The Dimmuborgir area consist of a massive, collapsed lava tube formed
by a lava lake flowing in from a large eruption out 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 diameter.
As the lava continued flowing towards lower ground in the
Mývatn
area, the top crust collapsed, but the hollow pillars of solidified
lava remained.