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 — 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 — 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 — that is 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.



