Mw 5.4 Earthquake Strikes the Southeastern Korean Peninsula
- EOS News
In the early evening of 12 September 2016, a moderate earthquake (Mw 5.4) struck the southeastern coast of South Korea, about 50 minutes after a Mw 4.9 foreshock. The tremor was strong enough to be felt across South Korea and the northern coast of Kyushu, Japan. Photographs shared on social media showed minor damage in nearby cities, mostly in the form of fallen plaster and ceilings, and minor ground cracks.
The tremor also resulted in panic in the Gyeongju area, a popular tourist destination in South Korea close to the earthquake’s epicentre. Usually, magnitude-5.4 earthquakes do not cause significant damage. However, in a region where seismic hazards are not properly mitigated, which is not uncommon in regions where earthquakes are rare, a magnitude-5.4 event can produce considerable damage.
According to the United States Geological Survey, the earthquake’s epicentre is 8 kilometres (km) south of Gyeongju, also known as Kyongju (35.769°N, 129.227°E). The magnitude of this earthquake (Mw 5.4) is about 1.4 times greater than the recent man-made explosion in North Korea, which was felt in the northern part of the Korean Peninsula and along the North Korea-China border. Although the timing of both events are close, the distance between them and their magnitudes suggest that they are unrelated.
The seismic analysis of the Mw 5.4 earthquake, conducted by Japan’s National Research Institute for Earth Science and Disaster Resilience (NIED), suggests that this quake was caused by rupture of a strike-slip fault within the shallow layers of the Earth’s crust, where the ground on both sides of the fault move horizontally in opposite directions. Given the location of the epicentre and its strike-slip focal solution, it is believed that this earthquake is likely to have been generated by one of the NNE-SSW right-lateral active faults in the southeastern coast of South Korea.
Although the slip rates of active faults in South Korea are generally very low (i.e. < 0.1 mm/yr), are very difficult to be detected and monitored by modern GPS and satellite technology, and the region was not considered to be earthquake-prone, written history informs us that the Korean Peninsula had been struck by more than 300 moderate earthquakes (magnitudes < 7.0) in the past 2,000 years. Many of these events had occurred in the southern part of the Peninsula, and were strong enough to cause damage to the cities close by.
The slow activity of the fault in this area, together with historical records of the region's earthquake occurrence, suggest that the Korean Peninsula is not completely seismically quiet. Even though it is more than 500 km away from major plate boundary faults, the on-going tectonic motions between the Philippine Sea plate and the Eurasian plate, as well as the tectonic deformation within northern China, are producing notable deformations in the peninsula, and reactivating the ancient fault in South Korea’s intraplate environment.