Gortdrumite is an exceptionally rare copper-mercury sulfide mineral first identified in the Gortdrum mine in Ireland. It is typically found as microscopic grains or small aggregates within copper sulfide ores, making it a prized discovery for systematic mineral collectors.
Is this gortdrumite?
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 gortdrumite with a known reference. Gortdrumite sits at Mohs 3.5-4, 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: lead gray, black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral grains, microscopic crystals.
Often confused with
Gortdrumite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gortdrumite
Minerals reported to co-occur with gortdrumite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Fe)₆Hg₂S₅
- Mohs hardness
- 3.5-4
- Density
- 6.8 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral grains, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Admixed with other sulfide minerals in a vein cutting dolomitized limestone; mineral associations suggest formation at less than 200°C
Where rockhounds find gortdrumite
Classic worldwide localities
- Gortdrum deposit, near Tipperary, Co. Tipperary, Ireland (type locality)
Field-hunting tip
Where it forms: Admixed with other sulfide minerals in a vein cutting dolomitized limestone; mineral associations suggest formation at less than 200°C. If you start seeing chalcopyrite, bornite, chalcocite in float, you are in the right ground. Typical habit: anhedral grains, microscopic crystals. Train your eye for that shape before scanning the outcrop.







