Amethyst occurs in primary
hues from a light lavender or pale violet to a deep purple. Amethyst may exhibit one or both secondary hues, red and blue. High-quality amethyst can be found in
Siberia,
Sri Lanka,
Brazil,
Uruguay, and the Far East. 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. "Rose de France" is defined by its markedly light shade of the
purple, reminiscent of a
lavender /
lilac shade. These pale colors were once considered undesirable, but have recently become popular due to intensive marketing. Green quartz is sometimes called
green amethyst; the scientific name is
prasiolite. Other names for green quartz are
vermarine and
lime citrine. Amethyst frequently shows color zoning, with the most intense color typically found at the crystal terminations. One of
gem cutters' tasks is to make a finished product with even color. Sometimes, only a thin layer of a natural, uncut amethyst is violet colored, or the color is very uneven. The uncut gem may have only a small portion that is suitable for faceting. The color of amethyst has been demonstrated to result from substitution by
irradiation of trivalent iron (Fe3+) for silicon in the structure, in the presence of trace elements of large ionic radius, but loses its dichroism, unlike genuine citrine. When partially heated, amethyst can result in
ametrine. Amethyst can fade in tone if overexposed to light sources, and can be artificially darkened with adequate irradiation. It does not
fluoresce under either short-wave or long-wave
UV light. ==Geographic distribution==