LIVE Connected
🇳🇮

1 earthquakes recorded in Nicaragua regional monitoring zone

Real-Time Earthquakes in Nicaragua

Continuous seismic tracking along the Middle America Trench and Nicaraguan Volcanic Arc.

NICARAGUA EVENTS

1

TECTONIC SETTING

Cocos Plate & Caribbean Plate Subduction Interface

TELEMETRY WINDOW

Live Telemetry Feed

LARGEST EVENT

M 3.1 64 km SSW of Corinto, 03, Nicaragua

Recent Earthquakes in Nicaragua

LIVE

Live telemetry feed and seismic report for earthquakes in Nicaragua.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:MIDDLE-AMERICA-TRENCH
Slip Rate:70–80 mm/year convergence
Stress Regime:Megathrust Subduction & Volcanic Graben Strike-Slip

Nicaragua is situated along the high-energy convergent margin where the Cocos Plate subducts beneath the Caribbean Plate at the Middle America Trench at 70–80 mm/year. Shallow crustal faulting occurs along the Nicaraguan Volcanic Depression directly beneath population centers like Managua.

Middle America Trench (Nicaragua Segment)

Subduction Megathrust

Convergent interface capable of generating slow 'tsunami earthquakes' with high wave runup.

Tiscapa & Managua Graben Faults

Sinistral Strike-Slip & Normal

Active shallow fault network traversing directly beneath downtown Managua.

Central American Volcanic Arc Faults

Intra-Arc Extensional

Shallow faults linking active volcanic centers from Cosigüina to Mombacho.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

1972M 6.2

Managua, Western Nicaragua

December 23, 1972

Shallow rupture on the Tiscapa Fault directly beneath downtown Managua; destroyed 75% of the capital's housing.

1992M 7.7

Offshore Pacific Coast, Nicaragua

September 2, 1992

Classic 'tsunami earthquake' with gentle ground shaking but devastating 10m tsunami waves along the Pacific coast.

2014M 6.1

Lake Managua / Nagarote

April 10, 2014

Shallow crustal event near Apoyeque volcano causing structural damage across Nagarote and Mateare.

Frequently Asked Questions

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

Why did the 1972 Managua earthquake cause such extreme destruction despite being M6.2?▾

The 1972 earthquake was exceptionally shallow (depth under 5 km) with its epicenter directly beneath downtown Managua along the Tiscapa Fault, delivering extreme high-frequency shaking to unreinforced masonry buildings.

What is a 'tsunami earthquake' as seen in Nicaragua in 1992?▾

A tsunami earthquake ruptures very slowly along the shallow, sediment-rich uppermost subduction trench, generating minimal high-frequency ground shaking that humans feel, but displacing massive volumes of ocean water.

How does INETER monitor earthquakes in Nicaragua?▾

INETER operates a nationwide seismic network of over 100 digital stations with real-time satellite telemetry, issuing automatic earthquake reports and tsunami warnings.