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Seismic Event Dossier23:45 Local (14:22 UTC)(baru saja)

M 8.2 earthquake Papua, Indonesia

A magnitude 8.2 (MW) earthquake occurred on 1914-05-26, 23:45 local time (14:22 UTC) (baru saja), centered 135 km SE of Biak (Indonesia). The hypocenter was located at a shallow depth of 15 km. Primary telemetry verified by USGS.

Historical Landmark Earthquake

#40 of All Time

Curated Global Seismic Archive (1700–Present)

Top-100 Earthquakes

A magnitude 8.2 earthquake struck ⁨Papua, Indonesia⁩ on 26 Mei 1914. Documented deaths: 101–1,000.

Documented Fatalities101–1,000Source: NOAA NCEI Significant Earthquake Database
Fault KinematicsActive fault
Equivalent Energy30.09 Mt TNT

Magnitudo

MW
M 8.2

30.09 Mt TNT

Kedalaman

15 km
15 km

shallow (Kerak dangkal)

Dampak PAGER

red
> 1,000 fatalities

Luka-luka: > 5,000 · ~42.2M merasakan

Peta Interaktif Episenter & Sesar

1.98°S, 136.94°E
Sesar5 km
Segmen Sesar Aktif
Slip · ~15.0 mm/yr
Felt byMMI III+
~42.2M exposed
~16.7M strong shaking
Primary SolutionUSGS
USGS#iscgem913984reviewed
1 agencies reporting
Setting2.0°S
Indonesia
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 utama26 Mei, 0426 Mei, 1627 Mei, 0427 Mei, 1628 Mei, 0428 Mei, 1629 Mei, 0429 Mei, 16M8.2
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
M8.2(Mw)Ref
15.0 kmRef
-1.98°, 136.94°Origin
Authoritative
iscgem913984

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

3 permukiman

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

TownDistanceIntensity
Biak · Papua135 kmMMI VIII
Nabire · Papua220 kmMMI VII
Timika · Papua286 kmMMI VII

Tectonic setting

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