Deep Siberian
The highest quality standard. Primary hue of deep purple (75-80%) with secondary flashes of blue and red. Contains the "Raspberry Flash".
Deep Dive: The Science of Siberian Color
The term "Siberian" originally referred to deposits in the Ural Mountains of Russia, which produced stones with a unique reddish velvet overtone. While these mines are largely depleted, the term persists in 2026 as a trade grade rather than an origin guarantee.
Optical Properties
A true Deep Siberian grade stone must display strong dichroism. When viewed through a dichroscope, one axis should show reddish-purple and the other bluish-purple. If the stone appears "dead" or black in low light (extinction), it fails to meet the grade. The "Raspberry Flash" is caused by the precise ratio of iron color centers allowing red wavelengths to pass through the crystal lattice under incandescent lighting.
Collector Considerations
For the serious collector, verifying this grade requires viewing the stone under multiple light sources. LED lighting often washes out the red flash. Top-tier specimens are typically unheated, as heat treatment generally lightens the stone. Synthetic production (hydrothermal growth) can replicate this color, making inclusion analysis (looking for natural imperfections) critical for verification.