The Dimmuborgir area consist of a massive, collapsed lava tube formed by a lava lake flowing in from a large eruption in the Threngslaborgir and Lúdentarborgir crater row to the East, about 2300 years ago. At Dimmuborgir, the lava pooled over a small lake. As the lava flowed across the wet sod, the water of the marsh started to boil, the vapour rising through the lava forming lava pillars from drainpipe size up to several meters in diameters. As the lava continued flowing towards lower ground in the Mývatn area, the top crust collapsed, but the hollow pillars of solidified lava remained. The lava lake must have been at least 10 meters deep, as estimated by the tallest structures still standing. The lava flow surface remains partly intact around the Dimmuborgir area, so that the Dimmuborgir itself sits below the surrounding surface area. The area is characterised by large hollow cell- or chamber-like structures formed around bubbles of vapour, and some dramatically standing lava pillars. Several of the chambers and pillar bases are large enough to house humans, giving rise to the term "castles" (borgir).