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. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: grayish tin white, reddish silver white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: massive.
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
- 6.055 g/cm³
- Colors
- Grayish tin whiteReddish silver white
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Massive
- Cleavage
- Perfect on {010}, less so on {101}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In deep-seated deposits of high-temperature hydrothermal origin
Where rockhounds find glaucodot
Classic worldwide localities
- Standard Consolidated mine, Sumpter, Grant Co., Oregon, and at Franconia, Grafton Co., New Hampshire, USA
- Huasco, Tarapacá, Chile (type locality)
- Cobalt-Gowganda district, Ontario, Canada
- Håkansböda, Västmanland, as large twinned and untwinned crystals, Sweden
- Tunaberg, Södermanland, Sweden
- Skutterud, Norway
Field-hunting tip
Where it forms: In deep-seated deposits of high-temperature hydrothermal origin. If you start seeing cobaltite, pyrite, chalcopyrite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.





