Silesiaite is a rare iron-rich member of the garnet group historically described from the Silesia region. It typically appears as yellowish to brown dodecahedral crystals formed in metamorphic environments and is highly sought after by systematic mineral collectors.
Is this silesiaite?
4-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 silesiaite with a known reference. Silesiaite sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: yellow, brown, greenish.
- 4Look at form & habitCrystal system: triclinic.
Often confused with
Silesiaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside silesiaite
Minerals reported to co-occur with silesiaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Fe₂Sn₂(Si₂O₇)₂(Si₂O₆OH)₂
- Mohs hardness
- 6.5-7
- Density
- 3.5-3.6 g/cm³
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In granitic pegmatite (Poland); in calcic Cu-Au skarn (Spain)
Where rockhounds find silesiaite
Classic worldwide localities
- Szklarska Poręba Huta quarry, Lower Silesia, Poland (type locality)
- El Valle-Boinás, Asturias, northern Spain
Field-hunting tip
Where it forms: In granitic pegmatite (Poland); in calcic Cu-Au skarn (Spain). If you start seeing andradite, clinopyroxene, actinolite in float, you are in the right ground.






