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Krafla is a volcanic caldera of about 10 km in diameter with a 90 km long fissure zone, in the north of Iceland in the Mývatn region. Its highest peak reaches up to 818 m and it is 2 km in depth. There have been 29 reported eruptions in recorded history.
A girl is standing near the steaming Krafla volcanic area at Hverir
|Elevation||650 m (2,130 ft)|
|Last eruption||September 1984|
Krafla includes the crater Víti, one of two well-known craters by this name in Iceland (the other is in Askja). The Icelandic word "víti" means "hell". In former times, people often believed hell to be under volcanoes. Víti has a green lake inside of it.
The Mývatn fires occurred between 1724–1729, when many of the fissure vents opened up. The lava fountains could be seen in the south of the island and a lava flow destroyed three farms near the village of Reykjahlíð, although nobody was harmed.
Between 1975 and 1984 there was a volcanic episode within the Krafla volcano. It involved nine volcanic eruptions and fifteen uplift and subsidence events. This interrupted some of the Krafla drillfields. During these events a large magma chamber emerged. This has been identified by analysing the seismic activity.
Since 1977 the Krafla area has been the source of the geothermal energy used by a 60 MWe power station. A survey undertaken in 2006 indicated very high temperatures at depths of between 3 and 5 kilometres and these favourable conditions have led to the development of the first well from the Iceland Deep Drilling Project (IDDP), that found magma only 2.1 km deep.
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