Convergent boundary
A convergent plate boundary is the boundary that occurs when two plates collide each other either a continental plate with continental plate or oceanic plate.[1] This causes very large earth movements. Plate collision can produce earthquakes, volcanoes, the formation of mountains, and other geological events over time.[2] 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.
![]() Oceanic-continental |
![]() Continental-continental |
![]() Oceanic-oceanic |
The diagram shows some differences between the two types of subduction.
- 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.
- 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.
References
- "Batas Lempeng Konvergen, Divergen dan Transform". Gurugeografi.id. Retrieved 2020-10-10.
- "Apakah Batas Lempeng Konvergen? ยท www.greelane.com - Sumber Daya Pendidikan Terbesar di Dunia". www.greelane.com - Sumber Daya Pendidikan Terbesar di Dunia (in Indonesian). 2019-07-15. Retrieved 2020-10-10.
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