The discussion centers on how gamma rays generated from hydrogen fusion in the Sun's core are transformed into the full spectrum of photons observed from Earth. It is clarified that gamma rays do not directly contribute to the visible spectrum; instead, they are absorbed and re-emitted as lower-energy photons through various processes as they travel to the surface. The photosphere, with a temperature of about 5800 K, emits the majority of visible light, while the chromosphere, which has a complex temperature profile, can produce both absorption and emission lines. The transformation of energy occurs through mechanisms such as Thomson scattering and bremsstrahlung, which are influenced by the temperature and density of different solar layers. Understanding the thermal processes involved allows for the prediction of a black-body spectrum without needing to know the specific details of the interactions.