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The 2012 Negros earthquake occurred on February 6 at 11:49 PST, with a body wave magnitude of 6.7 and a maximum intensity of VII (Destructive) off the coast of Negros Oriental, Philippines. The epicenter of the thrust fault earthquake [6] was approximately 72 kilometres (45 mi) north of Negros Oriental's provincial capital, Dumaguete. [7] [8] [9]
A magnitude 6.7 earthquake struck near island of Negros, and Cebu, Philippines on February 6, at a depth of 20 km, killing 113 people. [19] [20] [21] A magnitude 6.0 earthquake struck near the island of Negros, on February 6, at a depth of 15 km. [22] A magnitude 6.0 earthquake struck west coast of Quepos, on February 13, at a depth of 11 km. [23]
2010 Mindanao earthquakes triplet earthquake, deep focus events [19] 2012 February 6 11:49 Negros 6.7 VII 113 dead, 112 injured 2012 Negros earthquake [20] 2012 August 31 20:47 Samar 7.6 VII 1 dead, 1 injured 2012 Samar earthquake [21] 2013 October 15 08:12 Bohol 7.2 IX 222 dead, 976 injured 2013 Bohol earthquake [22] 2017 February 10 22:03 ...
February 6, 2012 03:49 Negros–Cebu region, Philippines see 2012 Visayas earthquake: 9.964 123.246 51 dead 62 missing 6.7 M w (USGS) Centred 72 km north of the Dumaguete, Negros, Philippines, at a depth of 11 km. [38] March 14, 2012 12:05 Near the east coast of Honshu, Japan see 2012 Chiba earthquake: 35.687 140.695 1 6.0
2012 Negros earthquake; Y. 2012 Yangzhou earthquake; 2012 Yiliang earthquakes This page was last edited on 7 September 2023, at 22:15 (UTC). Text is available under ...
The Negros trench was formed from subduction of the Eurasian Plate underneath the Philippine Sea plate which initiated during the Early Miocene (23.03-20.44 million years ago), The trench was previously the site of a collision zone with the Palawan plate, which formed the Philippine Trench 8–9 million years ago, This trench is located west of the Visayan Islands.
The 2013 Bohol earthquake was a deadly event which happened on 15 October, striking the provinces of Bohol, Cebu, Negros Oriental, Masbate and Leyte. The M w 7.2 earthquake produced a ~50-km-long, ~12-km-wide northeast trending zone of uplift with an ~8-km-long discontinuous ground rupture indicating predominantly reverse-slip movement on a ...
The tsunami generated by the 1976 earthquake caused about 4,000 deaths on Mindanao. Modelling of likely further tsunamis along the Cotabato Trench suggests that run-ups of several metres are likely for future earthquakes similar in size to the 1976 event.