continental crust
The Earth's crust varies in thickness, with an average thickness of about 35 km beneath continents and 7 km beneath oceans. However, in some places, like mountain ranges, the crust can be up to 70 km thick.
40 to 70 km thick
The crust is 19 miles/33km thickThe upper mantle is 415 miles/667km thickThe lower mantle is 1365 miles/2200km thickThe outer core is 1405 miles/2265km thickThe inner core is 760 miles/1220km thick (diameter of 2440 km)
The Earth's layers vary in thickness. The crust is thinnest under the oceans, around 5-10 km thick, and thicker under continents, around 20-70 km thick. The mantle extends from the crust to about 2,900 km below the surface, while the outer core is about 2,300 km thick and the inner core is about 1,200 km thick.
The asthenosphere is approximately 250 km to 400 km thick beneath the Earth's crust. However, its exact thickness can vary in different regions and can reach up to 700 km in some areas.
The continental crust, (where all the land is) is generally around 30 km (20 mi) to 50 km (30 mi) thick. The oceanic crust (the bottom of the sea) is roughly 5 km (3 mi) to 10 km (6 mi) thick.
the oceanic crust is thinner, generally5-8 killometers thick, and is made of basalt, but the continental crust is an average of 30 km and is made of granite
The Earth's crust varies in thickness, with an average thickness of about 35 km beneath continents and 7 km beneath oceans. However, in some places, like mountain ranges, the crust can be up to 70 km thick.
crust: average of 32 km thick mantle: 2900 km thick outer core: 2200 km thick inner core 1250 km thick
A batholith is a pluton exposed across more than 100 square km of Earth's surface. An average batholith is about 10 km thick, but can be up to 20 km thick. A stock is very similar to a batholith, but with less than 100 square km exposed.
The continental crust is about 25 to 70 kilometers thick. The average is about 50 kilometers.
A batholith is a pluton exposed across more than 100 square km of Earth's surface. An average batholith is about 10 km thick, but can be up to 20 km thick. A stock is very similar to a batholith, but with less than 100 square km exposed.
The thickness of Earth's layers varies: the crust is between 5-70 km thick, the mantle is about 2,900 km thick, the outer core is about 2,300 km thick, and the inner core is about 1,200 km thick.
Inner core: 2450 km thick Outer core: 2300 km thick Lower mantle: 2500 km thick Upper Mantle: 400 km thick continental crust: 30-70 km thick Oceanic Crust: 6 km thick
There are two types of crust's. I dont know which one you are talking about, but it is probably the continental crust. The other type of crust is the Oceanic crust. The first continental crust is about 4-7 miles (6-11 km) thick and mainly consists of heavy rocks, like basalt. The Continental crust is thicker than the Oceanic crust, about 19 miles(30 km) thick. It is mainly made up of light material like granite.
40 to 70 km thick
Its 10 km thick.