Stokesite is a rare calcium tin silicate that typically forms as small, colorless, prismatic crystals. It is primarily prized by advanced mineral collectors and is most famously associated with granite pegmatite deposits where it occurs as a secondary mineral in vugs.
Is this stokesite?
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 stokesite with a known reference. Stokesite 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous, pearly on {100}.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive.
Often confused with
Stokesite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside stokesite
Minerals reported to co-occur with stokesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaSnSi₃O₉·2H₂O
- Mohs hardness
- ~6
- Density
- 3.185 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous, pearly on {100}
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Massive
- Cleavage
- Perfect on {101}, imperfect on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On axinite (Roscommon Cli®, England); in miarolitic cavities in a quartz-albite pegmatite (Věžná, Czech Republic)
Where rockhounds find stokesite
Classic worldwide localities
- Himalaya mine, Mesa Grande district, San Diego Co., California, USA
- Roscommon Cli®, St. Just, and in the Halvosso quarry, Longdowns, Cornwall, England
- Ctidružice and Věžná, Czech Republic
- Pitkäranta district, Lake Lagoda, Karelia
- Crystals from Corrégo do Urucum, near Galiléia, Minas Gerais, Brazil
- Iwaguro Sekizai quarry, Tahara, Gifu Prefecture, Japan
Field-hunting tip
Where it forms: On axinite (Roscommon Cli®, England); in miarolitic cavities in a quartz-albite pegmatite (Věžná, Czech Republic). If you start seeing axinite, cassiterite, albite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.








