Continental is made mostly of granite. Oceanic is made mostly of basalt and gabbro.
The continental crust is thicker and less dense than oceanic crust. Oceanic crust is younger and primarily composed of basalt, while continental crust is older and made up of a variety of rock types, including granite and sedimentary rocks.
The oceanic crust is made out of basalts - (lava-hardened Iron/Magnesium Silicate mixtures which solidified rapidly).
The thinner but more dense crust of the Earth is found beneath ocean basins and is known as oceanic crust. It is made up of dense basalt rock and is thinner than the continental crust. This crust is constantly being formed and destroyed through the process of seafloor spreading and subduction, respectively.
The two types of crust are continental crust and oceanic crust. Continental crust is thicker and less dense, composed mainly of granite and sedimentary rocks. Oceanic crust is thinner and more dense, made up of basalt and gabbro rocks.
The oceanic crust is primarily made of solid rock, primarily basalt. However, beneath the oceanic crust, there is a layer of partially molten rock called the mantle that flows slowly over time.
Oceanic crust is primarily made up of basaltic rock, which is dense and rich in iron and magnesium. Continental crust is composed mainly of granite and other lighter silicate rocks, which are less dense than basalt.
The oceanic crust is mostly made up of basalt, which is a dense volcanic rock that forms from the cooling of lava at the Earth's surface.
The layer of the crust that is made of granite is called the continental crust. It is thicker and less dense compared to the oceanic crust, which is made of basalt. The continental crust is primarily composed of granite and covers the Earth's continents.
The continental crust is thicker and less dense than oceanic crust. Oceanic crust is younger and primarily composed of basalt, while continental crust is older and made up of a variety of rock types, including granite and sedimentary rocks.
The layer of the Earth mostly made out of granite and similar rocks is the continental crust. This outermost layer varies in thickness and is primarily composed of lighter, less dense materials compared to the underlying mantle. The continental crust contrasts with the oceanic crust, which is primarily made up of basalt.
Granite is very much less dense than basalt. This is why the continental crust (mostly composed of granite) floats on Oceanic crust (made mostly of basalt). Granite is 70 % silicon. Where basalt is mainly pyroxene.
The main type of rock in oceanic crust is basalt. Basalt is a fine-grained igneous rock formed from the rapid cooling of lava at or near the Earth's surface. It is dark in color and rich in minerals like pyroxene and plagioclase feldspar.
Continental crust is on top of the oceanic crust Continental crust is made of granite whereas oceanic crust is made of basalt Continental crust is partly above sea level and partly below whereas oceanic crust is always below sea level.
The oceanic crust is made out of basalts - (lava-hardened Iron/Magnesium Silicate mixtures which solidified rapidly).
The two types of crustal material are continental crust and oceanic crust. Continental crust is thicker and less dense, composed mainly of granite rocks, while oceanic crust is thinner and denser, made up primarily of basalt rocks.
The top layer of the Earth's crust is made up of solid rock called the lithosphere. It includes both continental crust, which is thicker and less dense, and oceanic crust, which is thinner and more dense.
Oceanic and Continental crusts are alike because they both shift and move and grow. They differ by there rock types. Oceanic crust is made up of dense basalt while continental crust is made up of less dense granite.