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Mendoza Seismic Zone • 250 km Monitoring Radius

Real-Time Earthquakes in Mendoza, Argentina

Live seismic telemetry, active fault rupture tracking, and ground motion hazard monitoring for the Mendoza metropolitan area.

TECTONIC SETTING:Precordillera Active Thrust Belt & Nazca Flat-Slab Subduction
METRO POPULATION:1.1 Million (Greater Mendoza)
OBSERVATORY:INPRES →

MENDOZA EVENTS (250 KM)

3

NEAREST ACTIVE FAULT

Falla La Cal (5 km)

TELEMETRY WINDOW

Live Telemetry Feed

Recent Earthquakes Near Mendoza

LIVE

Live telemetry feed and hypocenter reports recorded within a 250 km radius of Mendoza.

Landmark Historical Earthquakes in Mendoza

Significant seismic benchmarks, cataloged damage, and engineering lessons shaping modern safety standards.

2021M 6.4

Pocito / Media Agua, San Juan Precordillera

2021-01-18•135 km from Mendoza•INPRES Intensity V–VI in Greater Mendoza

Strongest crustal earthquake in the Cuyo region in over 40 years; struck at a shallow depth of 14 km, violently shaking high-rise apartments in Mendoza in the late night, creating cracks in roadway infrastructure including National Route 40, damaging hundreds of adobe homes, and cutting off electricity in several districts.

1861M 7.0

Mendoza City Center (Falla La Cal)

1861-03-20•2 km from Mendoza•MMI IX (Catastrophic)

Completely destroyed the colonial city of Mendoza, killed 6,000 out of 18,000 residents, and led to the city being rebuilt around five large earthquake-refuge plazas.

1985M 6.0

Barrancas / Godoy Cruz

1985-01-26•15 km from Mendoza•MMI VIII (Severe)

Shallow crustal event that damaged 12,000 adobe houses and led to stricter modern enforcement of INPRES-CIRSOC building regulations.

Seismic Geology & Soil Amplification in Mendoza

Plate boundaries, tectonic kinematics, and local geotechnical ground response characteristics.

PLATE BOUNDARY:Nazca Plate & South American Plate Flat-Slab Sector
SLIP RATE:60–65 mm/year regional convergence
STRESS REGIME:Compressional Crustal Thrusting & Foreland Shortening

Mendoza is situated in western Argentina directly at the eastern foothills of the Andes. It sits in a flat-slab subduction zone where the Nazca plate subducts at a shallow horizontal angle, causing intense intraplate crustal deformation and active thrust faulting directly beneath the oasis city.

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Local Soil Profile & Ground Motion Resonance

Mendoza sits on alluvial cones of coarse gravel from the Mendoza River, but fine sand and silt in eastern sectors experience seismic amplification.

Major Active Fault Systems Near Mendoza

Seismogenic fault lines, maximum credible magnitudes (MCE), and proximity to the metropolitan center.

5 KM FROM CITYM 7.0

Falla La Cal

East-Vergent Reverse Thrust1 mm/year

Active thrust fault running along the western perimeter of Greater Mendoza; source of the 1861 disaster.

Seismic Safety, Observatory & Building Codes

Official seismological monitoring, building construction standards, early warnings, and emergency response.

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OFFICIAL SEISMIC OBSERVATORY

Instituto Nacional de Prevención Sísmica (INPRES) (INPRES)

INPRES National Seismic Telemetry Network
BUILDING CODE STANDARD:Reglamento INPRES-CIRSOC 103 (Normas Argentinas para Construcción Sismorresistente)
Visit Official Observatory (INPRES) →
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EMERGENCY HOTLINE
911

Agáchate, Cúbrete y Sujétate. Move to open plazas after shaking.

Frequently Asked Questions About Earthquakes in Mendoza

Authoritative answers to common questions regarding seismic risks, building safety, and preparedness in Mendoza.

Why was Mendoza rebuilt with five large public plazas?▾

After the 1861 earthquake flattened the colonial city, urban planners redesigned Mendoza with wide tree-lined avenues and five large equidistant plazas (Plaza Independencia and four satellite squares) designed as safe evacuation refuges.