The continental crust is in the solid phase of matter. It is composed primarily of rocks and minerals, which are solid materials that form the Earth's outer layer. This crust is characterized by its varied composition and thickness, but it remains solid under normal conditions encountered on Earth's surface.
Continental crust is solid.
The crust is the outermost layer of the Earth's surface. It is solid rock and can be classified into two types: continental crust, which is thicker and less dense, and oceanic crust, which is thinner and more dense.
1. The Oceanic crust is dense while the Continental crust is relatively lighter. 2. The Oceanic crust consists of Silicon and Magnessium, while the Continental crust has Silicon and Alluminium. 3. The Oceanic crust is thin, while the Continental crust is thick. 4. The Oceanic crust makes up the ocean floor, while the Continental crust carries the continents.
Continental crust is far older than oceanic crust.
continental slope
Continental crust exists in a solid state..
Continental crust is solid.
the state of matter for the earth's crust is continental and oceanic.
The crust is the outermost layer of the Earth's surface. It is solid rock and can be classified into two types: continental crust, which is thicker and less dense, and oceanic crust, which is thinner and more dense.
Continental crust is the thicker of the two: it extends far beneath and above the Oceanic crust.
Continental crust is far older than oceanic crust.
It is not. The oceanic crust is thinner than the continental crust!
It is not. The oceanic crust is thinner than the continental crust!
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.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
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.