The crust consists of two parts: the oceanic and the continental crust.
All of these values vary slightly, of course, but oceanic crust is generally 4 - 7 miles (6 - 11 km) thick, whereas continental crust is much thicker, averaging 20 - 25 miles (30 - 40 km), reaching a maximum of 45 miles (70 km) beneath large mountain ranges (having to do with tectonics and isostacy, the "roots" of a mountain range).
The inner core is 1216 km and made of solid iron. It is approx 5000 degrees C and it doesnt melt because of everything else pushing down on it.
Earth's Atmosphere is 10km thin,and yet warm enough to keep EVERY living thing on Earth warm enough to survive or live
It is 10 mm thick.
wax paper is about 5cm thick
What are two ways that's scientists can study earths climates history
8 to 65 km thick
Once magma breaks through the earths crust it is called"lava"
a rift is a long deep valleys formed by movement of earths curst
The Earths crust is approximately 650 km deep.
These are called earthquakes, they are caused by two huge rock plates in the earth which crash into each other.
one and a half miles thick
asthenosphere
the convection currents in the mantle under the earths curst is moving the broken plates in earths lithosphere causing the plates slide across the lithosphere. this process is called tectonics. (jon lay wrote this,)
about 20 inches
I say thick because it's got many layers.
The part that is dry land is about 25 miles thick.
mantle is the thick layer before you reach the core of the earth