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Seismic Event Dossier06:32 Local (22:32 UTC)(99y ago)

M 7.7 earthquake Wuwei, Gansu, China

A magnitude 7.7 (MW) earthquake occurred on 1927-05-22, 06:32 local time (22:32 UTC) (99y ago), centered 32 km SW of Wuwei (China). The hypocenter was located at a shallow depth of 15 km. Primary telemetry verified by USGS.

Historical Landmark Earthquake

#24 of All Time

Curated Global Seismic Archive (1700–Present)

Top-100 Earthquakes

A magnitude 7.7 earthquake struck ⁨Wuwei, Gansu, China⁩ on 22 Mei 1927. Documented deaths: 40,912.

Documented Fatalities40,912Source: NOAA NCEI Significant Earthquake Database
Fault KinematicsActive fault
Equivalent Energy5.35 Mt TNT

Magnitudo

MW
M 7.7

5.35 Mt TNT

Kedalaman

15 km
15 km

shallow (Kerak dangkal)

Dampak PAGER

red
> 1,000 fatalities

Luka-luka: > 5,000 · ~198.6M merasakan

Peta Interaktif Episenter & Sesar

37.67°N, 102.49°E
Sesar21 km
Segmen Sesar Aktif
Slip · ~15.0 mm/yr
Felt byMMI III+
~198.6M exposed
~18.5M strong shaking
Primary SolutionUSGS
USGS#iscgem909273reviewed
1 agencies reporting
Setting37.7°N
China
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%Gempa utama22 Mei, 0422 Mei, 1623 Mei, 0423 Mei, 1624 Mei, 0424 Mei, 1625 Mei, 0425 Mei, 16M7.7
Hover or tap a point to inspect aftershocks and risk probability curve.
<35 km (Dangkal / Merusak)35–70 km (Menengah)>70 km (Fokus Dalam)Gempa utama

Situation Monitoring

Continuous verification
Multi-agency verification of casualties, tsunami alerts, and seismic sequence

Key facts so far

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
Monitoring
Aftershocks expected (Omori law)
LightGBM hazard model forecast
Multi-agency seismic telemetry active. Awaiting wire headlines.

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
M7.7(Mw)Ref
15.0 kmRef
37.67°, 102.49°Origin
Authoritative
iscgem909273

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 permukiman

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

TownDistanceIntensity
Wuwei · Gansu32 kmMMI IX
Jinchang · Gansu96 kmMMI VIII
Xining · Gansu133 kmMMI VII
Lanzhou · Gansu213 kmMMI VI
Zhangye · Gansu227 kmMMI VI
Linxia · Gansu238 kmMMI VI

Tectonic setting

Nearest mapped active fault: Segmen Sesar Aktif, 21 km away, slip rate ~15.0 mm/yr (GEM Global Active Faults).