In the southwest Pacific Ocean, off the coast of mainland Asia - south of Taiwan and north of Indonesia / Borneo Island, west of the Mariana Islands. The Republic of the Philippines is in Southeast Asia, in the western Pacific Ocean. Taiwan is to the north, Malaysia and Indonesia to the south.
Specifically, the Philippines is located between 116° 40', and 126° 34' E. longitude and 4° 40' and 21° 10' N. latitude and borders the Philippine Sea on the east, the South China Sea on the west, and the Celebes Sea on the south.
The Philippine archipelago is located between 116° 40', and 126° 34' E. longitude and 4° 40' and 21° 10' N. latitude and borders the Philippine Sea on the east, the South China Sea on the west, and the Celebes Sea on the south.
The Philippine sea plate is located under the Philippine Sea, to the east of the Philippines.
In the top of the Australian plate.
pacific plate
pacific plate
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.
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.
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 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
Japan is located near a triple fault line between the Eurasian plate and the Pacific plate (the Japan Trench) and the Philippine plate (the Nankai Trough).
in the top of the Australian plate
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.
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.
There are three main types of plate boundaries:Convergent--coming together, hitting one anotherDivergent--moving apart, separating from one anotherTransform--sliding past one another laterally
It rests on the Philippine plate
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 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.