Schoenfliesite is a rare magnesium-tin hydroxide mineral that typically forms small, sharp octahedral crystals. It is primarily found in hydrothermal tin deposits where it occurs as a secondary mineral alongside other tin-bearing species like cassiterite.
Is this schoenfliesite?
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 schoenfliesite with a known reference. Schoenfliesite sits at Mohs ~4, 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.
- 4Match the color rangeCompare against the expected color range: reddish brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: fibrous, prismatic.
Often confused with
Schoenfliesite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside schoenfliesite
Minerals reported to co-occur with schoenfliesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgSn(OH)₆
- Mohs hardness
- ~4
- Density
- 3.483 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Fibrous, prismatic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late-stage hydrothermal alteration product of hulsite in a boron-metasomatized limestone near the contact with a granite intrusive (Brooks Range, Alaska, USA)
Where rockhounds find schoenfliesite
Classic worldwide localities
- Northwest flank of Brooks Mountain, Seward Peninsula, Alaska, USA
- Pitkäranta district, Lake Ladoga, Karelia, Russia
- Damoshan deposit, Gejiu tin district, Yunnan Province, China
- Sungai Gow, Pahang, Malaysia
Field-hunting tip
Where it forms: A late-stage hydrothermal alteration product of hulsite in a boron-metasomatized limestone near the contact with a granite intrusive (Brooks Range, Alaska, USA). If you start seeing hulsite, goethite, maghemite in float, you are in the right ground. Typical habit: fibrous, prismatic. Train your eye for that shape before scanning the outcrop.







