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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.
It is a destructive plate boudary and it is where the Eurasian Plate, the Philippine sea plate and the pacific plate
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 eastern side is a boundary with the North American Plate to the north and a boundary with the Philippine Sea Plate to the south, and possibly with the Okhotsk Plate and the Amurian 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.
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.
It is a destructive plate boudary and it is where the Eurasian Plate, the Philippine sea plate and the pacific plate
the Honshu plate where the Pacific, Eurasian and the Philippine sea plate meets
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.
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
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 eastern side is a boundary with the North American Plate to the north and a boundary with the Philippine Sea Plate to the south, and possibly with the Okhotsk Plate and the Amurian Plate.
The Okhotsk Plate is the name of the tectonic plate near Hokkaido, Japan. Its borders are the Pacific Plate, the Philippine Sea Plate, the Eurasian Plate, and the Amurian Plate.
The Philippine Sea Plate lies under the Philippines. It is theorized that this plate is rotating slowly clockwise.
i am not sure. Most of the largest earthquakes in Japan are caused by subduction of the Philippine Sea Plate or Pacific Plate, with mechanisms that involve either energy released within the subducting plate or the accumulation and sudden release of stress in the overlying plate. Earthquakes of these types are especially frequent in the coastal regions of northeastern Japan.
Four Tectonic PlatesJapan lies over 4 tectonic plates. These are: The North American PlateThe Eurasian PlateThe Philippine Sea Plate, andThe Pacific Plate.
The Philippine sea is in the northern hemisphere.