Beaverite-(Zn) is a rare secondary mineral typically found in the oxidized zones of lead-zinc ore deposits. It usually appears as fine-grained, earthy coatings or crusts with a characteristic yellow color, often requiring micro-analysis for positive identification.
Is this beaverite-(zn)?
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 beaverite-(zn) with a known reference. Beaverite-(Zn) sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Beaverite-(Zn) leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Beaverite-(Zn) typically shows a earthy luster.
- 4Match the color rangeCompare against the expected color range: yellow, greenish-yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: microcrystalline aggregates, earthy crusts.
Often confused with
Beaverite-(Zn) vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Luster reads earthy on Beaverite-(Zn) and vitreous on Jarosite.

How to tell apart: Streak differs — Beaverite-(Zn) leaves yellow, Beaverite-(Cu) leaves pale yellow.

Often found alongside beaverite-(zn)
Minerals reported to co-occur with beaverite-(zn). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbCu₂(Zn,Fe³⁺)₂(SO₄)₂(OH)₆
- Mohs hardness
- 3.5
- Density
- 4.2 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Earthy
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Microcrystalline Aggregates, Earthy Crusts
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-zinc Hydrothermal Deposits
- Typical price
- $20-150 per specimen
Where rockhounds find beaverite-(zn)
Classic worldwide localities
- Beaver County, Utah, USA
- Tsumeb, Namibia
- Lavrion, Greece
- Broken Hill, Australia
Field-hunting tip
Look in oxidized lead-zinc hydrothermal deposits country — that is the host setting where beaverite-(zn) typically forms. If you start seeing anglesite, cerussite, smithsonite in float, you are in the right ground. Field specimens usually show a microcrystalline aggregates, earthy crusts habit, so train your eye for that shape before scanning the outcrop.




