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The rock of the continental crust is mostly granitic in composition, meaning it is a high silicate intrusive igneous rock.

The rock of the oceanic crust is basaltic in origin, meaning it is lower in silica and higher in heavier elements like iron and magnesium and is classified as a mafic igneous rock.

Oceanic crust is therefore more dense than continental crust.

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Q: How does the rock under the continents differ from rock under the oceans?
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