Earth Layers Explorer
Take a journey from the surface to the center of our planet.
1. Exploration Depth
2. Physical State
SOLID ROCK
The Crust
The thin, outer shell of the Earth where we live.
~35 km
Avg. Thickness
20 - 400 °C
Temp Range
Granite & Basalt
Primary Composition
Earth's Compositional Layers
Earth is organized into distinct layers, sorted primarily by density during the planet's formation over 4 billion years ago.
- The Crust: Composed of tectonic plates. Oceanic crust is dense and thin (basalt), while continental crust is thicker and lighter (granite).
- The Mantle: The thickest layer. Though hot and under immense pressure, it consists of solid, "plastic" rock that flows very slowly over millions of years.
- The Outer Core: A churning sea of liquid iron and nickel. Its convection currents generate Earth's vital magnetic field.
- The Inner Core: The intense pressure at the center of the Earth keeps this iron-nickel alloy in a solid state, despite temperatures hotter than the surface of the sun.