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The oceanic plate is more dense than the continental plate, and will subduct, or move underneath, the lighter continental plate. The result is that the continental plate is uplifted. As the oceanic crust goes deeper and deeper, the temperatures become higher, causing the subducting crust to eventually melt into the mantel. The heat and gas pressure from the melting of the subducting crust may eventually seek release in the form of a volcano. The rate of crustal movement is slow, measured in a small number of inches per year, but the volcanism and crustal uplifting and folding eventually create mountains.

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Q: How are mountains formed when a plated with an oceanic crust meets one with a cnotinental crust?
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Convergent boundaries can be divided into 3 categories what are these categories and what geological feature are created by each?

The categories are a continental and a continental plate colliding, continental and oceanic plates colliding, and oceanic and oceanic plates colliding. The two continental plates form mountains. The continental and oceanic plated colliding cause subduction zones and volcanoes. Oceanic and oceanic plates colliding form a trench.


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Indonesia has many volcanoes, not just one. Indonesia has volcanoes because it is located along a subduction zone, where a slab of oceanic crust is sinking under another plated and into the mantle. Water that the plate takes with it alters the chemistry of the mantle rock, causing some of it to melt and rise through the crust.


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I believe it's not height but how it was formed. Take for example Mt. Everest and the surrounding mountains. This mountain is created as the two continental plated push up against each other. This cause the Earth that meets between these two plates to push up.


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