Murdochite is an uncommon, dense black mineral that typically occurs as microscopic cubic crystals or crusts in oxidized mineral deposits. Collectors usually look for it in association with secondary copper and lead minerals like wulfenite. It is primarily valued as a rare species for systematic mineral collections.
Is this murdochite?
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 murdochite with a known reference. Murdochite 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. Murdochite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Murdochite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: cubic. Typical habit: tiny cubic crystals, massive, or as crusts.
Often confused with
Murdochite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside murdochite
Minerals reported to co-occur with murdochite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₄Cu₆O₈(Cl,Br)₂
- Mohs hardness
- 3.5-4
- Density
- 6.6 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Tiny Cubic Crystals, Massive, Or as Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Copper-lead Hydrothermal Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find murdochite
Classic worldwide localities
- Mammoth-St. Anthony Mine, Arizona, USA
- Tsumeb, Namibia
- Sierra Gorda, Chile
Field-hunting tip
Look in oxidized zones of copper-lead hydrothermal ore deposits country — that is the host setting where murdochite typically forms. If you start seeing wulfenite, cerussite, dioptase in float, you are in the right ground. Field specimens usually show a tiny cubic crystals, massive, or as crusts habit, so train your eye for that shape before scanning the outcrop.







