The Earth's crust is primarily composed of low-density silicate minerals, with a significant portion made up of feldspar, quartz, mica, and amphibole. These minerals are rich in silicon and oxygen, forming the foundation of continental and oceanic crust. The average composition of the crust is about 45% silicate minerals, which contribute to its relatively low density compared to the underlying mantle.
crust
There are almost no extrusive rocks on the earths surface because they are all under the earths surface. They are mainly lower than the earths surface.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
The earth's crust is not stress
continental crust
crust
There are almost no extrusive rocks on the earths surface because they are all under the earths surface. They are mainly lower than the earths surface.
There are several layers between the outer core and the crust mainly combined into one and called the Mantle.
The Earths crust is approximately 650 km deep.
The two types of Earth's crust are continental crust and oceanic crust. Continental crust is thicker, less dense, and composed mainly of granite, while oceanic crust is thinner, denser, and made up mostly of basalt.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
mantle
The earth's crust is not stress
The Earths Crust can be divided between Oceanic Crust and Continental Crust. Oceanic and Continental Crust are quiet different. The thickness of oceanic crust is between 5km and 10km. It is made of mainly basalt, grabbo and diabise. The thickness of continental crust is between 30km and 50km. It is made up of lighter rocks such as granite.
half of earths layer
continental crust
crust