Criddleite is an extremely rare sulfosalt mineral found in gold-bearing hydrothermal deposits. It is typically identified through microscopic examination of polished sections, appearing as small, grey metallic grains intergrown with other minerals like aurostibite and stibnite.
Is this criddleite?
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 criddleite with a known reference. Criddleite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Criddleite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Criddleite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains and inclusions.
Often confused with
Criddleite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Criddleite is noticeably harder (Mohs 3-3.5 vs. 2); streak differs, so Criddleite leaves black, Stibnite leaves lead-gray.

How to tell apart: Gudmundite is the harder of the two (Mohs 6 vs. 3-3.5); streak differs, so Criddleite leaves black, Gudmundite leaves dark gray to black.
Often found alongside criddleite
Minerals reported to co-occur with criddleite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₂Au₃Sb₁₀S₁₀
- Mohs hardness
- 3-3.5
- Density
- 8.7 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral Grains and Inclusions
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Gold Deposits
- Typical price
- $200-800+ depending on size and rarity of specimen
Where rockhounds find criddleite
Classic worldwide localities
- Hemlo gold deposit, Ontario, Canada
Field-hunting tip
Look in hydrothermal gold deposits country, the host setting where criddleite typically forms. If you start seeing aurostibite, stibnite, pyrite in float, you are in the right ground. Field specimens usually show a anhedral grains and inclusions habit, so train your eye for that shape before scanning the outcrop.



