Tideglass Studio
The eight stages

Stage 5 of 8

Protoplanet

Gains: Molten Core

Impacts melt you through. Forge a core and swallow bigger worlds.

Impacts and buried heat melt you through, and your metal sinks to make a core.

A glowing partly molten protoplanet struck by infalling debris.

Heat from a thousand impacts

Growing this fast is violent. Every body you swallowed struck with the energy of its fall, and that energy stayed as heat. Add the warmth of radioactive elements decaying deep inside, and you crossed a threshold: you began to melt. You are a protoplanet now, glowing softly in the dark.

Cutaway of a differentiating protoplanet with iron sinking to the core.

Iron finds the center

Molten, you sorted yourself out. Heavy iron and nickel sank toward your middle while lighter rock floated up. This is differentiation, and it gave you a dense metal core, a rocky mantle, and, in time, a magnetic field. You stopped being a pile of rubble and became a world with an inside.

True things

  • Differentiation is why Earth has an iron core, a rocky mantle, and a thin crust.
  • The decay of radioactive aluminum-26 was a major heat source for the first protoplanets.
  • A spinning molten metal core is what gives a world a protective magnetic field.