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Taipei Seismic Zone • 200 km Monitoring Radius

Real-Time Earthquakes in Taipei, Taiwan

Live seismic telemetry, active fault rupture tracking, and ground motion hazard monitoring for the Taipei metropolitan area.

TECTONIC SETTING:Okinawa Trough Back-Arc Rifting & Ryukyu-Manila Trench Intersection
METRO POPULATION:2.5 Million (7.0M Metro)
OBSERVATORY:CWA →

TAIPEI EVENTS (200 KM)

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NEAREST ACTIVE FAULT

Shanchiao Fault (山腳斷層) (4 km)

TELEMETRY WINDOW

Live Telemetry Feed

SEISMIC INTENSITY

LOW SEISMICITY (24H)

Landmark Historical Earthquakes in Taipei

Significant seismic benchmarks, cataloged damage, and engineering lessons shaping modern safety standards.

2024M 7.4

Hualien Offshore

2024-04-03•125 km from Taipei•CWA Intensity 5-weak in Taipei

Taiwan’s strongest earthquake in 25 years since the Chi-Chi disaster; vigorously shook Taipei skyscrapers, halted the Taipei MRT rapid transit network, caused exterior facade tiles to rain onto city streets, damaged older school buildings, and triggered island-wide early warning sirens.

1999M 7.7

Chi-Chi / Nantou, Central Taiwan

1999-09-21•140 km from Taipei•CWA Intensity 5 in Taipei

The catastrophic Chi-Chi earthquake collapsed the 12-story Tunghsing Building in Taipei, killing 87 people in the capital and triggering nationwide building code overhauls.

Seismic Geology & Soil Amplification in Taipei

Plate boundaries, tectonic kinematics, and local geotechnical ground response characteristics.

PLATE BOUNDARY:Philippine Sea Plate & Eurasian Plate Oblique Collision Zone
SLIP RATE:80 mm/year convergence
STRESS REGIME:Back-Arc Extensional Normal Faulting & Compressional Forearc Wedge

Taipei is situated in an extensional triangle basin formed by volcanic collapse and tectonic subsidence at the northern tip of Taiwan. Surrounded by volcanic mountains (Datun Volcano Group), the basin is directly intersected by the active Shanchiao Normal Fault.

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Local Soil Profile & Ground Motion Resonance

The Taipei Basin is filled with soft Sungshan Formation clay and silt up to 300 meters deep. This soft sediment traps seismic waves and resonates at 1.0 to 1.5 seconds, strongly amplifying ground motion in mid-rise and high-rise towers like Taipei 101.

Major Active Fault Systems Near Taipei

Seismogenic fault lines, maximum credible magnitudes (MCE), and proximity to the metropolitan center.

4 KM FROM CITYM 7.0–7.2

Shanchiao Fault (山腳斷層)

Normal Fault1.5–2.0 mm/year

Active normal fault bounding the western edge of the Taipei Basin from Beitou through Guandu and Sanchong.

Seismic Safety, Observatory & Building Codes

Official seismological monitoring, building construction standards, early warnings, and emergency response.

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OFFICIAL SEISMIC OBSERVATORY

Central Weather Administration (CWA) Seismological Center (CWA)

CWA National Earthquake Early Warning via PWS Cell Broadcast (7–15 sec warning)
BUILDING CODE STANDARD:Taiwan Seismic Design Code (CPA 2022 Revision) & Tuned Mass Dampers (Taipei 101)
Visit Official Observatory (CWA) →
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EMERGENCY HOTLINE
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🌊 COASTAL TSUNAMI PROTOCOL

Northern Taiwan coastal ports (Keelung, Tamsui) are susceptible to tsunamis generated in the southern Okinawa Trough.

Fúchēn, Zhedang, Wēngù (Drop, Cover, and Hold On). Taipei high-rises are engineered to sway safely.

Frequently Asked Questions About Earthquakes in Taipei

Authoritative answers to common questions regarding seismic risks, building safety, and preparedness in Taipei.

How does Taipei 101 protect against earthquakes?▾

Taipei 101 is suspended with a 660-tonne tuned mass damper pendulum between the 87th and 92nd floors that counteracts up to 40% of building sway during severe earthquakes and typhoons.