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Fill In: Convergent Boundary

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Fill in the blank on convergent boundaries

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Edad recomendada: 13 años
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Benjamin D Morgan
Benjamin D Morgan
Estados Unidos

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Fill In: Convergent Boundary

Fill in the blank on convergent boundaries

Benjamin D Morgan
1

DIVERGENTBOUNDARY low oceanic subducts stuck mountains tall volcanoes currents both foldup three melts continental trench more hot less folddown valleys islands CONVERGENTBOUNDARY convection

Where two plates collide this is called a . When two plates move apart it is a . Three are types of convergent boundaries .

One kind of convergent boundary is when a continental plates collides with an oceanic plate . When this occurs the dense plate is the oceanic plate . This is because it is made out of basalt . The continental plate is dense because it is made out of mostly granite . The oceanic plate or sinks into the mantle because it is this density difference . This sinking causes a spot to form in the water where the two plates meet . This low spot is called a . The continental plate does not subduct . Instead , it gets . But , the currents underneath the plate continues to push it so it folds up and down creating where it folds up and where it folds down . Finally , the subducted plate as it heats up in the mantle and moves closer to the core . The melted crust becomes and less dense , rises upward , and goes through the continent above . This creates on the continent .

There is another boundary that subduction like this also occurs . This is when two plates converge . The only difference is that the volcanoes form underwater volcanoes and volcanic . Also , the stuck plate creates underwater mountains and trenches instead of valleys . In addition , some of the mountains can become islands if they are enough to go through the surface of the ocean .

When two plates collide no plate subducts or sinks . This is because plates have a low density . As a result , both plates get stuck at the boundary . The two plates continue to get pushed together by the convection so they both fold . This creates mountains where they and valleys where the plates . Because there is no subduction there are novolcanoes .

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