Askja | Bárdarbunga | Blafell | Blafjall | Brennisteinsfjöll | Burfell | Eldey | Eríksjokull | Esjufjöll | Eyafjallajökull | Fjallgardar Ridge | Fremrinamur | Gaesafjoll | Geysir | Grensdalur | Grímsnes | Grímsvötn | Heiðarsporðar | Hekla | Helgrindur | Hengill | Herdubreid | Hlodufell | Hofsjökull | Hreppar | Hrómundartindur | Hrutfell | Hveravellir | Katla | Kerlingarfjöll | Kistufell | Kolbeinsey Ridge | Krafla | Krísuvík | Kverkfjöll | Lambafjoll | Langjökull volcano | Ljósufjöll | Loki-Fögrufjöll volcano | Lyngdalsheidi | Lysuhóll | Ok | Öraefajökull | Prestahnukur | Reykjanes | Sellandafjall | Snaefellsjökull | Strutur | Theistareykjarbunga | Thordarhyrna | Thorisjokull | Tindfjallajökull | Tjörnes Fracture Zone | Torfajökull | Tungnaarfjoll | Tungnafellsjökull | Valdalda | Vatnafjöll | Vestmannaeyjar (Heimaey + Surtsey)

Iceland, the land of ice and fire, is a true paradise for volcanologists. In few places on earth, geology and human history are so closely connected to volcanism as on Iceland. The island owns its existence to a large volcanic hot spot sitting on a mid-oceanic ridge, a unique setting. The plate boundary between the American and Eurasian tectonic plates crosses Iceland from south to North and the spreading process can be directly measured and observed on land.