Is there a high seismic risk in Ecuador?

Is there a high seismic risk in Ecuador?

The 7.8 magnitude earthquake that took place last Saturday, 16th April in Esmeraldas province (Ecuador), confirms a well-known fact: That the high seismic risk in that region of the Pacific Ocean is associated with the convergence of Nazca and Southamerica plates.

Where was the earthquake in Ecuador in April 2016?

On April 20, a 6.1–6.2 magnitude aftershock struck 15 miles west of Muisne around 3:30AM, local time. The quake had a depth of about 9 miles. José Joaquín de Olmedo International Airport in Guayaquil was also closed due to communication issues.

How many people died in the earthquake in Ecuador?

At least 676 people were killed and more than 16,600 others were injured in the earthquake. It was the worst natural disaster to hit Ecuador since the 1949 Ambato earthquake. Over 300 fatalities occurred in the cities of Manta and Portoviejo, both of which are located in Manabí Province.

Which is the most dangerous area in Ecuador?

The thesis, marked with a cum laude distinction, provided an Ecuador risk map, among other results, observing that Esmeraldas province, which has been the most affected area by the recent earthquake, is the most dangerous territory.

Where was the epicenter of the earthquake in Ecuador?

At 18:58 ECT on April 16, a 7.8 Mw earthquake struck the coast of Ecuador approximately 27 km (17 mi) south-southeast of Muisne, in the province of Esmeraldas, at a depth of 20.6 km (12.8 mi).

How big was the earthquake in Ecuador in 2016?

Six homes collapsed and many others lost power in the nation’s capital city of Quito. The earthquake was presaged by a magnitude 4.8 foreshock eleven minutes before the main quake struck, and followed by over fifty-five aftershocks in the first twenty-four hours.

What was the convergence rate of the plates in Ecuador?

The convergence rate between the plates in Ecuador is 61 mm (2.4 in) per year. The depth, location and focal mechanism of the earthquake are all consistent with rupture along the plate interface in the form of a megathrust earthquake.