March 29, 2015 Earthquake: Papua New Guinea

Felt (VI) at Kokopo. Also felt at Kerema and Rabaul. Felt at Helensvale, Australia. A tsunami with a wave height of 3 cm above the tide level was recorded at Tarekukure Wharf.

The March 29, 2015, M 7.5 earthquake southeast of Kokopo, Papua New Guinea, occurred as the result of thrust faulting on or near the plate boundary interface between the subducting Australia and overriding Pacific plates. At the location of the earthquake, the Australia plate moves towards the east-northeast at a velocity of 105 mm/yr with respect to the Pacific plate, and begins its subduction into the mantle beneath New Britain and New Ireland at the New Britain Trench south of the earthquake. The moment tensor and depth of the event are consistent with thrust-type motion on the interface between these two plates. Note that at the location of the earthquake, some researchers consider the edges of the Australia and Pacific plates to be divided into several microplates that take up the overall convergence between Australia and the Pacific, including the Solomon Sea and South Bismark microplates local to this event. The Solomon Sea microplate moves slightly faster and more northeasterly with respect to the Pacific plate than does the Australia plate due to sea-floor spreading in the Woodlark Basin several hundred kilometers to the south of the March 29th earthquake, facilitating the classic subduction evident beneath New Britain and New Ireland.

While commonly plotted as points on maps, earthquakes of this size are more appropriately described as slip over a larger fault area. Thrust-faulting events of the size of the March 29, 2015, earthquake are typically about 80x40 km (length x width); modeling of this earthquake implies dimensions of about 100x70 km, predominantly up-dip of the hypocenter.

The plate boundary between the Australia and Pacific plates in the Papua New Guinea region is very active seismically; 36 M 7+ events have occurred within 250 km of the March 29, 2015, earthquake over the past century. Few are known to have caused shaking-related fatalities because of the remoteness of the region, though a M 8.0 earthquake in November 2000, one of three similarly sized events over a 2-day period, did cause several deaths. The largest nearby earthquake was a M 8.1 event, 70 km to the east of the March 29, 2015, earthquake, and was one of two M 8+ earthquakes 140 km apart in July 1971.

Hayes et al. (2016) Tectonic summaries of magnitude 7 and greater earthquakes from 2000 to 2015, USGS Open-File Report 2016-1192. (5.2 MB PDF)

Felt (VI) at Kokopo. Also felt at Kerema and Rabaul. Felt at Helensvale, Australia. A tsunami with a wave height of 3 cm above the tide level was recorded at Tarekukure Wharf. Kokopo, East New Britain, Papua New Guinea - CDI: 6; Rabaul, East New Britain, Papua New Guinea - CDI: 5; Kerema, Gulf, Papua New Guinea - CDI: 4; Helensvale, Queensland, Australia - CDI: 2 (reference #13456)

Officials in the capital, Port Moresby, were working to contact their counterparts in the outer provinces, but hours after the quake, there still had been no reports of damage or injuries, said Mose, of the national disaster center. He said he was confident the nation had averted a major catastrophe. The quake caused strong shaking and knocked items off shelves in Kokopo, and was felt 800 kilometers (500 miles) away in Port Moresby, said Chris McKee, assistant director of the Geophysical Observatory in Port Moresby. (reference #11197)