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.

Hardness
5
Mohs
Luster
Metallic
Streak
Black
Transparency
Opaque

Is this glaucodot?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch glaucodot with a known reference. Glaucodot sits at Mohs 5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: black.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: metallic.
  • 4
    Match the color range
    Compare against the expected color range: grayish tin white, reddish silver white.
  • 5
    Look at form & habit
    Crystal 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.

Common questions

How do you identify glaucodot?+
Mohs hardness is 5. Luster: metallic. The streak is black. Common colors include grayish tin white, reddish silver white.
Where is glaucodot found?+
Notable localities include 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.
Is glaucodot safe to handle?+
Glaucodot contains arsenic and cobalt and calls for real care. Contains arsenic. Handle with care, wash hands after handling, avoid creating dust, and keep away from children and food preparation areas.
What rocks look like glaucodot?+
Glaucodot is most often confused with Arsenopyrite, Cobaltite, Skutterudite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with glaucodot?+
Glaucodot commonly co-occurs with Cobaltite, Pyrite, Chalcopyrite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does glaucodot form in?+
Where it forms: In deep-seated deposits of high-temperature hydrothermal origin. Working float back to the host body is the standard way to chase a fresh occurrence.
What is glaucodot used for?+
Glaucodot is used in collector.

Find glaucodot on the map

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