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Quito Seismic Zone • 250 km Monitoring Radius

Real-Time Earthquakes in Quito, Ecuador

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

TECTONIC SETTING:Inter-Andean Graben & Quito Blind Thrust Fault System
METRO POPULATION:2.8 Million
OBSERVATORY:IG-EPN →

QUITO EVENTS (250 KM)

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NEAREST ACTIVE FAULT

Quito Fault System (Falla de Quito) (2 km)

TELEMETRY WINDOW

Live Telemetry Feed

SEISMIC INTENSITY

LOW SEISMICITY (24H)

Landmark Historical Earthquakes in Quito

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

2016M 7.8

Pedernales / Manabí Coast

2016-04-16•170 km from Quito•MMI VI in Quito

Catastrophic megathrust rupture along the subduction interface that killed over 670 people nationwide; strongly shook Quito for over a minute, cracked bridges and overpasses, caused blackouts in several Quito neighborhoods, damaged over 60 buildings in the capital, and knocked out mobile phone coverage.

2014M 5.1

Calderón / Northern Quito

2014-08-12•8 km from Quito•MMI VI (Strong Shallow)

Shallow 5 km deep rupture on the Quito Fault that caused landslides in the San Antonio de Pichincha quarries, halted traffic on the Collas highway, and caused 4 fatalities.

Seismic Geology & Soil Amplification in Quito

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

PLATE BOUNDARY:Nazca Plate & North Andean Sliver Collision Zone
SLIP RATE:50–60 mm/year regional subduction / 2–4 mm/year local crustal shortening
STRESS REGIME:Compressional Blind Thrusting & Volcanic Arc Seismicity

Quito is nestled in an elongated north-south Andean intermontane valley at 2,850 meters altitude along the eastern slopes of the active Pichincha volcano. The city is underlain by the Quito Fault system—a series of active west-dipping blind thrust faults that rupture directly underneath northern and central neighborhoods.

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Local Soil Profile & Ground Motion Resonance

Quito’s foundation consists of volcanic ash (cangahua), lahar deposits, and saturated alluvium. Hillsides in western Quito face landslide hazards, while ravines and soft volcanic ash amplify high-frequency ground acceleration.

Major Active Fault Systems Near Quito

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

2 KM FROM CITYM 6.8–7.1

Quito Fault System (Falla de Quito)

West-Dipping Blind Thrust2–4 mm/year

A 60 km blind reverse thrust fault running directly beneath Bellavista, Ilaló, and the northern suburbs of Quito.

Seismic Safety, Observatory & Building Codes

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

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OFFICIAL SEISMIC OBSERVATORY

Instituto Geofísico de la Escuela Politécnica Nacional (IG-EPN) (IG-EPN)

IG-EPN Real-Time Telemetry & SNGRE Early Warning Alerts
BUILDING CODE STANDARD:Norma Ecuatoriana de la Construcción (NEC-15)
Visit Official Observatory (IG-EPN) →
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EMERGENCY HOTLINE
911

Agáchate, Cúbrete y Sujétate. In historic colonial masonry structures in the Centro Histórico, beware of collapsing adobe, roof tiles, and decorative towers.

Frequently Asked Questions About Earthquakes in Quito

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

Why is the Quito Fault so dangerous?▾

Because it is a blind thrust fault located only 2 to 5 km beneath the densely populated city. Even a moderate M 6.5 rupture would generate extreme localized ground motion and slope failures across northern Quito.