Rhabdoborite-(V) is an exceptionally rare borate mineral found primarily in the Kola Peninsula of Russia. It typically appears as small, colorless tabular crystals or aggregates within contact-metasomatic skarn environments associated with alkaline massifs.
Is this rhabdoborite-(v)?
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 rhabdoborite-(v) with a known reference. Rhabdoborite-(V) sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rhabdoborite-(V) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Rhabdoborite-(V) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Rhabdoborite-(V) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rhabdoborite-(v)
Minerals reported to co-occur with rhabdoborite-(v). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₁₂V₃O₆(BO₃)₆F₆
- Mohs hardness
- 5
- Density
- 3.37 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarns in Alkaline Igneous Complexes
- Typical price
- $50-300+ depending on crystal size and quality
Where rockhounds find rhabdoborite-(v)
Classic worldwide localities
- Kola Peninsula, Russia
Field-hunting tip
Look in skarns in alkaline igneous complexes country — that is the host setting where rhabdoborite-(v) typically forms. If you start seeing fluoborite, ludwigite, magnetite in float, you are in the right ground. Field specimens usually show a tabular crystals, subparallel aggregates habit, so train your eye for that shape before scanning the outcrop.




