Oceanic crust is denser than continental crust. This is primarily due to its composition; oceanic crust is mainly made of basalt, which is a denser volcanic rock, while continental crust is primarily composed of lighter granitic rocks. As a result, oceanic crust typically has a density of about 3.0 g/cm³, whereas continental crust averages around 2.7 g/cm³. This difference in density is a key factor in the behavior of tectonic plates and their interactions.
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