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Convergent boundaries is where two plates (a continental plate and the ocean floor) get "pushed together" by subduction. If they have the same density, they will be pushed up together creating a mountain (the Himalaya's mountain is a great example). If the plates have different density then the one with more density overlaps the other.
There is an example of all of the boundaries. Hope this helps!
In plate tectonics, a convergent plate boundary marks the point where two plates move towards each other to either form a mountain or a zone of subduction depending on the density of the plates.
- Plates move towards each other at convergent plate boundaries, while the divergent boundary marks the point where plates move away from each other.
- When the converging plates have equal density, none will be pushed downward due to equality, hence, the two plates push upwards to form a mountain.
- On the other hand, when plates of different densities converge, the lower density plate is pushed downward to for a zone of subduction.
Therefore, mountains are formed by plates of equal densities while a zone of subduction ensues when plates of unequal densities collide.
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