Philippine Sea Plate

But the Philippine Sea Plate is unusual in having no such ridge.

It was an intra-plate earthquake inside the Philippine Sea Plate.

Such large intra-plate earthquakes inside the Philippine Sea Plate are not very common in this region.

Volcanic activity in the region is thought to be related to subduction of the Philippine Sea Plate.

It has been suggested that this earthquake was related to the dehydration of the Philippine Sea Plate slab.

This earthquake is a normal faulting in-slab event within the subducting Philippine Sea Plate.

Along the border with the Philippine Sea Plate is a convergent boundary that transitions into a rift.

The fault, a few dozen miles from land, lies near the boundary where the Philippine sea plate is pushed beneath the Eurasian plate.

It is separated from the Philippine Sea Plate by a long divergent boundary with numerous transform fault offsets.

The Izu Peninsula is located in the northern tip of the Philippine Sea Plate.

They lie above a subduction zone between the Pacific Plate and the Philippine Sea Plate.

The IBM arc system is part of the Philippine Sea Plate, at least to the first approximation.

It developed where the Philippine Sea Plate is subducting under the Eurasia Plate.

They are formed by subduction of the Pacific Plate and the Philippine Sea Plate.

This trench lies between the Philippine Sea Plate and the Eurasian Plate.

The Philippine Sea Plate is subducting along the Philippine Trench in this region.

This marks the place where the Philippine Sea Plate moves under the Eurasian Plate.

Taiwan is part of the collision zone between the Yangtze Plate and Philippine Sea Plate.

Both mark the boundary of the Philippine Sea Plate subducting under the Amurian Plate.

This earthquake was an intraplate earthquake greater than 50 kilometers to the east of the boundary of the Philippine Sea Plate.

A subduction zone where the Pacific Plate is being subducted under the Philippine Sea Plate.

They are separated, with their continuity interrupted and displaced, by Benham Plateau on the Philippine Sea Plate.

The island experiences occasional earthquakes due to its location on the western edge of the Pacific Plate and near the Philippine Sea Plate.

The 1703 earthquake is thought to have involved rupture of the interface between the Eurasian Plate and the Philippine Sea Plate.

This earthquake was unusual in that it occurred as a result of reverse faulting within the oceanic lithosphere of the Philippine Sea Plate.