Carmichaelite is a rare titanium chromium iron hydroxide, typically cinnamon brown to black. It occurs as microscopic inclusions in mantle-derived pyrope crystals carried up in kimberlite.
Is this carmichaelite?
4-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 carmichaelite with a known reference. Carmichaelite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Carmichaelite typically shows a metallic luster.
- 3Match the color rangeCompare against the expected color range: cinnamon brown, black.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: microscopic inclusions in mantle-derived pyrope.
Often confused with
Carmichaelite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside carmichaelite
Minerals reported to co-occur with carmichaelite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ti,Cr,Fe)(O,OH)₂
- Mohs hardness
- 6
- Density
- 3.95 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Microscopic Inclusions in Mantle-derived Pyrope
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Volcanic Xenoliths
Where rockhounds find carmichaelite
Classic worldwide localities
- Garnet Ridge, an ultramafic diatreme on the Colorado Plateau in Arizona, USA
Field-hunting tip
Look in volcanic xenoliths country, the host setting where carmichaelite typically forms. If you start seeing corundum, spinel, ilmenite in float, you are in the right ground. Field specimens usually show a microscopic inclusions in mantle-derived pyrope habit, so train your eye for that shape before scanning the outcrop.




