Schüllerite is a rare member of the garnet group that is structurally related to andradite, appearing in small, well-formed dodecahedral crystals. It is typically found in contact metamorphic skarn environments associated with iron-rich hydrothermal alteration. Collectors look for its characteristic yellowish-brown hues and high luster, which distinguish it from more common garnet varieties.
Is this schüllerite?
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 schüllerite with a known reference. Schüllerite sits at Mohs 6.5-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Schüllerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Schüllerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, reddish-brown.
- 5Look at form & habitCrystal system: isometric. Typical habit: dodecahedral crystals.
Often confused with
Schüllerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside schüllerite
Minerals reported to co-occur with schüllerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Fe³⁺₂Si₃O₁₂
- Mohs hardness
- 6.5-7.5
- Density
- 3.5-3.8 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Isometric
- Crystal habit
- Dodecahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Skarn Deposits
- Typical price
- $20-200 depending on specimen quality
Where rockhounds find schüllerite
Classic worldwide localities
- Schwarzenberg, Germany
- Kola Peninsula, Russia
- San Benito County, California
Field-hunting tip
Look in skarn deposits country — that is the host setting where schüllerite typically forms. If you start seeing calcite, diopside, epidote in float, you are in the right ground. Field specimens usually show a dodecahedral crystals habit, so train your eye for that shape before scanning the outcrop.





