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On Luzon, the fault zone splays out into a number of different faults, including the Digdig Fault. One of the largest historical earthquake on the fault zone was the 1990 Luzon M s 7.8 event that left nearly 2,000 people dead or missing. The same part of the fault zone is thought to have ruptured in the 1645 Luzon earthquake. [7]
Among subduction zones in the Philippines, subduction along the Philippine Trench produces the most active and frequent seismic activities to the region. However, as the Philippine Trench is a young subduction system, the majority are shallow earthquakes (less than 30 km [ clarification needed ] ).
These tectonic plates have compressed and lifted parts of the Philippines causing extensive faulting, primarily on a north–south axis. All faults in the Philippines are inter-related by the tectonic forces of the Philippine Mobile Belt, or its tectonic induced volcanism. A more complete understanding can be gained by viewing the faults in the ...
A convergent zone borders an estimate of 45% of the Philippine Trench today. [ 15 ] Although there are vast areas of subduction zones, some authors have considered this region to have low seismic activity , [ 17 ] though the USGS has recorded many earthquakes with magnitude ≥ 7.2 in the region as shown by the map to the side.
Along this trench the oceanic crust of the Sunda Plate beneath the Celebes Sea is being subducted beneath the Philippines Mobile Belt. It forms part of a linked set of trenches along the western side of the Philippines formed over east-dipping subduction zones, including the Manila Trench and the Negros Trench . [ 1 ]
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 ...
There has been a decent amount of earthquakes with a magnitude ≥7.0 in the region, with the most recent occurring in 1994. It hit the trench in a depth of 15.0 km. Areas adjacent to the subduction zones have experienced large seismic activity. [citation needed] Significant earthquakes which are 7.0± related to the Luzon Trough:
The 1948 seismic codes were prepared in consideration of the seismic zone map. A new code was revised in 1961 and in 1963, the seismic zonation map was updated with four hazard levels based on predicted shaking on the Modified Mercalli intensity scale. It was subsequently added a fifth hazard level in the 1972 revision. [12]