![]() This +4 iron absorbs those wavelengths (357 and 545 nanometres) of light producing the colour of the amethyst. Gamma ray radiation (from radioactive decay in the underlying rocks) is capable of shaking the electron out of the iron lattice and depositing the electron in the interstitial carbon. Some of this iron is present in sites normally occupied by silicon, and some are interstitial (in sites where the atom is not normally present). Quartz will commonly contain trace amounts of iron (from 10 to 100 parts per million pieces of iron). Compared to this, lead was used, followed by the use of selenium. Manganese was used as a clearing ingredient in glass from 1860 to 1915. The purple color of ghost town glass comes from small amounts of manganese in the glass when exposed to ultraviolet light. They are produced when small amounts of iron are irradiated (from the normal radiation in the rocks). The color of the amethyst comes from the quartz color centers. These pale colors were once considered undesirable but have recently become popular as a result of intensive marketing. ‘Rose de France’ has a distinctly light shade of purple, reminiscent of a lavender / lila shade. The perfect classification is called “Ultra Siberian” which has a predominant purple hue of around 75–80 per cent, with 15–20 per cent blue which (depending on the light source) red secondary hues. ![]() High-quality amethyst can be found in Russia, Sri Lanka, Peru, Uruguay and the Far East. Amethyst may have one or both secondary shades, red and blue. The hardness of the stone is the same as quartz, making it ideal for use in jewelry.Īmethyst occurs in primary shades from a light pinkish purple color to a deep purple color. ![]() Image by Rudy and Peter Skitterians from PixabayĪmethyst is a purple quartz type (SiO2) and owes its violet color to irradiation, iron impurities and, in some cases, other transition metals, and the presence of other trace elements resulting in complex crystal lattice substitutions. ![]()
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