収束型境界
1. Convergent boundaryIn plate tectonics, a convergent boundary, also known as a destructive plate boundary, is an actively deforming region where two (or more) tectonic plates or fragments of lithosphere move toward one another and collide. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries. When two plates move towards one another, they form either a subduction zone or a continental collision.
Read “Convergent boundary” on English Wikipedia
Read “収束型境界” on Japanese Wikipedia
Read “Convergent boundary” on DBpedia
Read “Convergent boundary” on English Wikipedia
Read “収束型境界” on Japanese Wikipedia
Read “Convergent boundary” on DBpedia
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