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0 earthquakes recorded in Iran regional monitoring zone

Real-Time Earthquakes in Iran

Continuous seismic tracking along the Zagros Fold-and-Thrust Belt and Alborz Mountains.

IRAN EVENTS

0

TECTONIC SETTING

Arabian & Eurasian Plate Continental Collision

TELEMETRY WINDOW

Live Telemetry Feed

Recent Earthquakes in Iran

LIVE

Live telemetry feed and seismic report for earthquakes in Iran.

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:ZAGROS-BITLIS-COLLISION
Slip Rate:20–25 mm/year northward collision
Stress Regime:Compressional Fold-and-Thrust & Active Strike-Slip Shearing

Iran is caught in the active continental collision between the Arabian Plate moving north-northeast into the Eurasian Plate at ~25 mm/year. Crustal shortening is accommodated by the Zagros Fold-and-Thrust Belt in the south, the Alborz and Kopeh Dagh mountains in the north, and active strike-slip faults crossing central Iran.

Main Recent Fault (MRF)

Dextral Strike-Slip

Major right-lateral strike-slip fault accommodating oblique plate collision along the Zagros front.

Mosha & North Tehran Faults

Left-Lateral Oblique Reverse

Major faults bounding the southern foot of the Alborz Mountains, posing acute hazard to Tehran.

Bam Fault

Blind Strike-Slip

Fault in southeastern Iran that ruptured directly beneath the ancient city of Bam in 2003.

North Tabriz Fault

Right-Lateral Strike-Slip

100 km fault passing through northern Tabriz with a historical record of recurring M7.0+ events.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

2003M 6.6

Bam, Kerman Province

December 26, 2003

Devastating blind strike-slip rupture beneath adobe and unreinforced masonry city, destroying the ancient Arg-e Bam.

1990M 7.4

Manjil-Rudbar, Alborz Mountains

June 20, 1990

Left-lateral strike-slip rupture near the Caspian Sea causing widespread destruction across Gilan and Zanjan.

2017M 7.3

Ezgeleh, Kermanshah / Iran-Iraq Border

November 12, 2017

Zagros Mountain frontal thrust faulting felt across the entire Middle East.

Frequently Asked Questions

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

Why does Iran experience so many deadly earthquakes?▾

Iran is situated in the middle of the Arabian-Eurasian continental collision. Many rural and historic settlements feature traditional unreinforced adobe and heavy mud-brick construction that collapses readily under seismic shear.

What is the earthquake risk for Tehran?▾

Tehran is surrounded by several active faults (the Mosha Fault, North Tehran Fault, and Rey Faults). Seismologists estimate significant accumulated strain capable of generating an M7.0+ earthquake.

What is the Makran subduction zone in southeastern Iran?▾

The Makran Subduction Zone off the coast of southeastern Iran and Pakistan is where the Arabian plate subducts beneath Eurasia, capable of M8.0+ megathrust events and Indian Ocean tsunamis.