- Philippine Plate
The Philippine Plate is a
tectonic plate beneath thePacific Ocean to the east of thePhilippines . The Philippine plate comprises oceaniclithosphere that lies beneath thePhilippine Sea , and so is often referred to as the Philippine Sea Plate because most of thePhilippines lie west of this plate. The plate is bounded by thePhilippine Trench to the southwest,Taiwan and theRyukyu islands to the northwest,Japan to the north, the Izu-Ogasawara (Bonin) andMariana islands to the east, andYap ,Palau , and easternmostIndonesia (Halmahera } to the south. The eastern part of the plate is occupied by theIzu-Bonin-Mariana Arc system.The easterly side of the Philippine Sea Plate is a
convergent boundary with the subductingPacific Plate . The Philippine Plate is bounded on the west by theEurasian Plate , on the south partly by theCaroline Plate , on the north by theNorth American Plate and possibly by theAmurian Plate .Collision of the Philippine Plate and the Eurasian Plate formed
Taiwan and continues today. In the northernmost part of the plate, thickened crust of the Izu-Bonin-Mariana arc is colliding with Japan to form theIzu Collision Zone .The Philippine Plate forms the floor of this sea and it is one of the 5 minor lithospheric plates, about the size of the Arabian plate (Anderson, 2002). It is unique among all of the plates that now exist on Earth because it is completely surrounded by subduction zones. The Philippine Sea Plate is divided into a western “trapped” and inactive half and an eastern part that formed and continues to grow as a result of westward subduction of the Pacific Plate. The western half is doomed to disappear someday because it is being subducted to the west and north under the Eurasian Plate. This eastern half is composed of several N-S ridges (from W to E: Kyushu-Palau Ridge (KPR), Parece Vela-Shikoku West Marian Ridge (WMR large backarc basins (Fig. 1). The Izu-Ogasawara (Bonin) and Mariana islands and submarine volcanoes is sometimes referred to as the IBM (Izu-Bonin-Mariana) arc system.
The
Izu Peninsula is the northernmost tip of the Philippine Plate. The Philippine Plate, the Eurasian Plate (or the Amurian Plate), and the North American or Okhotsk Plate meet atMount Fuji .Mount Pinatubo eruption - 15th June 1941After the days before of smaller eruptions on the 15th of June 1941 the mountain exploded. Ash was sent 100,000 feet in to the air andPyroclastic flows were forming in all directions. No lava exited the volcano in this eruption, for it was such a forceful one that ash clouds came instead.Mount Pinatubo is in the
Philippines .References
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