Volcanoes
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 landforms that could develop at a continental and oceanic divergent plate boundary includes; Rifts and Volcanic Mountains.
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.
The Philippine archipelago is primarily formed through tectonic plate movements along the boundaries of the Philippine Sea Plate, Eurasian Plate, Pacific Plate, and the small Philippine Mobile Belt. The collision and subduction of these plates result in the formation of volcanic arcs, trenches, and uplifted regions, creating the diverse landforms and islands that make up the Philippine archipelago.
volcanoes
in the top of the Australian plate
The volcanic landforms at divergent ocean plate boundaries are oceanic ridges.
Plate movements.
The volcanic landforms at divergent ocean plate boundaries are oceanic ridges.
plate tictonics
Mountains, Continents, Volcanoes, Islands, and Fault Lines are the 5 landforms caused by plate movement.
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.
Earthquakes form at a Transform boundary when the plate slips past each other.
mountains, mountain ranges, volcanoes and many other landforms.