Planet formation takes place within the protoplanetary disk. This process begins with small dust particles sticking together through electrostatic forces.
As they grow in size, gravity helps clump more materials together, forming planetesimals and eventually protoplanets.
There are two main methods of planet formation:
- Core Accretion: This is the dominant theory for forming terrestrial planets like Earth. It involves the gradual buildup of solid materials.
- Disk Instability: This method may form gas giants quickly by the disk's gas forming dense clumps, collapsing under its gravity.
Understanding planet formation gives insights into the diversity of planetary systems observed throughout the galaxy.