Red
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.
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 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 the thicker of the two: it extends far beneath and above the 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!
Continental crust is far older than oceanic crust.
younger
The continental crust is made up of igneous, sedimentary, and metamorphic rocks. These rocks form the continents and the continental shelves, areas of seabed close to the shore.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.