Hodgesmithite is a rare secondary sulfate mineral that typically forms as a crust or as thin, platy crystals. It is primarily known from the oxidized zones of lead-zinc deposits, specifically found at the Broken Hill mine in Australia. Collectors usually identify it through association with other zinc-rich secondary minerals like smithsonite.
Is this hodgesmithite?
4-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 hodgesmithite with a known reference. Hodgesmithite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 3Match the color rangeCompare against the expected color range: white, colorless.
- 4Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals, radiating aggregates.
Often confused with
Hodgesmithite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hodgesmithite
Minerals reported to co-occur with hodgesmithite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Cu,Zn)₆Zn(SO₄)₂(OH)₁₀·3H₂O
- Mohs hardness
- 2
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Tabular crystals, radiating aggregates
- Rarity
- Rare
- Uses
- Collector
- Host rock
- oxidized ore deposits
Where rockhounds find hodgesmithite
Classic worldwide localities
- Block 14 Opencut, Broken Hill, New South Wales, Australia
Field-hunting tip
Where it forms: oxidized ore deposits. If you start seeing calcite, smithsonite, gypsum in float, you are in the right ground. Typical habit: tabular crystals, radiating aggregates. Train your eye for that shape before scanning the outcrop.






