Florenskyite is a extremely rare iron titanium phosphide mineral discovered in the Kaidun meteorite. It occurs as microscopic inclusions within metallic phases and is highly prized by meteorite collectors and researchers for its unique extraterrestrial origin.
Is this florenskyite?
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 florenskyite with a known reference. Florenskyite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: cream white.
- 4Look at form & habitCrystal system: orthorhombic. Typical habit: inclusions, microscopic crystals.
Often confused with
Florenskyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside florenskyite
Minerals reported to co-occur with florenskyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeTiP
- Mohs hardness
- 5-6
- Density
- 6.12 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Inclusions, microscopic crystals
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Inclusion in serpentine in a carbonaceous, enstatitic, and Rumaruti type chondrodite meteorite
Where rockhounds find florenskyite
Classic worldwide localities
- Kaidum chondritic meteorite, which fell in South Yemen in 1980 (type locality)
Field-hunting tip
Where it forms: Inclusion in serpentine in a carbonaceous, enstatitic, and Rumaruti type chondrodite meteorite. If you start seeing fe-rich serpentine, pentlandite, andreyivanovite in float, you are in the right ground. Typical habit: inclusions, microscopic crystals. Train your eye for that shape before scanning the outcrop.


