Iceland.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 1968VEI 0Observed1968-05-23 – 1968-06-16
- 1959VEI 1Observed1959-07-02 – Ongoing
- 1929VEI 1Observed1929-01 – 1929-02Hveradalur area
- 1729VEI 1Observed1729-02-15 – Ongoing
- 1729VEI 1Observed1729-08 – Ongoing
- 1655VEI 0Observed1655-04-15 – Ongoing
- 5000 BCE (±1000 yrs)VEI ?Geological estimateBCE 5000 – OngoingKrepputunguhraun, Kverfjallahraun
- 7050 BCEVEI ?Geological estimateBCE 7050 – OngoingArnadalsoldugjoska
External links
⚠ For reference only. Not for emergency response.