Geology Of The Philippines
The Philippine Mobile Belt is a complex portion of the tectonic boundary between the Eurasian Plate and the Philippine Sea Plate, comprising most of the country of the Philippines. It includes two subduction zones, the Manila Trench to the west and the Philippine Trench to the east, as well as the Philippine Fault System. Within the Belt, a number of crustal blocks or microplates which have been sheared off the adjoining major plates are undergoing massive deformation.
Most segments of the Philippines, including northern Luzon, are part of the Philippine Mobile Belt, which is separate from the Philippine Sea Plate to the east, the Molucca Sea Collision Zone to the south, Sunda Plate to the southwest, and the South China Sea Basin to the west and north-west. To the north it ends in eastern Taiwan, the zone of active collision between the North Luzon Trough portion of the Luzon Volcanic Arc and South China. The Philippine Mobile Belt has also been called the Philippine Microplate and the Taiwan-Luzon-Mindoro Belt.
Read more about Geology Of The Philippines: Palawan and Sulu, East and West Boundaries, Northern Terminus, Southern Terminus, Luzon, Collage of 17 Principal Blocks, See Also