Continental crust is thicker than oceanic crust. Continental crust can be up to 70 kilometers thick, while oceanic crust is typically around 7 kilometers thick.
younger
The boundary between the oceanic crust and continental crust is known as the continental shelf. This is the shallowest part of the ocean that extends from the shore to the continental slope.
The continental margin typically consists of a combination of continental crust that extends from the shoreline to the continental shelf's outer edge, where it transitions into oceanic crust of the ocean basin.
Continental crust is generally thicker than oceanic crust. Continental crust can be up to 70 km thick, while oceanic crust is usually around 5-10 km thick.
Continental crust is thicker than oceanic crust. Continental crust can be up to 70 kilometers thick, while oceanic crust is typically around 7 kilometers thick.
It is not. The oceanic crust is thinner than the continental crust!
It is not. The oceanic crust is thinner than the continental crust!
Continental crust is far older than oceanic crust.
younger
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
The boundary between the oceanic crust and continental crust is known as the continental shelf. This is the shallowest part of the ocean that extends from the shore to the continental slope.
The continental margin typically consists of a combination of continental crust that extends from the shoreline to the continental shelf's outer edge, where it transitions into oceanic crust of the ocean basin.
Continental crust is generally thicker than oceanic crust. Continental crust can be up to 70 km thick, while oceanic crust is usually around 5-10 km thick.
The continental crust is land, it is perfectly solid.
Oceanic and Continental crust. Oceanic crust is made of basalt. Continental crust is made of granite
Oceanic crust is thinner and denser than continental crust. Oceanic crust is primarily made of basalt, while continental crust is composed of granitic rocks. Continental crust is older and more complex in structure compared to oceanic crust. Oceanic crust is constantly being created at mid-ocean ridges and destroyed at subduction zones, while continental crust is more stable and less prone to being recycled.