The more dense plate subducts (goes under) the less dense plate.
For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
The Eurasian and Pacific plates collide into the Indian and Australian plates, also known as Indo-Australian plate.
sinks
Convergent Boundary.
the plates will push each other up and form a mountain range.
when 2 plates collide and form a "little hill "
The more dense plate subducts (goes under) the less dense plate. For example if continental and oceanic crust collide oceanic crust will go underneath the continental.
The movement or action of the plate determines what type it is. When two plates collide, they are creating a convergent boundary. Therefore you could state that they are convergent (or colliding) tectonic plates.
The Eurasian and Pacific plates collide into the Indian and Australian plates, also known as Indo-Australian plate.
sinks
this is because the oceanic plate is much denser than the continental plate so when they collide the oceanic plate will sink easily
sinks
sinks
sinks
The pacific plate and the cocos plate
Eurasian Plate, African Plate, and Arabian Plate.
Convergent boundary
this depends on the two plates that collide. Ocean plates are much heavier than continental plates. If an ocean and continental plate collide, the ocean plate sinks underneath and creates a trench. If two ocean plates or two continental plate collide, it creates a mountain range/ oceanic ridge depending on the type.