🌋VolcanoAtlas

Irazú

Costa Rica's Tallest Volcano, Towering Over San José

Elevation

3,436 m

Last Eruption

1977 (possible 1994)

Type

Stratovolcano

Country

Costa Rica

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows
  • Lava flows
  • Volcanic bombs and ballistics
  • Lahars and mudflows

Risk Level

Population at RiskLow
Infrastructure RiskHigh
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Unknown
Silica Content
Varied composition

Tectonic Setting

Unknown
Intraplate setting with hotspot or regional volcanic activity.

Age & Formation

Epoch
Unknown
Evidence
Unknown

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent Activity-19769968 years agoVery RecentCurrently active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Active
Recent volcanic activity detected. Continuous monitoring in place.
green and brown mountain under blue sky during daytime

Emmanuel Appiah

via Unsplash

green and brown mountain under blue sky during daytime

Emmanuel Appiah

via Unsplash

aerial photography of lake under blue sky

Juliana Barquero

via Unsplash

Other Volcanoes in Costa Rica

Interesting Facts

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Irazú is Costa Rica's tallest volcano at 3,436 m (11,273 ft), and on clear days both the Pacific Ocean and Caribbean Sea are visible from its summit.

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The 1963 eruption began on the same day that U.S. President John F. Kennedy arrived in San José for a state visit — ash reportedly fell on the presidential motorcade.

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The 1963–1965 eruption lasted approximately two years, depositing volcanic ash across the entire Central Valley and triggering lahars that killed approximately 20 people.

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All known Holocene eruptions of Irazú have been explosive — no lava has flowed from the volcano in approximately 14,000 years.

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The summit crater lake changes color dramatically from vivid green to turquoise to rust-red, depending on chemical and mineral conditions, making it one of Costa Rica's most photographed natural features.

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Irazú's volcanic massif covers approximately 500 km², making it one of the largest volcanic edifices in Central America by area.

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At least 10 parasitic cinder cones on the south flank indicate that the volcanic system extends well beyond the main summit complex.

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The Diego de la Haya Crater is named after the Spanish colonial governor who first documented an eruption of Irazú in 1723.

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Approximately 2 million people live in the San José–Cartago metropolitan corridor within Irazú's broader ashfall hazard zone.

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Irazú Volcano National Park, established in 1955, is one of the most visited national parks in Costa Rica thanks to the paved road access to the summit.

Frequently Asked Questions

Is Irazú an active volcano?
Yes, Irazú is classified as an active volcano by the Smithsonian Global Volcanism Program. It has 31 recorded eruptions, with the last confirmed magmatic eruption in 1977 (VEI 1) and uncertain phreatic activity reported in 1994. The most significant modern eruption was the 1963–1965 VEI 3 event that caused widespread destruction across Costa Rica's Central Valley. The volcano is continuously monitored by OVSICORI-UNA and RSN, and scientists consider future eruptions possible. The current dormancy period of approximately 50 years is within the historical range of inter-eruption intervals.
Can you visit Irazú Volcano?
Yes, Irazú Volcano National Park is one of Costa Rica's most accessible and popular natural attractions. A paved road leads to within walking distance of the summit crater viewpoints, making it one of the easiest active volcanoes to visit in the world. The park is approximately 80 km from San José (about a 2-hour drive) and 30 km from Cartago. Visitors can view the famous colored crater lake and surrounding craters. The best time to visit is early morning during the dry season (December–April) when cloud cover is minimal. An entrance fee is charged.
What happened during the 1963 Irazú eruption?
The 1963–1965 eruption was Costa Rica's most destructive modern volcanic event. Beginning on March 13, 1963, the VEI 3 eruption produced continuous ash emissions over approximately two years, blanketing San José, Cartago, and the Central Valley. The eruption coincided with U.S. President Kennedy's state visit. The most devastating impacts were lahars (volcanic mudflows) in the Reventazón river valley triggered by heavy rains mobilizing ash deposits, which killed approximately 20 people and destroyed bridges and homes. Agricultural and economic losses were severe.
How tall is Irazú?
Irazú rises to 3,436 m (11,273 ft) above sea level, making it the tallest volcano in Costa Rica. Its neighboring volcano Turrialba is slightly shorter at 3,340 m. For comparison, Costa Rica's highest point overall is Cerro Chirripó at 3,821 m, which is not volcanic. Irazú's broad massif covers approximately 500 km², and on clear days both the Pacific and Caribbean coasts are visible from the summit — a span of over 200 km.
Why is Irazú's crater lake different colors?
Irazú's main crater lake changes color due to variations in its chemical and mineral composition. The lake can appear vivid emerald green, turquoise blue, or rust-red at different times. These changes reflect fluctuations in dissolved minerals (particularly sulfur and iron compounds), pH levels, suspended sediment, and volcanic gas input from the underlying hydrothermal system. Scientists monitor the lake's chemistry as an indicator of volcanic unrest — significant color or temperature changes can signal increased magmatic activity at depth.
Is Irazú dangerous?
Irazú poses one of the highest volcanic risks in Central America. Approximately 2 million people live in the San José–Cartago metropolitan corridor within its ashfall hazard zone. The 1963–1965 eruption demonstrated the volcano's capacity for sustained explosive eruptions that disrupt life across the densely populated Central Valley. Lahars are a particular concern due to steep flanks, multiple river drainages, and heavy tropical rainfall. A future eruption of similar or greater intensity would affect a much larger urban population than existed in 1963.