LIVE Connected
🇪🇨

0 earthquakes recorded in Ecuador regional monitoring zone

Real-Time Earthquakes in Ecuador

Continuous seismic tracking along the Ecuador Trench, Carnegie Ridge, and Inter-Andean Depression.

ECUADOR EVENTS

0

TECTONIC SETTING

Nazca & South American Subduction & Carnegie Ridge Collision

TELEMETRY WINDOW

Live Telemetry Feed

Recent Earthquakes in Ecuador

LIVE

Live telemetry feed and seismic report for earthquakes in Ecuador.

Awaiting Seismic Telemetry

No recent events reported for global slug "world". Data streams automatically when earthquakes occur.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:CARNEGIE-RIDGE-COLLISION
Slip Rate:50–55 mm/year convergence
Stress Regime:Megathrust Subduction & Shallow Inter-Andean Reverse Faulting

Ecuador is situated where the oceanic Nazca Plate subducts beneath the South American Plate along the Ecuador-Colombia Trench. The ongoing collision of the thick Carnegie Ridge produces high seismicity, localized coastal uplift, and complex reverse faulting in the Inter-Andean valley.

Ecuador-Colombia Trench

Subduction Megathrust

Primary convergent interface capable of generating M8.0+ megathrust events.

Quito Fault System

Blind Reverse Thrust

System of active reverse thrust faults directly underlying western Quito.

Pallatanga-Chingual Fault Zone

Dextral Strike-Slip

Major transpressional fault zone cutting through the Ecuadorian Andes.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

2016M 7.8

Pedernales / Muisne, Manabí

April 16, 2016

Severe megathrust rupture along the central subduction interface; heavily damaged Pedernales, Portoviejo, and Manta.

1906M 8.8

Offshore Esmeraldas / Ecuador-Colombia

January 31, 1906

One of the largest earthquakes ever recorded globally; triggered a destructive trans-Pacific tsunami.

1987M 7.1

El Reventador, Napo Province

March 5, 1987

Shallow Andean thrusting triggering massive mudflows and landslides that destroyed vital national pipeline infrastructure.

Frequently Asked Questions

Common questions about seismic activity, safety, and monitoring in Ecuador.

Why was the 2016 Pedernales earthquake so destructive in Ecuador?▾

The 2016 M7.8 earthquake was a major subduction megathrust event that released stress accumulated since 1942, generating strong accelerations in soft coastal soils that caused structural collapse of unreinforced concrete buildings.

What is the Carnegie Ridge and how does it affect Ecuador's earthquakes?▾

The Carnegie Ridge is a thick volcanic underwater ridge on the Nazca Plate that is subducting beneath central Ecuador, increasing friction and coupling at the plate interface.

How does the Instituto Geofísico (IGEPN) monitor quakes and volcanoes?▾

IGEPN operates the Red Nacional de Sismógrafos (RENSIG) with over 150 digital stations across mainland Ecuador and the Galápagos Islands, providing 24/7 monitoring of both earthquakes and active volcanoes.