About Askja
Askja is a composite caldera complex in the Dyngjufjöll Mountains of the central highlands. The volcano rises to 1,519 m, and the largest caldera contains a deep crater lake (Öskjuvatn). This otherworldly landscape served as a training ground for Apollo astronauts preparing for the Moon landing.
🌋 Volcanic System
- Large caldera complex: 50 km²
- Part of Dyngjufjöll Mountains
- Peak elevation: 1,519 m
- Contains Öskjuvatn crater lake
- Multiple eruption sites within caldera
🏔️ Highland Location
- Remote central highlands
- Elevation: 1,519 m (peak)
- Surrounded by black sand desert
- F-road access only (summer)
🚀 Apollo Training Ground
In 1965 and 1967, NASA sent Apollo astronauts to Askja to train for the Moon landing. The lunar-like landscape, volcanic craters, and basalt formations provided an ideal environment to practice geology and rover operations before the historic Apollo 11 mission.
Caldera of Fire and Water
Askja's nested calderas hold two remarkable lakes: the vast Öskjuvatn (Iceland's second deepest at 220 m) and the smaller, geothermally heated Viti crater with its milky turquoise water.
The contrast between the cold, dark Öskjuvatn and the warm, vivid Viti creates one of Iceland's most otherworldly landscapes - the same qualities that drew NASA to use this terrain for lunar training.
The 1875 Eruption
Askja's most famous eruption occurred on March 29, 1875, one of Iceland's most powerful and consequential volcanic events.
💥 Plinian Eruption - March 29, 1875
An explosive eruption ejected huge volumes of tephra. Ashfall darkened daytime skies across eastern Iceland and deposited ash as far as Sweden, Norway and Germany. This catastrophic event led to crop failure and livestock deaths, triggering a significant wave of emigration from Iceland.
Eruption Impact
- March 29, 1875 - Plinian explosive phase
- Ash cloud reached 25+ km high
- Tephra covered eastern Iceland
- Created Víti explosion crater
- Ash reached Sweden, Norway & Germany
Historical Consequences
- Destroyed farmland in east Iceland
- Livestock deaths and crop failures
- Triggered mass emigration to North America
- ~2,000 Icelanders left for Canada/USA
- Changed Iceland's settlement patterns
Complete Eruption History
- 10 Jul 1961 - early Aug 1961: Effusive eruption produced basaltic lava flows (Vikrahraun) covering ~15 km². The eruption was preceded by increased geothermal activity and seismicity.
- 1920s-1930: A series of small eruptions occurred between 1921 and 1930
- 29 Mar 1875: Catastrophic Plinian eruption - Iceland's most devastating volcanic event of the era
🔍 Recent Unrest (2021-Present)
Since 2021 the caldera floor has uplifted ~70 cm, and seismic swarms (e.g., March 2024) indicate magma accumulation. Scientists monitor the region for a possible new eruption.
Visiting Askja
Askja is one of Iceland's most remote and challenging destinations, accessible only in summer via F-roads requiring 4WD vehicles.
Access & Route
- Route: F88 (Askja Road)
- Vehicle: 4WD essential
- Season: Late June - early September
- Distance: ~85 km from Ring Road
Journey Time
- From Ring Road: 2-3 hours each way
- Total day trip: 6-8 hours
- Popular stop: Herðubreið mountain
- River crossings may be required
What to See
- Víti Crater: Turquoise geothermal lake
- Öskjuvatn: Iceland's second deepest lake (220m)
- Herðubreið: "Queen of Icelandic Mountains"
- Lava Fields: Black volcanic desert landscapes
- Dreki Hut: Mountain hut and campsite
⚠️ Important Safety Information
- Check road conditions at road.is before departure
- Weather changes rapidly - check vedur.is
- 4WD with high clearance required
- River crossings may be necessary
- Bring extra food, water, and warm clothing
- Cell phone coverage is limited/nonexistent
- Register your trip at safetravel.is
Tour Options
Due to the challenging access, many visitors choose guided super jeep tours or bus tours from Mývatn or Akureyri. These tours handle the difficult driving and provide expert knowledge about the area's geology and history.