Bredigite is an uncommon nesosilicate mineral typically found in high-temperature contact metamorphic environments and artificial slag. It most often occurs as small granular aggregates or massive patches, making it a challenging species for non-specialist collectors to identify without analytical verification.
Is this bredigite?
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 bredigite with a known reference. Bredigite sits at Mohs 5.5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bredigite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bredigite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular, massive, rarely distinct crystals.
Often confused with
Bredigite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bredigite
Minerals reported to co-occur with bredigite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₇Mg(SiO₄)₄
- Mohs hardness
- 5.5-6
- Density
- 3.39-3.41 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Granular, Massive, Rarely Distinct Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Contact Metamorphic Zones, High-temperature Furnace Slag
- Typical price
- n/a (rarely traded)
Where rockhounds find bredigite
Classic worldwide localities
- Bredig quarry, Pennsylvania, USA
- Hatrurim Formation, Israel
- Cimini Mountains, Italy
Field-hunting tip
Look in contact metamorphic zones, high-temperature furnace slag country — that is the host setting where bredigite typically forms. If you start seeing larnite, merwinite, calcite in float, you are in the right ground. Field specimens usually show a granular, massive, rarely distinct crystals habit, so train your eye for that shape before scanning the outcrop.





