Convergent boundary

A convergent plate boundary is where two or more tectonic plates meet. This causes very large earth movements. It also forms mountains, hills, and volcanoes. The Himalayas were formed by such a collision. Earthquakes and volcanoes are common near convergent boundaries. This is because of pressure, friction, and plate material melting in the mantle.


The diagram shows some differences between the two types of subduction.

  1. Oceanic crust moves under. A deep ocean trench forms at the coast, and an arc of mountainous volcanoes forms inland. Seen along the west edge of the Americas.
  2. Continental crust moves under. The edge of the continental plate folds into a huge mountain range. Behind it is a high plateau. The Himalayas and the Tibetan plateau are a perfect example of this.
Other Languages
العربية: حدود متقاربة
čeština: Aktivní okraj
فارسی: مرز همگرا
한국어: 수렴 경계
Bahasa Indonesia: Batas konvergen
íslenska: Flekamót
Kreyòl ayisyen: Limit konvèjan
日本語: 収束型境界
português: Limite convergente
slovenčina: Aktívny okraj
srpskohrvatski / српскохрватски: Konvergentna granica
Tiếng Việt: Ranh giới hội tụ