Vanadio-pargasite is a rare member of the hornblende group distinguished by its vibrant green color resulting from vanadium substitution in the crystal structure. It is typically found as prismatic crystals in metamorphosed limestone or dolomitic rocks. Collectors value it for its striking color and limited geographic distribution.
Is this vanadio-pargasite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch vanadio-pargasite with a known reference. Vanadio-pargasite sits at Mohs ~6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale green.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: bright green, emerald-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals.
Often confused with
Vanadio-pargasite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside vanadio-pargasite
Minerals reported to co-occur with vanadio-pargasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂(Mg₄V)[Si₆Al₂]O₂₂(OH)₂
- Mohs hardness
- ~6
- Density
- 3.05 g/cm³
- Streak
- Pale green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals
- Cleavage
- Perfect on {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed during prograde (granulite-facies) metamorphism of Cr-V-bearing calcite-dolomite and siliceous sediments
Where rockhounds find vanadio-pargasite
Classic worldwide localities
- Pereval marble quarry, near Sludyanka, Irkutsk region, southern Lake Baikal, Siberia, Russia
Field-hunting tip
Where it forms: Formed during prograde (granulite-facies) metamorphism of Cr-V-bearing calcite-dolomite and siliceous sediments. If you start seeing magnesiocoulsonite-magnesochromite, cr-v-rich spinel, phlogopite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.






