Keystoneite is a rare magnesium nickel iron oxide, typically golden yellow. It was approved as a distinct mineral species in 1987. It was first described from Keystone mine, Magnolia district, Boulder Co., Colorado, USA.
Is this keystoneite?
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 keystoneite with a known reference. Keystoneite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale yellow-green.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: golden yellow, orange yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular, radial.
Often confused with
Keystoneite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside keystoneite
Minerals reported to co-occur with keystoneite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mg₀.₅NiFe³⁺(Te⁴⁺O₃)₃·4H₂O
- Mohs hardness
- 2-3
- Density
- 4.4 g/cm³
- Streak
- Pale yellow-green
- Luster
- Adamantine
- Transparency
- Semitransparent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular, radial
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare secondary mineral formed in the oxidized zone of a complex polymetallic hydrothermal mineral deposit
Where rockhounds find keystoneite
Classic worldwide localities
- Keystone mine, Magnolia district, Boulder Co., Colorado, USA
Field-hunting tip
Where it forms: A rare secondary mineral formed in the oxidized zone of a complex polymetallic hydrothermal mineral deposit. If you start seeing melonite, tellurium, paratellurite in float, you are in the right ground. Typical habit: acicular, radial. Train your eye for that shape before scanning the outcrop.








