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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.
this is because the oceanic plate is much denser than the continental plate so when they collide the oceanic plate will sink easily
sinks
The pacific plate and the cocos plate
convergence
The Eurasian and Pacific plates collide into the Indian and Australian plates, also known as Indo-Australian plate.
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.
sinks
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.
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.