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What the Earth appears to look like when viewed from outer space
A ball
Main layers of the Earth
Crust, mantle, core
The point where beyond direct observation of Earth’s interior is impossible
10 km deep
Outermost layer of Earth composed of continents and ocean basins
Crust
Thicker than the oceans
continental crust
Thinner than the continents
ocean crust
Continental crust thickness
35-70 km thick
Ocean crust thickness
5-10 km thick
Ocean crust
compact and composed of basalt
Continental crust
mainly composed of granite rock
Oxygen
Most abundant element in the crust
Crust
less than 2% of Earth’s radius
Mantle
about 2900 km thick, divided into upper and lower portions.
ferro-magnesium silicates
what the mantle is mainly composed of
plastic zone
allegedly where lava originates
Core
about 3500 km thick, divided into inner and outer layers; hottest part of the earth
Outer core
liquid iron and nickel, around 2300 km thick
Inner core
solid iron and nickel due to pressure, about 1200
6,000 - 10,000 degrees Celsius
Temperature in the core
Continental drift theory, tectonic plate theory
Two main theories on crustal movement
200 million years ago
Allegedly when continents broke into smaller forms
Alfred Wegener
A German geophysicist and meteorologist who proposed the continental drift theory in 1912