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, 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.





