Hengill


Hengill volcano, geothermal heat & Iceland's renewable energy 


The Hengill volcano mountain range and geothermal field are located in south-western Iceland. The volcano system consists of a series of basaltic fissure vents, crater rows and small shield volcanoes. It lies at the triple junction of the Reykjanes Peninsula volcanic zone, the western volcanic zone and the south Iceland seismic zone. Hengill’s highest peak is 806 m, formed of volcanic ash.

The plateau to the south of the range, Hellisheiði (Hellisheidi), is covered with layers of old and new lava from Hengill’s postglacial lava flows. The latest eruption happened in 1000 AD when Iceland was in the process of Christianization. Kristni Saga, in the Book of Icelanders, makes specific mention of the eruption taking place, just as the issue of acceptance of Christianity is being fiercely debated at the Alþingi (Althing), Icelandic open-air Parliament at Þingvellir (Thingvellir), Parliament Plains. Consequently, the lava field was named Kristnitökuhraun, “Christianity-taking-lava”. Radiocarbon dating has since established that the eruption actually took place at a 5 km distance from Thingvellir at a vent in the Brennisteinsfjöll (Brennisteinsfjoll) volcanic area, on Reykjanes Peninsula. 

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