الانتقال إلى المحتوى الرئيسي
Open on Map
Seismic Event Dossier02:50 Local (18:50 UTC)(الآن)

Earthquake near Pingtung, Taiwan

A magnitude 7.8 (MW) earthquake occurred on 1951-11-24, 02:50 local time (18:50 UTC) (الآن), centered 88 km NE of Pingtung (Taiwan). The hypocenter was located at a shallow depth of 30 km. Primary telemetry verified by USGS.

Historical Landmark Earthquake

#72 of All Time

Curated Global Seismic Archive (1700–Present)

Top-100 Earthquakes
Magnitude 7.8 historical earthquake occurring on 1951-11-24 in Taiwan. Associated with the Longitudinal Valley fault (Active Fault). Documented casualties: > 1,000.
Documented Fatalities> 1,000
Fault KinematicsActive Fault
Equivalent Energy7.56 Mt TNT

القدر

MW
M 7.8

7.56 Mt TNT

العمق

30 km
30 km

shallow (قشري ضحل)

أثر PAGER

red
> 1,000 fatalities

الإصابات المقدرة: > 5,000 · ~55.5M محسوس

خريطة تفاعلية للبؤرة السطحية والصدوع

23.09°N, 121.21°E
فالق5 km
Longitudinal Valley fault
Active Fault · ~15.0 mm/yr
Felt byMMI III+
~55.5M exposed
~33.4M strong shaking
Primary SolutionUSGS
USGS#iscgem894988reviewed
1 agencies reporting
Setting23.1°N
Taiwan
Continental / Inland crustal

Seismic Activity & Aftershock Sequence

Timeline of foreshocks, main rupture, aftershocks and machine learning risk probability evolution.

M0.0M4.5M9.0100%50%0%الهزة الرئيسية27 نوفمبر2 ديسمبر7 ديسمبرM7.8
Hover or tap a point to inspect aftershocks and risk probability curve.
<35 كم (ضحل)35–70 كم (متوسط العمق)>70 كم (عميق)الهزة الرئيسية
توقعات مخاطر تعلم الآلة:12h38%24h51%72h66%7d82%

Verified Disaster & Impact Assessment

Official emergency management data cross-checked against multi-agency wires

Continuous verification
Casualties
Damage assessment in progress
Tsunami Status
No tsunami threat
NOAA PTWC & regional buoys
Citizen Felt Reports
0
No felt reports submitted
Macroseismic DYFI verification
Aftershock Sequence
Aftershocks: 3
High Omori aftershock probability
LightGBM hazard model forecast

Agency Discrepancy Matrix (Cross-Network Verification)

Comparing multi-network solutions from primary and teleseismic monitoring agencies.

Network / SourceMagnitude (Scale & Diff)Depth & DiffEpicenter & Shift (Δd)ConsensusEvent ID / Data
USGS
United States Geological Survey · Global / US
M7.8(Mw)Ref
30.0 kmRef
23.09°, 121.21°Origin
Authoritative
iscgem894988

Why do agency magnitudes differ? Seismological agencies use different instrumentation networks, crustal velocity models, and mathematical magnitude scales (e.g. Moment Magnitude Mw vs Local Richter ML vs Surface Wave Ms). Differences of 0.1–0.3 are common and reflect physical observation geometry rather than errors.

Where it was felt

6 تجمعات سكانية

Shaking intensity is modelled from magnitude, depth and distance (GMPE attenuation), not reported by residents.

TownDistanceIntensity
Taitung · Taitung38 kmMMI IX
Pingtung · Pingtung88 kmMMI VIII
Chiayi · Chiayi City90 kmMMI VIII
Douliou · Yunlin97 kmMMI VIII
Taibao · Chiayi98 kmMMI VIII
Tainan · Tainan City104 kmMMI VIII

Tectonic setting

Nearest mapped active fault: Longitudinal Valley fault, 5 km away, slip rate ~15.0 mm/yr (GEM Global Active Faults).