0
About 2700 kilometers
Still curious? Ask our experts.
Chat with our AI personalities
Professor
Devin
BeauThe 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.
- The oceanic crust is 5 km (3 mi) to 10 km (6 mi) thick.
- The continental crust is typically from 30 km (20 mi) to 50 km (30 mi) thick.
For the source and more detailed information concerning your request, click on the related links section (Wikipedia) indicated directly below this answer section.
- The oceanic crust is 5 km (3 mi) to 10 km (6 mi) thick.
- The continental crust is typically from 30 km (20 mi) to 50 km (30 mi) thick.
For the source and more detailed information concerning your request, click on the related links section (Wikipedia) indicated directly below this answer section.
- The oceanic crust is 5 km (3 mi) to 10 km (6 mi) thick.
- The continental crust is typically from 30 km (20 mi) to 50 km (30 mi) thick.
For the source and more detailed information concerning your request, click on the related links section (Wikipedia) indicated directly below this answer section.
- The oceanic crust is 5 km (3 mi) to 10 km (6 mi) thick.
- The continental crust is typically from 30 km (20 mi) to 50 km (30 mi) thick.
For the source and more detailed information concerning your request, click on the related links section (Wikipedia) indicated directly below this answer section.
- The oceanic crust is 5 km (3 mi) to 10 km (6 mi) thick.
- The continental crust is typically from 30 km (20 mi) to 50 km (30 mi) thick.
For the source and more detailed information concerning your request, click on the related links section (Wikipedia) indicated directly below this answer section.
- The oceanic crust is 5 km (3 mi) to 10 km (6 mi) thick.
- The continental crust is typically from 30 km (20 mi) to 50 km (30 mi) thick.
For the source and more detailed information concerning your request, click on the related links section (Wikipedia) indicated directly below this answer section.
- The oceanic crust is 5 km (3 mi) to 10 km (6 mi) thick.
- The continental crust is typically from 30 km (20 mi) to 50 km (30 mi) thick.
For the source and more detailed information concerning your request, click on the related links section (Wikipedia) indicated directly below this answer section.
Add your answer:
Earn +20 pts
What is the thickness of the earths crust in miles?
The Earth's crust varies in thickness, ranging from around 3 to 25 miles thick. However, on average, the Earth's crust is about 18-25 miles thick below continents and around 3-6 miles thick below the oceans.
The relative thickness of the Earths crust is similar to the relative thickness of the?
The relative thickness of the Earth's crust is similar to the relative thickness of an apple's skin compared to the apple itself. Both the Earth's crust and an apple's skin are thin outer layers in relation to the entire object.
What is the thickness of an earth layer?
The thickness of Earth's layers vary depending on the specific layer. For example, the Earth's crust can range from 5-70 km thick, the mantle is about 2,900 km thick, and the outer core is approximately 2,200 km thick. The inner core has a radius of about 1,220 km.
How wide is the crust?
The Earth's crust can vary in thickness, but on average it is about 5-70 kilometers (3-44 miles) thick. However, it can be much thicker under mountain ranges and thinner under the ocean floor.
The earths crust varies from 8km to 40 km what does this show?
This variation in the thickness of Earth's crust demonstrates that it is not uniform and can vary significantly depending on location. It indicates the diverse geological processes that have occurred over time, such as the formation of mountain ranges or ocean basins, leading to this variability in crust thickness. Additionally, it highlights the dynamic nature of Earth's lithosphere.
