When partially heated, amethyst can result in ametrine.Īmethyst can fade in tone if overexposed to light sources, and can be artificially darkened with adequate irradiation. Natural amethyst is dichroic in reddish violet and bluish violet, but when heated, turns yellow-orange, yellow-brown, or dark brownish and may resemble citrine, īut loses its dichroism, unlike genuine citrine. In the presence of trace elements of large ionic radius, and to a certain extent, the amethyst color can naturally result from displacement of transition elements even if the iron concentration is low. The color of amethyst has been demonstrated to result from substitution by irradiation of trivalent iron (Fe 3+) for silicon in the structure, The uncut gem may have only a small portion that is suitable for faceting. Sometimes, only a thin layer of a natural, uncut amethyst is violet colored, or the color is very uneven. One of gem cutters' tasks is to make a finished product with even color. Other names for green quartz are vermarine and lime citrine.Īmethyst frequently shows color zoning, with the most intense color typically found at the crystal terminations. Green quartz is sometimes called green amethyst the scientific name is prasiolite. These pale colors were once considered undesirable, but have recently become popular due to intensive marketing. 'Rose de France' is defined by its markedly light shade of the purple, reminiscent of a lavender / lilac shade. The ideal grade, called 'Deep Siberian', has a primary purple hue of around 75–80%, with 15–20% blue and (depending on the light source) red secondary hues. High-quality amethyst can be found in Siberia, Sri Lanka, Brazil, Uruguay, and the Far East. Amethyst may exhibit one or both secondary hues, red and blue.

The hardness of the mineral is the same as quartz, thus making it suitable for use in jewelry.Īmethyst occurs in primary hues from a light lavender or pale violet to a deep purple.

This structure is quite rigid and results in quartz's hardness and resistance to weathering. Ions that replace Si in the lattice to lose an electron and form a [FeOĪmethyst is a three-dimensional network of tetrahedra where the silicon atoms are in the center and are surrounded by four oxygen atoms located at the vertices of a tetrahedron. ) and in some cases other transition metals, and the presence of other trace elements, which result in complex crystal lattice substitutions. Ancient Greeks wore amethyst and carved drinking vessels from it in the belief that it would prevent intoxication.Īmethyst, a semiprecious stone, is often used in jewelry.Īmethyst is a purple variety of quartz ( SiOĢ) and owes its violet color to irradiation, impurities of iron ( Fe 3+ The name comes from the Koine Greek αμέθυστος amethystos from α- a-, 'not' and μεθύσκω ( Ancient Greek) methysko / μεθώ metho ( Modern Greek), 'intoxicate', a reference to the belief that the stone protected its owner from drunkenness. 6 sided prism ending in 6 sided pyramid (typical)Ģ.65 constant variable in impure varietiesĪmethyst is a violet variety of quartz.

Purple rose quartz