5 km thick
Continental crust.
Continental crust is less dense than oceanic crust, so it floats higher on the mantle. This means that the same thickness of continental crust will displace less mantle compared to oceanic crust. Additionally, continental crust is composed of lighter rocks like granites, while oceanic crust is made of denser rocks like basalt.
The Earth's crust ranges in thickness from five to 25 miles. It is the outermost layer of the Earth and is divided into two types: continental crust and oceanic crust. Continental crust is thicker than oceanic crust.
The two main differences between continental and oceanic crust are their composition and thickness. Continental crust is primarily made up of granitic rocks, which are less dense than the basaltic rocks that make up oceanic crust. Additionally, continental crust is much thicker, averaging around 35 km thick, compared to oceanic crust, which is typically around 7 km thick. These differences in composition and thickness contribute to the contrasting properties and behaviors of continental and oceanic crust in geological processes.
The Earth's crust is most similar in thickness to that of the atmosphere. The Earth's crust varies in thickness from oceanic crust (around 5-10 km) to continental crust (around 20-70 km), which is comparable to the thickness of the atmosphere (around 100 km).
Continental crust.
The oceanic crust.
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.
CONTINENTAL CRUST is 35km of thickness and oceanic is 7 km. i hope that helped
7-10 km
CONTINENTAL CRUST is 35km of thickness and oceanic is 7 km. i hope that helped
Continental crust is less dense than oceanic crust, so it floats higher on the mantle. This means that the same thickness of continental crust will displace less mantle compared to oceanic crust. Additionally, continental crust is composed of lighter rocks like granites, while oceanic crust is made of denser rocks like basalt.
The Earth's crust ranges in thickness from five to 25 miles. It is the outermost layer of the Earth and is divided into two types: continental crust and oceanic crust. Continental crust is thicker than oceanic crust.
In technical terms, the oceanic crust is denser than the continental crust so when the continental crust and the oceanic crust meet the continental crust will sink under and the oceanic crust will slide over and a volcano will be formed as well as producing earthquakes in the process.
The two main differences between continental and oceanic crust are their composition and thickness. Continental crust is primarily made up of granitic rocks, which are less dense than the basaltic rocks that make up oceanic crust. Additionally, continental crust is much thicker, averaging around 35 km thick, compared to oceanic crust, which is typically around 7 km thick. These differences in composition and thickness contribute to the contrasting properties and behaviors of continental and oceanic crust in geological processes.
Where oceanic crust meets continental crust and earthquakes can occur.
The Earth's crust is most similar in thickness to that of the atmosphere. The Earth's crust varies in thickness from oceanic crust (around 5-10 km) to continental crust (around 20-70 km), which is comparable to the thickness of the atmosphere (around 100 km).