Skútustaðagígar Pseudocraters

Background

History & Background

Skútustaðagígar Pseudocraters is part of Iceland's dramatic volcanic landscape in North Iceland, shaped by millennia of eruptions along the Mid-Atlantic Ridge. Iceland's volcanic history stretches back 16-18 million years, with the island itself emerging from the ocean through volcanic activity. The geological formations here tell the story of fire and ice — of eruptions that reshaped the land and glaciers that carved it further. Historical eruptions in this region have been documented in Icelandic annals dating back to the 12th century. The interplay between volcanic heat and Arctic climate has created a unique ecosystem found nowhere else on Earth, making sites like this invaluable for both scientific research and tourism.

Skútustaðagígar are remarkable pseudocraters on the southern shore of Lake Mývatn, formed about 2,300 years ago when flowing lava encountered wetlands, causing steam explosions. Unlike true volcanic craters, these weren't formed by eruptions from beneath. A circular walking path allows visitors to explore the crater formations up close. The area is part of the Lake Mývatn nature reserve and protects important birdlife.