Linked from

The 21 pages that link to Philippine Sea Plate, each with the reason it gives.

• Eurasian PlateRelated: Its subduction beneath the Eurasian margin helps form island arcs and deep trenches in East Asia.

• LuzonRelated: Plate interactions east of Luzon contribute to earthquakes and volcanic activity.

• Nankai TroughRelated: Its convergence drives subduction along the trough.

• Great Kantō EarthquakeRelated: Its motion beneath central Japan drives earthquakes near the Sagami Trough.

• Izu–Bonin–Mariana arcRelated: It is the overriding plate beneath which the Pacific Plate descends.

• Sulu SeaRelated: Plate motions help explain the region’s basin structure and volcanic margins.

• Philippine archipelagoRelated: Its westward subduction helps shape trenches and volcanic arcs east of the islands.

• Philippine SeaRelated: Its movement helps define the sea’s western and eastern tectonic boundaries.

• Izu PeninsulaRelated: Its motion brought the Izu volcanic arc into collision with central Honshu.

• Japanese island arcRelated: It subducts beneath southwestern Japan, shaping the Ryukyu and Nankai margins.

• Miura PeninsulaRelated: Its motion beneath the region contributes to the peninsula’s tectonic activity.

• Taal VolcanoRelated: Regional plate convergence contributes to the volcanism of the Philippine archipelago.

• Central Mountain RangeRelated: Its collision with the Eurasian Plate drives uplift in Taiwan’s mountains.

• Izu IslandsRelated: Its interaction with the Pacific Plate drives volcanism beneath the island chain.

• Mount AsoRelated: Its descent contributes to the magma-generating tectonic setting beneath Kyushu.

• Median Tectonic LineRelated: Its subduction shapes present-day deformation near the southern end of the fault system.

• Hualien CountyRelated: Plate convergence helps explain the region’s steep relief and frequent earthquakes.

• Itoigawa-Shizuoka Tectonic LineRelated: Its interaction with nearby plates helps complicate central Japan’s tectonics.

• Philippine TrenchRelated: Its westward descent beneath the Philippine Mobile Belt drives trench formation.

• Babuyan IslandsRelated: Its interaction with surrounding plates contributes to regional volcanism.