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, 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.





