LIVE Connected
🇦🇱

2 earthquakes recorded in Albania regional monitoring zone

Real-Time Earthquakes in Albania

Continuous seismic tracking along the Adriatic Coastal Thrust and Albanides mountain chain.

ALBANIA EVENTS

2

TECTONIC SETTING

Eurasian & Adria Microplate Collisional Thrust Belt

TELEMETRY WINDOW

Live Telemetry Feed

LARGEST EVENT

M 2.3 27 km ENE of Burrel, 41, Albania

Recent Earthquakes in Albania

LIVE

Live telemetry feed and seismic report for earthquakes in Albania.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:HELLENIC-ADRIATIC-COLLISION
Slip Rate:4–8 mm/year convergence
Stress Regime:Compressional Crustal Thrusting & Transverse Strike-Slip

Albania is situated along the convergent margin where the Adria Microplate collides with the Eurasian Plate in the Hellenic-Dinaric orogenic belt. Intense crustal shortening drives active blind thrust faulting along the Adriatic coastline and extensional graben faulting in eastern mountain basins.

Durrës Coastal Thrust Fault

Blind Reverse Thrust

Compressional blind thrust fault beneath the Adriatic coastal plain; source of the 2019 earthquake.

Vlora-Lushnja Fault Zone

Thrust & Strike-Slip

Active fault zone accommodating convergence between the Adriatic foreland and Albanides mountain chain.

Shkodra-Peja Transverse Fault

Regional Strike-Slip

Major tectonic boundary dividing the Dinaric and Hellenic geological domains.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

2019M 6.4

Durrës / Thumanë, Adriatic Coast

November 26, 2019

Strongest earthquake to hit Albania in 40 years; blind thrusting collapsed modern residential buildings in Durrës.

1979M 6.9

Montenegro-Albania Border

April 15, 1979

Severe offshore compressional thrusting causing heavy damage in Shkodra and along the northern Albanian coastline.

1967M 6.6

Dibra, Eastern Albania

November 30, 1967

Shallow crustal event along the eastern graben systems causing surface fault ruptures and mountain village collapses.

Frequently Asked Questions

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

Why did the 2019 Durrës earthquake cause such extensive damage?▾

The 2019 M6.4 earthquake was shallow (20 km) on a blind thrust fault directly beneath coastal mud and sand deposits, causing strong ground amplification and structural failure in buildings lacking seismic reinforcement.

Which parts of Albania have the highest earthquake risk?▾

The Adriatic coastal belt (Durrës, Vlora, Lezha, Shkodra) and the Ionian zone in the south feature the highest seismic hazard in Albania.

How does IGEO monitor seismic activity in Albania?▾

The Institute of GeoSciences (IGEO) at the Polytechnic University of Tirana operates digital broadband seismic stations across Albania, streaming telemetry in real time.