Russian Jadeite — Polar Ural Production
Russian Jadeite — Polar Ural Production
A minor but gemmologically significant source of jadeite outside the Burmese-Guatemalan main supply
Russian jadeite is the trade name for jadeite from the Polar Ural Mountains of Russia, principally from the Pusyierka and Levyi Keros deposits in the Yamal-Nenets and Khanty-Mansi autonomous regions. The deposits were discovered in the late twentieth century and brought to commercial production in the 1990s and 2000s. Russian jadeite is a minor source by global volume — Myanmar (Burma) remains the dominant world supplier, with Guatemala the secondary commercial source — but the Polar Ural material is gemmologically significant as a documented serpentinite-hosted jadeite source outside the main supply.
Composition and properties
Jadeite is the high-pressure sodium-aluminium pyroxene, NaAlSi2O6, monoclinic, with hardness 6.5 to 7 and refractive indices 1.652 to 1.688. Specific gravity ranges 3.30 to 3.36. Russian jadeite shows the standard jadeite optical and physical properties; it is not chemically distinct from Burmese or Guatemalan material in routine gemmological testing. Identification of geographic origin requires either documented chain of custody or specialised laboratory analysis (LA-ICP-MS trace element fingerprinting), and origin reports for Russian jadeite are not routinely issued.
Colour ranges from apple-green to near-colourless, with white, grey-green, and occasional lavender material reported. The chromium-coloured imperial-green saturation characteristic of fine Burmese material is rarely encountered in Russian rough; most Russian jadeite cuts to less saturated greens or to white-and-green mixed material suitable for bangles and carvings rather than for high-end cabochons.
Geology of the Polar Ural deposits
The Polar Ural jadeite deposits are hosted in serpentinite ophiolite — Mesozoic-age oceanic crust caught between the European and Siberian plates and exposed by orogenic uplift. The geological context resembles the Burmese, Guatemalan, and Californian jadeite settings: high-pressure, low-temperature metamorphism in subduction-zone or related ophiolite settings produces the conditions necessary for jadeite stability. The Polar Ural deposits are at the intersection of European and Siberian continental fragments and represent a distinct geological terrane from the Eurasian continental interior.
Production is small. The deposits are remote, climate is harsh, and operational economics are challenging. Russian jadeite reaches the international trade through Yekaterinburg and Moscow dealers and onward to Hong Kong, Bangkok, and Western markets in modest quantities.
In the trade
Russian jadeite occupies a niche position in the global jadeite market. The material does not match the saturation and translucency of fine Burmese imperial jade and trades at a substantial discount to top Burmese rough. It is broadly comparable to Guatemalan apple-green material and to the Russian-Chinese border deposit production from the Sayan range. Calibrated cabochons in 5 to 15 mm sizes are reasonably available in the Hong Kong and Bangkok wholesale markets at modest prices; bangle-quality material is supplied to Chinese carving workshops.
The 2022 onward Russian sanctions environment has affected commercial flows of Russian-origin coloured stones. The G7 Russian-origin diamond sanctions of 2024 do not specifically target coloured stones, but enhanced compliance scrutiny across the broader trade has increased documentation requirements for Russian-origin material. Buyers of Russian jadeite in 2026 should expect heightened provenance verification at customs and at the wholesale trade level.
Identification
Standard refractive index, specific gravity, and Raman spectroscopy identify jadeite without difficulty. Distinction between Russian, Burmese, and Guatemalan jadeite requires either documented provenance or specialised LA-ICP-MS trace-element analysis. The chromium-to-iron ratio differs between sources but the differences are not always definitive at trade-relevant scales. Treated jadeite — bleached and polymer-impregnated B-jade and dyed C-jade — is the standard concern in jadeite identification across all sources, and Russian rough is subject to the same treatment-disclosure conventions as Burmese material under AGTA and CIBJO guidelines.
Care
Jadeite is durable and well-suited to daily wear. Hardness 6.5 to 7 and very high toughness make it one of the more practical coloured stones for ring use. Clean with mild soap and warm water; avoid prolonged exposure to acids and to strong cleaning chemicals which can attack any polymer impregnation in treated material. Ultrasonic cleaning is generally safe for untreated jadeite but should be avoided for treated material.
Position in the market
Russian jadeite remains a minor commercial source in 2026. The species is genuinely interesting to collectors of geographic provenance — it documents jadeite formation in a distinct ophiolite terrane outside the main supply — but does not displace Burmese material at the high end of the market. For mainstream jewellery work, Russian jadeite is a sensible supply alternative for white, grey-green, and apple-green cabochon production at intermediate price points.