Live seismic activity in Ecuador — updated every 60 seconds from USGS data. Ecuador lies on the Pacific Ring of Fire, where the Nazca Plate subducts beneath the South American Plate, causing frequent strong earthquakes and volcanic activity.
Ecuador lies on the Pacific Ring of Fire, where the Nazca Plate subducts beneath the South American Plate, causing frequent strong earthquakes and volcanic activity. The 1906 Ecuador–Colombia earthquake (M8.8) was one of the largest ever recorded in the region, generating a trans‑Pacific tsunami. Major faults include the subduction interface of the Nazca Plate and the Chingual–Cosanga–Payamino fault system. Notable quakes include 1906 Esmeraldas (M8.8), 2016 Muisne (M7.8). The seismic risk is very high. Tectonically, Ecuador lies on the convergent boundary where the Nazca Plate subducts beneath the South American Plate. This page provides real‑time USGS data and historical context for Ecuador.
The largest earthquake recorded in Ecuador in the past 100 years was M7.8 in 1942 (12 km SE of Pedernales, Ecuador). The region is defined by Nazca subduction interface, Chingual–Cosanga–Payamino fault system, and the risk level is classified as Very High.
With a population of 17 million, understanding local seismic hazards is crucial. This page provides real‑time USGS data and historical context for Ecuador.
Ecuador lies on Nazca Plate subducting beneath South American Plate. The movement of these plates builds up stress, which is released as earthquakes. In subduction zones, one plate dives beneath another, generating some of the largest quakes on Earth. In some regions, strike‑slip faults produce frequent moderate earthquakes.
Data sources: USGS real‑time feed, USGS historical archive (last 100 years), and Wikipedia. Page refreshes live earthquake data every 60 seconds.