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100 earthquakes recorded in Japan regional monitoring zone

Real-Time Earthquakes in Japan

Continuous seismic tracking along the Japan Trench, Nankai Trough, and Pacific Ring of Fire.

JAPAN EVENTS

100

TECTONIC SETTING

Pacific, Philippine Sea, Eurasian & Okhotsk Quad-Plate Intersection

TELEMETRY WINDOW

Live Telemetry Feed

LARGEST EVENT

M 5.1 9 km SE of Omigawa, Japan

Recent Earthquakes in Japan

LIVE

Live telemetry feed and seismic report for earthquakes in Japan.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:JAPAN-TRENCH-NANKAI-TROUGH
Slip Rate:80–90 mm/year (Pacific), 40–50 mm/year (Phil. Sea)
Stress Regime:Megathrust Subduction & Intraplate Crustal Faulting

Japan sits at the intersection of four major tectonic plates (Pacific, Philippine Sea, Eurasian, and Okhotsk). The subduction of the Pacific and Philippine Sea plates beneath Japan generates frequent megathrust events, active volcanism, and automated EEW (Early Warning) alerts.

Japan Trench & Kuril Trench

Subduction Megathrust

Deep oceanic trench where the Pacific Plate dives beneath northeast Honshu and Hokkaido.

Nankai Trough & Suruga Trough

Subduction Megathrust

High-risk convergent margin along southern Honshu with periodic M8+ recurring megathrust cycles.

Median Tectonic Line (MTL)

Right-Lateral Strike-Slip

Japan's longest onshore fault system cutting across Shikoku and the Kii Peninsula.

Itoigawa-Shizuoka Tectonic Line (ISTL)

Intraplate Compressional Thrust

Major tectonic suture dividing northeast and southwest geological domains in central Honshu.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

2011M 9.1

Offshore Sanriku, Tohoku

March 11, 2011

Great East Japan Earthquake; spawned a massive tsunami up to 40m, precipitating the Fukushima Daiichi nuclear accident.

1995M 6.9

Awaji Island / Kobe, Kansai

January 17, 1995

Great Hanshin earthquake directly rupturing beneath dense urban infrastructure; overhauled modern Japanese seismic codes.

1923M 7.9

Sagami Bay, Kanto Region

September 1, 1923

Great Kanto Earthquake; caused devastating urban fires in Tokyo and Yokohama.

2024M 7.6

Noto Peninsula, Ishikawa

January 1, 2024

Shallow reverse fault rupture causing substantial coastal land uplift and localized tsunami waves.

Frequently Asked Questions

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

What is the JMA Seismic Intensity (Shindo) scale?▾

Unlike moment magnitude (Mw) which measures total seismic energy, Japan's Shindo scale (0 to 7) measures the localized intensity of surface shaking experienced at specific geographic points.

How fast is Japan's Earthquake Early Warning (EEW) system?▾

JMA's EEW detects the fastest-moving P-waves at near-epicenter seismometers and broadcasts audible alarms to smartphones and television networks seconds before destructive S-waves arrive.

What is the Nankai Trough earthquake hazard?▾

The Nankai Trough has produced M8+ megathrust ruptures roughly every 100 to 150 years. Government seismologists estimate a 70–80% probability of an M8–M9 event occurring within the next 30 years.