Home » Special Events » Magnitude 8.0 earthquake in the Samoa Islands region, Pacific Ocean

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last updated: 09/29/09 13:45.26 (PDT)

On Tuesday September 29 2009 at 10:48 AM (PDT) the USArray seismic network recorded an earthquake (preliminary Mw 8.0) located in the Samoa Islands region, Pacific Ocean.

Initial source parameters for this tremor are indicated below. The epicentral distance (i.e. distance separating the epicenter and the closest station in the recording network, SCI2) for the USArray is 7830 km (70.34 degrees).

If you felt the quake, the USGS would like to know. Please add your comments to the USGS page "Did you feel it?".

Summary

Global map view
Solution Parameters
Local Date:Tuesday September 29, 2009
Local Time:10:48 AM PST
Universal Time:09/29/09 (272) 17:48.11 UTC
Magnitude:8.0 Mw
Latitude:-15.5580
Longitude:-172.0730
Depth:18 km
Author:USGS NEIC
Authoritative:yes

Proximity to Population Centers

  • 185 km (115 miles) ENE of Hihifo, Tonga
  • 195 km (125 miles) S of Apia, Samoa
  • 705 km (435 miles) NNE of Nuku'Alofa, Tonga
  • 2700 km (1670 miles) NNE of Auckland, New Zealand

Maps

Mercator projection regional view

The red star denotes the earthquake epicenter. Triangle symbols are active stations at the time of the earthquake in the USArray (excluding ANSS backbone stations and GSN stations, which are represented by a diamond symbol) and colored by network. Gray lines are major rivers.

Regional map view
Network Legend
 Transportable Array (TA)
 UC San Diego (AZ)
 CalTech (CI)
 Uni. Utah (UU)
 ANSS backbone stations (US)
 Global Seismograph Network (IU)

Regional satellite view

The red marker denotes the earthquake epicenter.

Detailed terrain view

The red marker denotes the earthquake epicenter.

Current seismic activity measured by USArray

Click the links below to observe near real time maps of earthquakes recorded by the USArray deployment:

Further information

Learn more about the Array Network Facility (ANF) component of USArray, the USArray experiment, the EarthScope project, and the Incorporated Research Institutions for Seismology (IRIS).