Image via USGS. At the bottom of the oceans and some seas, there is oceanic crust. Oceanic crust is very thin (usually under 10 km), and is composed of dense, typically dark (mafic) rocks: basalt, gabbro, diabase. The continental crust is thicker than that – usually it's around 40 km deep, but can go up to 70
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Answer:
Image via USGS. At the bottom of the oceans and some seas, there is oceanic crust. Oceanic crust is very thin (usually under 10 km), and is composed of dense, typically dark (mafic) rocks: basalt, gabbro, diabase. The continental crust is thicker than that – usually it's around 40 km deep, but can go up to 70
Explanation:
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