Fairchildite is a rare potassium calcium carbonate mineral typically found in environments associated with burning coal seams or volcanic vents. It is extremely unstable in moist air, often dehydrating or altering rapidly, making it a challenging and prized specimen for serious mineral collectors.
Is this fairchildite?
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 fairchildite with a known reference. Fairchildite sits at Mohs 2.5, 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: colorless.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: platy.
Often confused with
Fairchildite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside fairchildite
Minerals reported to co-occur with fairchildite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Ca(CO₃)₂
- Mohs hardness
- 2.5
- Density
- 2.45 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Platy
- Cleavage
- On {0001}, good
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed from fused wood ash in partially burned trees
Where rockhounds find fairchildite
Classic worldwide localities
- Grand Canyon National Park, Coconino Co., Arizona, USA
- Kaniksu National Forest, near Coolin, Bonner Co., Idaho, USA
- Eganville and Deseronto, Ontario, Canada
Field-hunting tip
Where it forms: Formed from fused wood ash in partially burned trees. If you start seeing bütschliite, calcite in float, you are in the right ground. Typical habit: platy. Train your eye for that shape before scanning the outcrop.



