Raman spectroscopy is a convenient, efficient, and non‐destructive technique that could estimate the metamictization degree of zircon, particularly for gem‐class or historical samples. The full width at half maximum value of the ν3(SiO4) band around 1000 cm−1 can classify the structural state of zircon as crystallized (the full width at half maximum value is less than 5 cm−1), intermediate (the full width at half maximum value ranges from 5 to 15 cm−1), and metamict (the full width at half maximum value is more than 15 cm−1). This study focuses on the zircon samples from Sri Lanka in the gemological collection of Abraham Gottlob Werner. These samples show red to green, according to the Munsell color system and the CIEL*C*h* color system, and their density is from 4.07 to 4.87 g/cm3. Comparing the color and metamictization degree data of zircon samples, crystallized zircon displays a more red tone with yellow. The green tone in zircon occurs with metamictization. The density of zircon could be an indicator of the metamictization degree as crystallized zircon is 4.57 to 4.70 g/cm3 in a 95% confidence interval, which matches the theoretical density (4.61–4.76 g/cm3) better, whereas metamict zircons present a density of 4.37–4.59 g/cm3, and the density of zircon decreases with metamictization. The metamictization has a significant influence on the gemological properties of zircon, whereas the typical color tone and low density can be a sign of the metamictization.