Askja

Highland Caldera

50 km² Caldera Size
1875 Famous Eruption
1,516m Peak Elevation
Last updated: February 2026

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.

Víti crater lake and Askja caldera in the Icelandic highlands

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.

Víti Crater Lake

💎 Iceland's Blue Jewel

Víti (meaning "Hell" in Icelandic) is a stunning turquoise-blue crater lake formed during the 1875 eruption. The geothermal-heated water reaches temperatures of 20-60°C, creating a dramatic contrast against the dark volcanic rock.

Crater Features

  • Diameter: ~150 meters
  • Water temperature: 20-60°C
  • Turquoise color from minerals
  • Formed in 1875 eruption

Swimming

  • Swimming is allowed (but check current status)
  • Milky, mineral-rich water
  • Steep descent to water's edge
  • Changing weather conditions

⚠️ Swimming Safety

While swimming in Víti has been popular, always check current conditions and restrictions. The path down is steep and can be slippery. Weather can change rapidly in the highlands. Never swim alone.

Aerial view of Askja caldera and the Dyngjufjöll mountains

The Dyngjufjöll mountains cradle Askja's caldera complex. This remote highland terrain, surrounded by black sand desert, remains one of Iceland's most isolated volcanic landscapes.

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.

F88 highland road leading to Askja volcano in Iceland

The Journey to Askja - Route F88

The F88 highland road stretches 85 km from the Ring Road across black sand desert to Askja's caldera. The journey itself is an adventure, crossing rivers and traversing one of Europe's last true wilderness areas.

A high-clearance 4WD vehicle is essential. The road opens in late June when snow melts and closes again in September. Many visitors opt for guided super jeep tours from Myvatn or Akureyri.

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