The color of the continental crust varies, but it is typically light in color, ranging from shades of gray to brown or reddish. This coloration is primarily due to the mineral composition of the rocks that make up the continental crust, such as quartz, feldspar, and mica. The presence of these minerals gives the continental crust its characteristic light color compared to the darker oceanic crust.
Continental crust is mainly composed of granitic rocks such as granite and rhyolite, which are light in color and less dense. Oceanic crust is primarily composed of basaltic rocks, specifically basalt, which are dark in color and more dense than granitic rocks.
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
Oceanic crust is denser than continental crust, so when they collide, the oceanic crust will subduct beneath the continental crust. This subduction process can lead to the formation of volcanic arcs and mountain ranges.
Red
Light colored
Continental crust is generally lighter in color than oceanic crust. This is because continental crust is composed of lighter-colored rocks such as granite, which contain lighter minerals like quartz and feldspar. In contrast, oceanic crust is made up of darker-colored rocks like basalt, which contain heavier minerals like pyroxene and olivine.
Oceanic crust is darker than continental crust because it is often composed of dense basalt, which contains minerals like pyroxene and olivine that give it a dark color. In contrast, continental crust is typically made of lighter-colored rocks, such as granite, that have different mineral compositions. The mineral content and composition of the crust can influence its overall color.
Continental crust is the thicker of the two: it extends far beneath and above the Oceanic crust.
Continental crust is mainly composed of granitic rocks such as granite and rhyolite, which are light in color and less dense. Oceanic crust is primarily composed of basaltic rocks, specifically basalt, which are dark in color and more dense than granitic rocks.
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.