What are the 3 types of convergent boundaries?
Convergent boundaries , where two plates are moving toward each other, are of three types, depending on the type of crust present on either side of the boundary — oceanic or continental . The types are ocean-ocean, ocean-continent, and continent-continent.
What type of convergent boundaries make volcanoes?
Convergent boundaries know as subduction zones create volcanos by forcing a plate under another plate melting the plate and creating the pressure that results in a volcano.
Do volcanoes form at convergent or divergent boundaries?
Sometimes, the plates collide with one another or move apart. Volcanoes are most common in these geologically active boundaries. The two types of plate boundaries that are most likely to produce volcanic activity are divergent plate boundaries and convergent plate boundaries.
What is the difference between a convergent and divergent boundary?
Divergent boundaries — where new crust is generated as the plates pull away from each other. Convergent boundaries — where crust is destroyed as one plate dives under another.
What are some examples of convergent boundaries?
Examples. The collision between the Eurasian Plate and the Indian Plate that is forming the Himalayas. Subduction of the northern part of the Pacific Plate and the NW North American Plate that is forming the Aleutian Islands. Subduction of the Nazca Plate beneath the South American Plate to form the Andes.
What are two examples of convergent boundaries?
What are the non examples of convergent boundaries?
Explanation: Examples of non-convergent boundaries include “Mid-Atlantic Ridge and Great Rift Valley”. Iceland is an example of country undergoing continental non-convergent boundaries. Convergent boundaries are the boundaries between “two or more tectonic plates” which are coming towards each other.