🌋VolcanoAtlas

Láscar

The Most Active Volcano of the Northern Chilean Andes

Elevation

5,592 m

Last Eruption

2022–2023

Type

Stratovolcano(es)

Country

Chile

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 RiskModerate
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-20219997 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.

Other Volcanoes in Chile

Interesting Facts

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Láscar is the most active volcano in the northern Chilean Andes, with 37 eruptions recorded since the mid-19th century.

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The April 1993 VEI 4 eruption was the largest in the central Andes since a major event at Huaynaputina in Peru in 1600 — a gap of nearly 400 years.

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Ash from the 1993 eruption traveled approximately 1,500 km to Buenos Aires, Argentina, and was reportedly detected as far as São Paulo, Brazil.

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Pyroclastic flows during the 1993 eruption extended 8.5 km from the summit and were hot enough to partially weld in their proximal deposits.

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Láscar stands at 5,592 m (18,346 ft) in one of the driest environments on Earth — the Atacama Desert receives less than 100 mm of rain per year at these elevations.

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The volcano has six overlapping summit craters, documenting a complex history of repeated crater formation and collapse.

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Láscar consists of two distinct edifices — an older eastern volcano (Aguas Calientes) and the currently active western cone.

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No fatalities have been recorded from any of Láscar's eruptions, primarily due to its extreme remoteness in the high Atacama Desert.

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The 1993 eruption column reached an estimated 22–25 km altitude, penetrating well into the stratosphere.

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Activity at Láscar has migrated between eastern and western edifices over the past ~26,500 years, a pattern of vent migration seen at other complex volcanic centers.

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The Atacameño village of Talabre, the closest settlement at ~15 km, received heavy ashfall during the 1993 eruption but was spared pyroclastic flows.

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Láscar's eruptions in the ultra-dry Atacama produce minimal lahar hazard — a rarity among active volcanoes worldwide.

Frequently Asked Questions

Is Láscar volcano still active?
Láscar is an active stratovolcano in northern Chile that has erupted 37 times since historical records began in the mid-19th century. Its most recent eruption occurred in 2022–2023, a VEI 3 event that prompted SERNAGEOMIN (Chile's national geological survey) to raise the alert level to orange. Persistent fumarolic activity, thermal anomalies, and intermittent degassing are ongoing at the summit craters. Láscar is the most active volcano in the northern Chilean Andes, and volcanologists expect continued activity. The volcano is continuously monitored using seismometers, satellite-based deformation and SO2 sensors, and webcams.
What happened in the 1993 Láscar eruption?
On April 19–20, 1993, Láscar produced a VEI 4 eruption — the largest in the central Andes in nearly 400 years. The eruption sent an ash column an estimated 22–25 km into the stratosphere, well above the tropopause. Pyroclastic flows cascaded 8.5 km down the northwest flanks, hot enough to partially weld near the vent. Fine volcanic ash was carried by upper-level winds across the Andes, with measurable ashfall reported in Buenos Aires (~1,500 km away) and possibly São Paulo, Brazil. The eruption deposited an estimated 0.1 km³ of tephra. No fatalities occurred due to the volcano's extreme remoteness in the Atacama Desert.
How tall is Láscar?
Láscar stands at 5,592 m (18,346 ft) above sea level, making it one of the highest active volcanoes in northern Chile. It rises from the high Altiplano at approximately 4,000–4,500 m elevation, so its local prominence above the surrounding terrain is approximately 1,000–1,500 m. The neighboring extinct Volcán Aguas Calientes, 5 km to the east, is slightly higher. The extreme altitude makes any approach to the summit physically demanding, requiring full high-altitude acclimatization. For context, Láscar is considerably lower than the highest Andean volcanoes like Ojos del Salado (6,893 m) or Llullaillaco (6,739 m).
Where is Láscar volcano located?
Láscar is located in the Antofagasta Region of northern Chile at coordinates 23.370°S, 67.730°W, within the Atacama Desert — one of the driest places on Earth. The nearest town is the small Atacameño village of Talabre, approximately 15 km away. The popular tourist hub of San Pedro de Atacama lies approximately 70 km to the west. The volcano sits within the Central Andean Volcanic Arc along the Chile-Argentina border, at an altitude of 5,592 m on the high Altiplano. The nearest airport is at Calama, connected to San Pedro de Atacama by paved road.
Can you visit Láscar volcano?
Visiting Láscar is possible during periods of low volcanic activity, though it requires a 4WD vehicle, good navigation skills, high-altitude acclimatization, and respect for volcanic hazard zones. The volcano is reached via unpaved desert roads from San Pedro de Atacama (~70 km). There are no marked trails, services, or shelter. Summit attempts are extremely demanding at 5,592 m altitude. During eruptions, SERNAGEOMIN establishes exclusion zones that prohibit approach. The broader Atacama region offers outstanding attractions including the Salar de Atacama, Valle de la Luna, El Tatio geysers, and world-class stargazing. Always check SERNAGEOMIN's current volcanic alert level before planning any visit.
Why is Láscar so active?
Láscar's persistent activity results from the subduction of the Nazca Plate beneath the South American Plate along the Central Andean Volcanic Arc. As the oceanic plate descends into the mantle, water released from the slab lowers the melting point of the overlying mantle wedge, generating magma that rises through the extremely thick continental crust (>60 km) of the central Andes. The extreme crustal thickness produces silica-rich, gas-charged magmas that erupt explosively. Láscar's position within the arc, combined with a sustained magma supply evidenced by its persistent thermal anomalies and gas emissions, makes it the most frequently erupting volcano in the northern Chilean segment of the arc.
What type of volcano is Láscar?
Láscar is classified as a stratovolcano (composite volcano) built from alternating layers of lava flows and pyroclastic deposits. More specifically, the Smithsonian classifies it as 'Stratovolcano(es)' — reflecting that it comprises two distinct volcanic edifices: an older eastern cone and the currently active western cone. The volcano's magmas are andesitic to dacitic in composition, producing eruptions that are typically explosive. Six overlapping summit craters document repeated episodes of crater formation and collapse. Láscar's eruption style ranges from minor ash emissions (VEI 1) to significant explosive events (VEI 4) producing pyroclastic flows.
Has anyone died from a Láscar eruption?
No fatalities have been recorded from any of Láscar's eruptions. This is primarily due to the volcano's extremely remote location in the high Atacama Desert, where the nearest settlement (the Atacameño village of Talabre) is approximately 15 km away and has a small population. During the powerful 1993 VEI 4 eruption, pyroclastic flows extended 8.5 km — far enough to be dangerous but not reaching Talabre. However, the growing tourism industry around San Pedro de Atacama has increased the number of people who may be in the volcano's vicinity during eruptions, and SERNAGEOMIN's exclusion zones during active periods are critical for maintaining this safety record.