GEOL201 - Earth History
In astronomy, a giant (or supergiant) is a star that has finished core hydrogen fusion and left the main sequence on the Hertzsprung–Russell (H–R) diagram. Compared to its main-sequence years, such a star is much larger in radius, often cooler and redder at the surface, but can be far more luminous overall because it radiates from an enormous surface area.
The interior reorganizes: the core contracts and heats while outer layers expand and cool. The star may burn fuel in shells outside the core, and more massive stars can ignite heavier elements in the core over time. The giant phase is when the star is changing how it produces energy and moving toward its final outcome (white dwarf, neutron star, black hole, or shedding mass into space), depending on mass.
Earth History courses often begin with the formation of the solar system from a nebula and the assembly of a layered planet. Our Sun will eventually pass through giant stages (billions of years from now). Understanding what “giant” means sets up later ideas about where the chemical ingredients of planets came from, not only from the primordial nebula, but from earlier generations of stars.