Two tectonic plates move toward each other at what kind of boundaries?
When two plates move towards each other, they join or join together. The accident between two plates moving towards each other is known as the concurrent boundary. At the point when an oceanic plate meets a mainland plate near a straight line (180°), the result is a subduction zone. There is usually a deep sea channel at the edge of the landmass. Various earthquakes occur along the line of contact between two plates where the oceanic plate and its remnants are eroded. The landmass consists of lava mountains and wells that form along the edge of the mainland due to collisions. A convergent change plate results when an oceanic plate meets a mainland plate at a practically identical point, for example, the San Andreas issue in California. The impact brings about huge destructive earthquakes. When two mainland plates meet, the result is a system of huge crumbling mountains. The exemplary model is the crash between the Indian plate and the Asia plate. The result is the Himalaya Mountains. When two oceanic plates meet over a deep ocean channel, the result is that parts of the two plates are destroyed. The curves (often volcanic) of ocean islands are formed by collision. Whenever, at any point, two plates merge, a concurrent boundary results. Each type of joint boundary leads to consolidation and loss of crustal material.
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