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12 600 13 000 kg m 3.
Diagram of the earth s core. 5 000 c 6 000 c state. The metal at the inner core stays solid because of the incredible. Made mainly of iron the temperature of the ball is 5 000 c to 6 000 c that s up to 6 000 times hotter than our atmosphere and scorching enough to make metal melt.
In figure 1 we can see the different layers of the earth including the core mantle and lithosphere. It is the center and the hottest part of the earth. It is the thin relatively outermost layer that wraps around the earth and ranges in.
The layers of earth diagram. Earth s core is the very hot very dense center of our planet the ball shaped core lies beneath the cool brittle crust and the mostly solid mantle the core is found about 2 900 kilometers 1 802 miles below earth s surface and has a radius of about 3 485 kilometers 2 165 miles. Within the diagram there are two representations of the layers.
At the heart of our planet lies a solid iron ball about as hot as the surface of the sun. Trevor nace layers of earth 1. The problem is hard to attack because seismic waves have to go pretty much straight from an earthquake right through the earth s center to a seismograph.
Similar to the outer core the inner core is composed primarily of iron and nickel and has the highest density among all other layers. A cut away illustration of earth s interior. Earth s inner core is the innermost geologic layer of the planet earth it is primarily a solid ball with a radius of about 1 220 km 760 mi which is about 20 of earth s radius or 70 of the moon s radius.
The earth s inner core is a huge metal ball 2 500km wide. It is really quite fascinating. Seismologists continue to probe the inner core.
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This Is A Diagram Showing The Layers Of The Earth S Center Outer Core Inner Core Earth
