Edoylerite is a rare mercury chromium oxide that forms canary yellow to orangeish yellow acicular to prismatic crystals. Associated minerals include cinnabar, deanesmithite and quartz. It was first described from the Clear Creek claim, San Benito Co., California, USA.
Is this edoylerite?
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 edoylerite with a known reference. Edoylerite 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. Edoylerite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Edoylerite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: canary yellow, orangeish yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular to prismatic crystals.
Often confused with
Edoylerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside edoylerite
Minerals reported to co-occur with edoylerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Hg²⁺₃(Cr⁶⁺O₄)S₂
- Mohs hardness
- 2.5
- Density
- 7.11 g/cm³
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Acicular to Prismatic Crystals
- Cleavage
- On {010}, Good; On {101}, Fair
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Serpentinite
Where rockhounds find edoylerite
Classic worldwide localities
- Clear Creek claim, San Benito County, California, USA
Field-hunting tip
Look in serpentinite country, the host setting where edoylerite typically forms. If you start seeing benitoite, nefedievite, chromite in float, you are in the right ground. Field specimens usually show a acicular to prismatic crystals habit, so train your eye for that shape before scanning the outcrop.




