The convergent plate boundaries are characterized by the moving of plates towards each other. his leads o the collision of plates and lighter plates such as the continental plates rise above the heavier such as the oceanic plate and which in turn leads to the formation of volcanic eruptions, earthquakes, and crustal deformations. Through the process of slab push and slab pull the plate margins experiences massive geologic changes. The process creates a heavier plate to enter into the asthenosphere and melt at a very fast rate. The burning plate produces tremors with the release of fluids from the rocks. The molten rocks rise up violently to form volcanoes, often builds island arc along the boundaries. An example of the Pacific and North American plate that is moving towards the west. The force that makes the plate dive deep into the mantel is called subduction. The zone where it takes space is called the subduction zone. They can be found at a depth of 160 km and lead to magma chambers. Normally the older plate tends to get subducted easily as compared to the younger plate. This boundary where the plates collide is called an interactive plate boundary.Thus, earthquakes with an increasing depth towards the oceanic plate are found along the margins of the plate. The earthquake's activity is shallow along the continental margins but increases its intensity as the slab goes deeper. Thus volcanic activity along with earthquakes are commonly found.

Answered: continental crust

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Question

Which of the following characteristics would you expect at convergent plate margins that contain oceanic crust on one plate and continental crust on the other?
		mountains forming
		earthquakes with increasing depth toward the oceanic plate
		a spreading center
		All of the characteristics might be expected.
		None of the answers is correct.

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