Significant Earthquake

Date Earthquake Location Earthquake Parameters
Focal
Depth
Magnitude MMI Int
Year Mo Dy Hr Mn Sec Name Latitude Longitude Mw Ms Mb Ml Mfa Unk
2009 9 29 17 48 10.9 SAMOA ISLANDS -15.489 -172.095 18 8.0 8.1 7.1
Significant Earthquake
Earthquake Effects Total Effects (Earthquake and Tsunami, Volcano, etc.)
Deaths Missing Injuries Damage Houses
Destroyed
Houses
Damaged
Deaths Missing Injuries Damage Houses
Destroyed
Houses
Damaged
Num De Num De Num De $Mill De Num De Num De Num De Num De Num De $Mill De Num De Num De
192 3 7 1 275.000 4


Comments for the Significant Earthquake

Comments for the Significant Earthquake

Display listing of nearby significant earthquakes

Felt Reports

At least 149 people killed in Samoa, 34 killed in American Samoa and 9 killed, 7 injured and 500 displaced on Niuatoputapu, Tonga. Widespread damage to infrastructure occurred at Pago Pago, American Samoa, in many parts of Samoa and on Niuatoputapu, Tonga. Nearly all of the casualties and damage was caused by large tsunamis, with run up heights of 12 m at Poloa, 7 m at Pago Pago and Tula, American Samoa and 3 m on Niuatoputapu. Felt (V) at Apia, Samoa and (IV) at Ili`ili and Tafuna, American Samoa. Felt in much of American Samoa, Samoa and northern Tonga and as far away as Wallis and Futuna Islands.

Tectonic Summary

The broad-scale tectonics of the Tonga region are dominated by the relative convergence of the Pacific and Australia plates, with the Pacific plate subducting westward beneath the Australia plate at the Tonga trench. At the latitude of the earthquake of September 29, 2009, the Pacific plate moves westward with respect to the interior of the Australia plate at a velocity of about 86 mm/year. The earthquake occurred near the northern end of a 3,000 km long segment of the Pacific/Australia plate boundary that trends north-northeast.; farther north of the earthquake’s source region, the plate boundary trends northwest and then west. The eastern edge of the broad Australia plate may be viewed as a collection of small plates or microplates that move with respect to each other and with respect to the Pacific plate and the Australia plate interior.

On the basis of currently available location and fault mechanism information, we infer that the September 29 earthquake occurred as a normal fault rupture on or near the outer rise of the subducting Pacific plate.

The broad-scale Australia/Pacific plate boundary is one of the most active earthquake regions in the world. Earthquakes occur on the thrust-fault boundary between the Australia and Pacific plates, within the Pacific plate on both sides of the trench, and within and on the boundaries of the small plates that compose the eastern edge of the overall Australia plate.

(above from reference #1053)


References for the Significant Earthquake

References for the Significant Earthquake

ID Author Year Citation
1053 National Earthquake Information Center (NEIC) 1971 to present Preliminary Determination of Epicenters (PDE), a weekly and monthly publication, National Earthquake Information Center, U.S. Geological Survey, Golden, Colorado, 1971 to present.
8555 Lay, Thorne, Charles J. Ammon, Hiroo Kanamori, Luis Rivera, Keith D. Koper and Alexander R. Hutko 2010 The 2009 Samoa–Tonga great earthquake triggered doublet. Nature, vol. 466, no. 19, p. 964–968. DOI:10.1038/nature09214
8556 Beavan, J., X. Wang, C. Holden, K. Wilson, W. Power, G. Prasetya, M. Bevis and R. Kautoke 2010 Near-simultaneous great earthquakes at Tongan megathrust and outer rise in September 2009. Nature, vol. 466, no. 19, p. 959-963, DOI:10.1038/nature09292