Dimmuborgir
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Dimmuborgir

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Dimmuborgir is a large area of unusually shaped lava fields east of Mývatn in Iceland. The Dimmuborgir area is composed of various volcanic caves and rock formations, reminiscent of an ancient collapsed citadel (hence the name). The dramatic structures are one of Iceland's most popular natural tourist attractions.

The Dimmuborgir area consist of a massive, collapsed lava tube formed by a lava lake flowing in from a large eruption in the Þrengslaborgir and Lúdentsborgir 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 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. 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).

 

Source: https://en.wikipedia.org/wiki/Dimmuborgir

Dimmuborgir eru nálægt Mývatni.

Natural landmarks of Iceland

About Dimmuborgir

Dimmuborgir is a large area of unusually shaped lava fields east of Mývatn in Iceland. The Dimmuborgir area is composed of various volcanic caves and rock formations, reminiscent of an ancient collapsed citadel (hence the name). The dramatic structures are one of Iceland's most popular natural tourist attractions.

The Dimmuborgir area consist of a massive, collapsed lava tube formed by a lava lake flowing in from a large eruption in the Þrengslaborgir and Lúdentsborgir 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 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. 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).

 

Source: https://en.wikipedia.org/wiki/Dimmuborgir

Quick facts

TypeLava formations
DifficultyEasy
Rock typeBasalt lava
Formation typeLava formations
Best seasonSummer
Hiking routeHikeable
Glacier coverNot glacier covered
VolcanismVolcano
Volcanic activityNot an active volcano

Overview

Dimmuborgir is not a mountain but a remarkable field of lava pillars, arches, caves and walls near Lake Myvatn.

History

Dimmuborgir has long been one of the best-known natural attractions in the Myvatn region. Cultural context: Dimmuborgir contributes to the visual and cultural identity of its region and is part of the long relationship between Icelandic communities and mountain landscapes.

Geology

The formations developed when lava interacted with wet ground and temporary lava ponds. Steam activity, cooling and drainage left behind complex standing lava structures.

Hiking

Hiking possibilities around Dimmuborgir vary by route, season and access point. Exact distance and duration should be taken from a dedicated route record where available.

Safety

Conditions on Dimmuborgir can change quickly. Wind, low cloud, rain, snow, ice and loose ground can all increase difficulty. Visitors should check current conditions and choose routes appropriate to their experience. Practical visitor information: A practical nature stop rather than a mountain ascent

Views & surroundings

Within the area, the strongest views are of the lava formations themselves, with occasional openings towards Myvatn and nearby volcanic mountains. Surroundings: Dimmuborgir should be understood as part of its wider Icelandic landscape, including neighbouring valleys, ridges, lowlands and volcanic or glacial features. Nearby highlights: Lake Myvatn; Hverfjall; Reykjahlid Destination area: Lake Myvatn area

Interesting facts

Dimmuborgir is strongly associated with Icelandic troll folklore and modern Yule Lad traditions. Understand Dimmuborgir by noticing not just the summit, but also its rock, slopes, neighbouring landforms and position within the wider landscape. Notable features: The lava landscape resembles ruined castles and hidden passages, giving it a character unlike most ordinary lava fields. Summary: A complex lava-formation area near Myvatn, known for arches, walls, caves and strong folklore connections. Themes: Lava formations; folklore; nature walks

Frequently asked questions

Are Dimmuborgir a mountain?
No. Dimmuborgir is a lava-formation area near Myvatn with pillars, walls, arches and caves.
What makes Dimmuborgir special?
The lava created a complex three-dimensional landscape resembling ruined castles and walls, with strong connections to Icelandic folklore.
How should visitors explore Dimmuborgir?
Visitors should stay on marked trails to protect both fragile vegetation and the lava formations.

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Dimmuborgir

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