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PHIVOLCS FaultFinder – This web app is a product of the joint collaboration between PHIVOLCS, DOST, GSJ, AIST. It was developed by Dr. Joel C. Bandibas of GSJ with the cooperation of the research and development personnel of PHIVOLCS. Media related to Marikina Valley Fault System at Wikimedia Commons
PHIVOLCS Observatory at Mount Hibok-Hibok.. The Philippine Institute of Volcanology and Seismology (PHIVOLCS, Tagalog:; Tagalog: Surian ng Pilipinas sa Bulkanolohiya at Sismolohiya [2]) is a Philippine national institution dedicated to provide information on the activities of volcanoes, earthquakes, and tsunamis, as well as other specialized information and services primarily for the ...
The Philippine fault system is a major inter-related system of geological faults throughout the whole of the Philippine Archipelago, [1] primarily caused by tectonic forces compressing the Philippines into what geophysicists call the Philippine Mobile Belt. [2]
2 Phivolcs FaultFinder. 1 comment. Toggle the table of contents. Talk: Marikina Valley Fault System. Add languages. Page contents not supported in other languages.
There was a foreshock which preceded the main quake, recorded M w 4.8 at 7:28 AM PST by Philippine Institute of Volcanology and Seismology with a PHIVOLCS Earthquake Intensity Scale of IV (Moderately Strong). [2] The foreshock lasted 10–15 seconds which made people feel dizzy and nauseated.
Earthquakes in the Philippines and adjacent areas 1900 to 2012 Earthquakes in the Philippines and adjacent areas 1500 to 1899. Much of the Philippines lie within the area of strongly tectonised blocks of mainly island arc origin, known as the Philippine Mobile Belt.
The Bohol fault system is a reverse fault system in Bohol province, Philippines. This fault system contains three segments: the newly found North Bohol Fault following the 2013 Bohol earthquake, [2] the South Offshore Fault, [3] and the East Bohol Fault.
The 7.1 magnitude earthquake was registered at 3:41 p.m. by the Philippine Institute of Volcanology and Seismology (PHIVOLCS) and determined it to be of tectonic origin. . The depth of focus was measured at 15 kilometers (9 miles) and its epicenter was located in the vicinity of Culasi, Antique.