Uvarovite Garnet
Uvarovite
A variety of Garnet Group
What is Uvarovite Garnet?
Uvarovite Garnet is a rare variety of garnet that usually bears a rich green color. Unfortunately, its crystals are usually too small to be faceted into gemstones, though pieces are sometimes incorporated into jewelry anyway. Found in scattered locations around the world, the most prominent source of uvarovite Garnet is a mine in central Finland.
Optical Properties
- Refractive Index
- 1.87
- Optical Character
- Isotropic
- Dispersion
- 0.014-0.021
Market Value Factors
Pricing varies for every rock and mineral, so use these universal factors to gauge Uvarovite Garnet before comparing listings or appraisals.
Size & Weight
Larger, intact specimens usually command higher prices.
Rarity & Demand
Scarce material or popular varieties sell at a premium.
Condition & Finish
Chips, repairs, and heavy wear lower value; clean prep helps.
Treatment & Provenance
Untreated specimens with documented locality are prized.
Uvarovite Garnet Localities Map
See where Uvarovite Garnet is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.
Key Characteristics
Characteristics of Uvarovite Garnet
Minerals in the uvarovite-grossular series are stable up to temperatures of 1410 °C at low pressure.
Formation of Uvarovite Garnet
Uvarovite most commonly occurs in solid solution with grossular or andradite, and is generally found associated with serpentinite, chromite, metamorphic limestones, and skarn ore-bodies. The most significant source of uvarovite historically has been a now-closed copper mine at Outokumpu, Finland, from where most museum specimens have been collected. The uvarovite crystals found in the Outokumpu district are among a wide range of chromium-rich silicate phases found in association with volcanogenic copper-cobalt-zinc sulfide ore deposits which are known to have an unusually high chromium content. Uvarovite occurrences in the United States are predominantly found in the western portion of the country, including localities in New Mexico, Arizona, and California. In the eastern United States, uvarovite has been confirmed in Lancaster County, Pennsylvania. The mineral has also been reported from eastern Cuba.. 9 grains of uvarovite occur in a heavy mineral fraction of bulk stream sediment HM-10 collected in Bunker Hill creek, below the historic Bunker Hill gold mine, south of Nelson in British Columbia Canada. Its source is likely near serpentinites and argillaceous limestones within about 450 m upstream of the silt site . Notable localities in Europe besides the Outokumpu site known to bear uvarovite include Roros, Norway; Pitkaranta, Finland; Val Malenco, Italy; Pico do Posets near Venasque, Spain; Kip Daglari, Turkey; and Biserk and Sarany, Russia. In Africa, uvarovite has been reported from the Bushveld Igneous Complex of Transvaal, South Africa and from the Vumba Schist Belt in Botswana. In Asia, uvarovite has been reported from Taiwan. and Japan In Australia, uvarovite has been reported from chromite deposits in southern New South Wales.
Quick Facts
Physical Properties
- Color
- Green, emerald-green, green-black
- Hardness (Mohs)
- 6.5 - 7
- Density
- 3.848 g/cm³
- Streak
- White
- Luster
- Vitreous
- Crystal System
- Isometric
Chemical Properties
- Chemical Formula
- Ca3Cr2(SiO4)3
- Elements
- Ca, Cr, O, Si
Also Known As
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Uvarovite Garnet FAQs
How do I identify Uvarovite Garnet?
Uvarovite Garnet can be identified by its hardness of 6.5 - 7 on the Mohs scale, Green color, Vitreous luster, Isometric crystal system. Look for these key characteristics when examining specimens.
What color is Uvarovite Garnet?
Uvarovite Garnet typically appears in Green, emerald-green, green-black. Color can vary depending on impurities and formation conditions.
How hard is Uvarovite Garnet?
Uvarovite Garnet has a hardness of 6.5 - 7 on the Mohs scale. This gives it moderate hardness.
What is the characteristics of uvarovite garnet of Uvarovite Garnet?
Minerals in the uvarovite-grossular series are stable up to temperatures of 1410 °C at low pressure.
What is the formation of uvarovite garnet of Uvarovite Garnet?
Uvarovite most commonly occurs in solid solution with grossular or andradite, and is generally found associated with serpentinite, chromite, metamorphic limestones, and skarn ore-bodies. The most significant source of uvarovite historically has been a now-closed copper mine at Outokumpu, Finland, from where most museum specimens have been collected. The uvarovite crystals found in the Outokumpu district are among a wide range of chromium-rich silicate phases found in association with volcanogenic copper-cobalt-zinc sulfide ore deposits which are known to have an unusually high chromium content. Uvarovite occurrences in the United States are predominantly found in the western portion of the country, including localities in New Mexico, Arizona, and California. In the eastern United States, uvarovite has been confirmed in Lancaster County, Pennsylvania. The mineral has also been reported from eastern Cuba.. 9 grains of uvarovite occur in a heavy mineral fraction of bulk stream sediment HM-10 collected in Bunker Hill creek, below the historic Bunker Hill gold mine, south of Nelson in British Columbia Canada. Its source is likely near serpentinites and argillaceous limestones within about 450 m upstream of the silt site . Notable localities in Europe besides the Outokumpu site known to bear uvarovite include Roros, Norway; Pitkaranta, Finland; Val Malenco, Italy; Pico do Posets near Venasque, Spain; Kip Daglari, Turkey; and Biserk and Sarany, Russia. In Africa, uvarovite has been reported from the Bushveld Igneous Complex of Transvaal, South Africa and from the Vumba Schist Belt in Botswana. In Asia, uvarovite has been reported from Taiwan. and Japan In Australia, uvarovite has been reported from chromite deposits in southern New South Wales.