Miersite is a rare silver copper iodide mineral that typically occurs as small, bright yellow tetrahedral crystals. It is primarily found in the oxidized zones of silver ore deposits where it is often associated with other halide minerals. Collectors value it for its distinct bright yellow color and relatively rare occurrence.
Is this miersite?
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 miersite with a known reference. Miersite sits at Mohs 2-2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Miersite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Miersite typically shows a resinous luster.
- 4Match the color rangeCompare against the expected color range: yellow, bright yellow, pale yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: tetrahedral crystals.
Often confused with
Miersite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside miersite
Minerals reported to co-occur with miersite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ag,Cu)I
- Mohs hardness
- 2-2.5
- Density
- 5.62 g/cm³
- Streak
- Yellow
- Luster
- Resinous
- Transparency
- Translucent
- Crystal system
- Cubic
- Crystal habit
- Tetrahedral Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Silver-bearing Ore Deposits
- Typical price
- $50-500 depending on specimen size and quality
Where rockhounds find miersite
Classic worldwide localities
- Broken Hill, New South Wales, Australia
- Tonopah, Nevada, USA
- Bisbee, Arizona, USA
Field-hunting tip
Look in oxidized zones of silver-bearing ore deposits country — that is the host setting where miersite typically forms. If you start seeing cerussite, smithsonite, malachite in float, you are in the right ground. Field specimens usually show a tetrahedral crystals habit, so train your eye for that shape before scanning the outcrop.





