The Pacific plate is moving at a rate of speed of 8.10 cm per year. The Philippine plate is moving at a rate of speed of 6.35 cm per year.
The Philippine Trench (also known as the Manila Trench) is a deep underwater trench that is caused by the collision of two tectonic plates (the Philippine Sea Plate and the Eurasian Plate) east of the Luzon island of the Philippines. The Eurasian Plate is subducting underneath the Philippine Sea Plate at a rate of approx. 16 cm/year. This tectonic activity causes most of the volcanic activity on Luzon, including the cataclysmic eruption of Mt. Pinatubo in 1991.
The Philippine Trench (also known as the Manila Trench) is a deep underwater trench that is caused by the collision of two tectonic plates (the Philippine Sea Plate and the Eurasian Plate) east of the Luzon island of the Philippines. The Eurasian Plate is subducting underneath the Philippine Sea Plate at a rate of approx. 16 cm/year. This tectonic activity causes most of the volcanic activity on Luzon, including the cataclysmic eruption of Mt. Pinatubo in 1991.
in the top of the Australian plate
Mount Pinatubo is above a subduction zone from the philippine plate and the Eurasian Plate, The Philippine Plate is being subducted beneath the Eurasian plate because it is more dense.
It rests on the Philippine plate
The Philippine plate slid under the Eurasian plate.
It is a destructive plate boudary and it is where the Eurasian Plate, the Philippine sea plate and the pacific plate
Volcanoes
Yes the North American plate and Russian Plate.
The Philippine Plate is going under the Eurasian plate.
the Caribbean and cocos plate