π Layers of the Earth
Scientists divide Earth into four main layers:
1. Crust
-
The outermost layer.
-
It’s thin compared to other layers (like the skin of an apple π).
-
Made of solid rock.
-
This is where we live, and it includes continents and ocean floors.
2. Mantle
-
The layer beneath the crust.
-
Much thicker than the crust.
-
Made of hot, semi-solid rock that can slowly flow.
-
Movement in the mantle causes earthquakes, volcanoes, and plate movement.
3. Outer Core
-
Beneath the mantle.
-
Made of liquid iron and nickel.
-
The movement of this liquid metal creates Earth’s magnetic field π§.
4. Inner Core
-
The center of the Earth.
-
Made of solid iron and nickel.
-
Extremely hot (hotter than the surface of the sun ☀️), but stays solid because of the high pressure.
✨ Quick Summary:
-
Crust → Thin, solid rock, where we live.
-
Mantle → Thick, hot, semi-solid rock, causes movement.
-
Outer Core → Liquid metal, makes magnetic field.
-
Inner Core → Solid metal, hottest part.
No comments:
Post a Comment