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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 ...
Feeling the earth move under one's feet can be unsettling, even in places like California, where it's a natural and fairly common occurrence. But far more disconcerting is when major tremors in ...
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 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 ...
Sulawesi lies within the complex zone of interaction between the Australian, Pacific, Philippine and Sunda plates in which many small microplates are developed. The main active structure onshore in the western part of Central Sulawesi is the left-lateral NNW-SSE Palu-Koro strike-slip fault that forms the boundary between the North Sula and Makassar blocks.