Calderite is a rare manganese-iron garnet species primarily found in manganese-rich metamorphic environments. It is notoriously difficult to distinguish visually from other garnets like Spessartine without chemical analysis, though its association with black manganese ores is a helpful diagnostic clue for collectors.
Is this calderite?
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 calderite with a known reference. Calderite sits at Mohs 7-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Calderite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Calderite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: reddish-brown, brown, orange-brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: dodecahedral crystals, massive, granular.
Often confused with
Calderite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside calderite
Minerals reported to co-occur with calderite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn³⁺₂Fe³⁺₂(SiO₄)₃
- Mohs hardness
- 7-7.5
- Density
- 3.9-4.0 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral Crystals, Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Manganese Deposits
- Typical price
- $50-500 depending on specimen quality and size
Where rockhounds find calderite
Classic worldwide localities
- Kodur, India
- Jakobsberg, Sweden
- Franklin, New Jersey, USA
- Otanmäki, Finland
Field-hunting tip
Look in metamorphosed manganese deposits country — that is the host setting where calderite typically forms. If you start seeing braunite, hausmannite, bixbyite in float, you are in the right ground. Field specimens usually show a dodecahedral crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.





