Genplesite is a rare tin-bearing calcium hydroxide mineral typically found as small, clear, tabular crystals in skarn environments. It is predominantly known from the Pitkyaranta mining district, where it forms alongside various tin and sulfide minerals. Due to its extreme rarity and small crystal size, it is almost exclusively sought after by advanced systematic mineral collectors.
Is this genplesite?
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 genplesite with a known reference. Genplesite sits at Mohs ~3, 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: colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals.
Often confused with
Genplesite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside genplesite
Minerals reported to co-occur with genplesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Sn(SO₄)₂(OH)₆·3H₂O
- Mohs hardness
- ~3
- Density
- 2.78 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late-stage, low-temperature hydrothermal mineral in cavities in massive chalcopyrite
Where rockhounds find genplesite
Classic worldwide localities
- No. 1 shaft (level 750-m), Oktyabr’skoe Cu-Ni-Pd-Pt deposit (Oktyabr’sky mine), Talnakh, Norilsk district, Siberia, Russia
Field-hunting tip
Where it forms: A late-stage, low-temperature hydrothermal mineral in cavities in massive chalcopyrite. If you start seeing greenalite, chamosite, pectolite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.







