Now, it's the boundary you've been waiting for, convergent boundary. In a convergent boundary, 2 plates collide.
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In a continental-continental crust, a convergent boundary creates mountains. When the 2 plates collide, they build up on each to form mountains. Because they stay collided, each year the mountains grow.
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In an continental-oceanic crust, a convergent boundary creates a volcano. When the plates collide, the oceanic crust goes under the continental crust. This causes magma to rise to the continental crust. This process is called subduction. AAAAAAAAHHHHHHH. The volcano is about to erupt lets go.
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Such a peaceful island. We should store some of our children in here. Now let's get back to the topic. In a oceanic-oceanic crust, the convergent boundary forms volcanic island arcs. This is also created by the rise of magma, but not subduction.
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Well that's it, but now I'm hungry, and I need to fix you up because you are malfunctioning. Lucky for you, there is 1 thing that can fix us robots and we have it. Time to go get some dinner.
DELICIOUS
DINNER'S READY
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