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Global Volcanism Program | Image GVP-05074

The Hengill volcanic system, mostly located SW of Thingvallavatn lake, consists of a series of NE-SW-trending fissure vents, crater rows, and small shield volcanoes occupying a strongly faulted graben.  This view looks NE from the margin of a graben containing Hengill lava at Thingvellir, the site of Iceland's old parliament.  The latest eruption of the Hengill volcanic system was radiocarbon dated at about 1900 years before present.  Geothermally heated greenhouses, hot springs, and geysers are found at Hveragerdi.   Copyrighted photo by Katia and Maurice Krafft.

The Hengill volcanic system, mostly located SW of Thingvallavatn lake, consists of a series of NE-SW-trending fissure vents, crater rows, and small shield volcanoes occupying a strongly faulted graben. This view looks NE from the margin of a graben containing Hengill lava at Thingvellir, the site of Iceland's old parliament. The latest eruption of the Hengill volcanic system was radiocarbon dated at about 1900 years before present. Geothermally heated greenhouses, hot springs, and geysers are found at Hveragerdi.

Copyrighted photo by Katia and Maurice Krafft.

Copyrighted image used with permission. All Rights Reserved. Contact photographer for any usage requests.


Hengill