Fengchengite is a rare sodium calcium iron silicate, typically rose to deep rose. It was approved as a distinct mineral species in 2007. It was first described from near Saima Town, ~60 km NNE of Fengcheng City, Liaoning Province, China.
Is this fengchengite?
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 fengchengite with a known reference. Fengchengite sits at Mohs ~5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: rose, deep rose.
- 5Look at form & habitCrystal system: trigonal.
Often confused with
Fengchengite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fengchengite
Minerals reported to co-occur with fengchengite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₁₂☐₃Ca₆Fe³⁺₃Zr₃Si(Si₂₅O₇₃)(H₂O)₃(OH)₂
- Mohs hardness
- ~5
- Density
- 2.90 g/cm³
- Colors
- RoseDeep rose
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Trigonal
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In agpaitic nepheline syenite and pegmatite, crystallized directly from a REE-, U-, Th-, and Zr-rich alkaline magma enriched in volatile components
Where rockhounds find fengchengite
Classic worldwide localities
- Fengcheng, Liaoning Province, China
Field-hunting tip
Where it forms: In agpaitic nepheline syenite and pegmatite, crystallized directly from a REE-, U-, Th-, and Zr-rich alkaline magma enriched in volatile components. If you start seeing microcline, orthoclase, albite in float, you are in the right ground.








