Planet formation is a fascinating process that takes place within a protoplanetary disk. This disk consists of gas and dust surrounding a newborn star. Over time, these particles collide and stick together to form larger bodies, known as planetesimals.
These planetesimals, through further collisions and gravitational interactions, grow into protoplanets. As they continue to accumulate mass, they can eventually become full-fledged planets.
The process of planet formation can be divided into a few main stages:
- Dust grain accumulation: Small dust particles and ice grains stick together due to static and chemical forces.
- Formation of planetesimals: Collisions and coagulation of dust grains form kilometer-sized bodies.
- Growth into protoplanets: Planetesimals collide and merge, growing larger through accretion.
- Planetary differentiation: Protoplanets differentiate into core, mantle, and crust due to internal heating and melting.
Understanding planet formation helps us learn about the origins of our own solar system and other planetary systems in the universe.