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The Philippine Sea plate or the Philippine plate is a tectonic plate comprising oceanic lithosphere that lies beneath the Philippine Sea, to the east of the Philippines.Most segments of the Philippines, including northern Luzon, are part of the Philippine Mobile Belt, which is geologically and tectonically separate from the Philippine Sea plate.
The Philippine Mobile Belt (also called as Taiwan–Luzon–Mindoro Mobile Belt [11]) is a complex tectonic zone which sits at the convergence zone of the Eurasian plate, Philippine Sea plate, and Indo-Australian plate. [9] It covers the whole Philippine archipelago and extends southwards to the Molucca Sea and eastern Indonesia.
Much of the Philippines lie within the area of strongly tectonised blocks of mainly island arc origin, known as the Philippine Mobile Belt. To the east, Philippine Sea plate is subducting beneath the mobile belt along the line of the Philippine Trench and the East Luzon Trench at the northern end of the belt.
The North Luzon Trough formed as a result of the oblique convergence between the Eurasian and Philippine Sea plates. [citation needed] The Philippine Sea Plate is subducting beneath the Eurasian Plate at a rate of approximately 80 millimeters per year (3.1 inches per year). This oblique convergence creates a complex tectonic setting, with both ...
The Philippine Sea is a marginal sea of the Western Pacific Ocean east of the Philippine Archipelago (hence the name) and the largest sea in the world, occupying an estimated surface area of 5 million square kilometers (2 × 10 ^ 6 sq mi). [1] The Philippine Sea Plate forms the floor of the sea. [2]
Here, the Pacific plate is being subducted beneath the Philippine Sea plate, creating the Izu Islands and Bonin Islands on the Izu–Bonin–Mariana Arc system. [ 3 ] It is 9,826 metres (32,238 ft) +/- 11m at its deepest point and first dived to its base on August 13, 2022, during a joint Caladan Oceanic/University of Western Australia ...
Major physiographic elements of the Philippine Mobile Belt Puerto Princesa Subterranean River National Park marker describing the geologic history of the Philippines. In the 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.
The Manila Trench was formed by the subduction of the Eurasian Plate underneath the Philippine Sea Plate, which initiated during the Middle Miocene (22-25 million years ago). A characteristic feature of this plate boundary is the gradual change from normal subduction (on the southern margin) to a collisional regime (on the northern margin ...