Glaucodot is a rare cobalt-iron sulfarsenide that is frequently confused with arsenopyrite and cobaltite due to its similar metallic appearance. It is typically found in hydrothermal veins associated with other cobalt minerals and is notable for its silver-white to tin-white color that may tarnish to a dull gray.
Is this glaucodot?
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 glaucodot with a known reference. Glaucodot 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. Glaucodot leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Glaucodot typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: tin-white, silver-white, gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Glaucodot vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside glaucodot
Minerals reported to co-occur with glaucodot. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Co,Fe)AsS
- Mohs hardness
- 5
- Density
- 5.99-6.03 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Massive, Granular
- Cleavage
- Distinct On {110}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins, Contact Metamorphic Deposits
- Typical price
- $20-150 thumbnail, $200-500 cabinet specimen
Where rockhounds find glaucodot
Classic worldwide localities
- Huallapa, Peru
- Tunaberg, Sweden
- Hakansboda, Sweden
- Schneeberg, Germany
- Ouro Preto, Brazil
Field-hunting tip
Look in hydrothermal veins, contact metamorphic deposits country — that is the host setting where glaucodot typically forms. If you start seeing cobaltite, arsenopyrite, chalcopyrite in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






