🌋VolcanoAtlas

Tacaná

Central America's Second-Highest Volcano on Two Nations' Border

Elevation

4,064 m

Last Eruption

1986

Type

Stratovolcano

Country

Mexico-Guatemala

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 Activity40 years agoRecentRecently active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Watch
Dormant but monitored. Capable of renewed activity.
a rocky area with trees and a bright sun

Baptiste Coppéré

via Unsplash

Interesting Facts

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Tacaná is the second-highest peak in Central America at 4,064 m (13,333 ft), surpassed only by neighboring Tajumulco (4,220 m) just 20 km to the southeast.

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The international border between Mexico and Guatemala runs directly through or very near Tacaná's summit, making it one of the world's few volcanoes shared between two nations.

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Tacaná's most powerful known eruption (~70 CE, VEI 4) produced pyroclastic flows — a capability that far exceeds its mild historical phreatic activity, which has been limited to VEI 1.

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Approximately 300,000 people live within 30 km of the summit, including residents of Tapachula, Mexico's major border city with Guatemala.

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The Soconusco region at Tacaná's base produces some of Mexico's finest coffee, cultivated on volcanic soils at elevations of 900-1,500 m.

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Tacaná marks the precise geological transition between the Central American volcanic arc and the Trans-Mexican Volcanic Belt — two distinct volcanic systems driven by the same subducting Cocos Plate.

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Three large calderas on the volcano's upper flanks, all breached to the south, record episodes of massive edifice collapse.

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Cross-border volcanic hazard coordination between Mexico (CENAPRED) and Guatemala (INSIVUMEH) is required for Tacaná, adding complexity to emergency management.

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The volcano's name likely derives from the Mam Maya language, with a meaning related to 'fire' or 'high place.'

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Lahars from Tacaná could travel down deeply incised river valleys and reach populated lowland areas tens of kilometers from the summit.

Frequently Asked Questions

Is Tacaná still active?
Yes, Tacaná is classified as an active volcano. Its most recent eruption was a phreatic (steam-driven) event in February 1986. While historical eruptions have been mild (VEI 1), the geological record reveals that the volcano produced a VEI 4 eruption with pyroclastic flows approximately 1,950 years ago, demonstrating its capacity for much more powerful events. Fumarolic activity continues at the summit area, indicating an active hydrothermal system. CENAPRED (Mexico) and INSIVUMEH (Guatemala) jointly monitor the volcano.
How tall is Tacaná?
Tacaná stands 4,064 m (13,333 ft) above sea level, making it the second-highest peak in Central America. Only neighboring Tajumulco in Guatemala surpasses it at 4,220 m. Tacaná rises approximately 1,800 m above the surrounding metamorphic and plutonic terrain at its base. Its summit is the highest point in the Mexican state of Chiapas and in all of southern Mexico.
Which countries share Tacaná?
Tacaná straddles the international border between Mexico and Guatemala. The Mexican side falls within Chiapas state, while the Guatemalan side is in the San Marcos department. The summit lies essentially on the border. This binational status means that volcanic hazard management requires coordination between two different government systems — CENAPRED and UNAM on the Mexican side, and INSIVUMEH on the Guatemalan side. Communities on both sides of the border would be affected by a significant eruption.
What are the main hazards from Tacaná?
Tacaná's primary hazards include lahars (volcanic mudflows), pyroclastic flows, ashfall, and dome-collapse events. Lahars are considered the greatest risk because the volcano's steep, deeply incised terrain channels debris flows down river valleys toward populated lowlands, including areas near Tapachula (population ~350,000). The geological record of a VEI 4 eruption with pyroclastic flows (~70 CE) shows the volcano can produce events far more dangerous than its recent mild phreatic eruptions. Ashfall could impact the Soconusco coffee-growing region and disrupt air traffic.
Can you climb Tacaná?
Yes, Tacaná is a popular mountaineering destination, climbed from both Mexican and Guatemalan sides. The Mexican route typically begins from the village of Talquián above Unión Juárez in Chiapas, involving a demanding multi-day trek through cloud forest to the summit. Clear-weather views from the top are spectacular, encompassing the Pacific Ocean, Guatemala's volcanic chain, and the Mexican highlands. Climbers should prepare for cold temperatures at altitude, rapidly changing weather, and remote conditions. Local guides are available in Unión Juárez.
When did Tacaná last erupt?
Tacaná's most recent eruption occurred on February 16, 1986, from the northeast flank at approximately 3,600 m elevation. It was a phreatic (steam-driven) eruption classified at VEI 1, producing steam explosions and minor ash without fresh magma reaching the surface. Prior to that, a similar phreatic event occurred in 1949-1950. The volcano has been quiet since 1986 — a period of 39 years — but remains considered active by both Mexican and Guatemalan monitoring agencies.