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A boundary where two plates meet and collide forming mountains is called a convergent boundary. It is also known as destructive plate boundary.
Convergent boundary.
A convergent boundary causes compressional stress.
A convergent plate boundary occurs between the Nazca Plate and the South American Plate. The Nazca Plate is subducting beneath the South American Plate, leading to the formation of the Andes mountain range.
The Mariana Trench is a convergent boundary, where two tectonic plates are colliding and one plate is forced beneath the other.
convergent
Destructive
convergent
there the same
A convergant boundary is destructive because the plates approach one another.
A boundary where two plates meet and collide forming mountains is called a convergent boundary. It is also known as destructive plate boundary.
It is a convergent/destructive plate boundary.
A convergent boundary is a tectonic plate boundary where two plates collide, often leading to destructive geological processes. For example, when an oceanic plate converges with a continental plate, the oceanic plate is forced beneath, resulting in volcanic activity and earthquakes. This destructive nature of convergent boundaries can reshape landscapes and create mountain ranges over time.
A destructive boundary is a certain type of boundary of a tectonic plate. Destructive boundaries make the plates move toards each other and eventually collide. This is why they are often called collision boundaries.
No, Nyiragongo is not located on a convergent plate boundary. It is situated within the East African Rift system, which is associated with a divergent plate boundary where the African Plate is splitting into two tectonic plates.
Yes, China is located on a destructive plate boundary known as the convergent boundary. This boundary is where two tectonic plates are moving towards each other, resulting in subduction and the formation of mountain ranges like the Himalayas.
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.