granite
Oceanic crust is mainly made up of the mineral basalt, while continental crust is primarily composed of the mineral granite. Both types of crust are rich in other minerals as well, but these are the predominant ones in each.
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.
Granite is the rock that makes up most of the continental crust. It is a coarse-grained igneous rock that is formed through the slow cooling of magma beneath the Earth's surface. Granite is composed mainly of quartz, feldspar, and mica minerals.
The mineral silicate that makes up about half of Earth's crust and is a main component of most rocks is known as feldspar. It is a group of rock-forming minerals that are abundant in the Earth's crust and have a wide range of chemical compositions and colors.
The lithosphere can have two main types of crust: continental crust and oceanic crust. Continental crust is thicker, older, and less dense than oceanic crust. Oceanic crust is thinner, younger, and denser, primarily composed of basaltic rocks.
Oceanic crust is mainly made up of the mineral basalt, while continental crust is primarily composed of the mineral granite. Both types of crust are rich in other minerals as well, but these are the predominant ones in each.
The main mineral that makes up the Earth's crust is called feldspar. Feldspar is a group of rock-forming minerals that make up about 60% of the Earth's crust by weight.
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.
Granite is the rock that makes up most of the continental crust. It is a coarse-grained igneous rock that is formed through the slow cooling of magma beneath the Earth's surface. Granite is composed mainly of quartz, feldspar, and mica minerals.
The mineral silicate that makes up about half of Earth's crust and is a main component of most rocks is known as feldspar. It is a group of rock-forming minerals that are abundant in the Earth's crust and have a wide range of chemical compositions and colors.
Continental crust is made primarily of granite.
The lithosphere can have two main types of crust: continental crust and oceanic crust. Continental crust is thicker, older, and less dense than oceanic crust. Oceanic crust is thinner, younger, and denser, primarily composed of basaltic rocks.
Basalt is the main rock of which the oceanic crust is composed of. Continental crust is mainly granitic.
Continental drift or gravity pulling
The two main types of crust are oceanic crust, which is denser and thinner, primarily composed of basaltic rock, and continental crust, which is less dense and thicker, mainly made up of granitic rock.
manganese
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.