Rossmanite is a rare member of the tourmaline group, chemically distinguished by a lithium-rich composition and vacancies in the X-site of its crystal structure. It typically occurs as small, pale pink or colorless prismatic crystals within highly evolved lithium pegmatites. Collectors prize it as a rare species, though it is visually indistinguishable from other light-colored tourmalines without advanced analytical testing.
Is this rossmanite?
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 rossmanite with a known reference. Rossmanite sits at Mohs 7-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rossmanite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Rossmanite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, colorless, pale red.
- 5Look at form & habitCrystal system: trigonal. Typical habit: prismatic crystals.
Often confused with
Rossmanite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside rossmanite
Minerals reported to co-occur with rossmanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ☐(LiAl₂)Al₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
- Mohs hardness
- 7-7.5
- Density
- 3.06 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- Indistinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Lithium-rich Pegmatites
- Typical price
- $50-500 thumbnail
Where rockhounds find rossmanite
Classic worldwide localities
- Rožná, Czech Republic
- Corinth, Massachusetts, USA
- San Diego County, California, USA
Field-hunting tip
Look in lithium-rich pegmatites country — that is the host setting where rossmanite typically forms. If you start seeing quartz, lepidolite, albite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.







