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.

Hardness
3.5
Mohs
Luster
Vitreous to subadamantine
Streak
Yellow ochre
Transparency
Transparent

Is this beaverite-(zn)?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try 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.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: yellow ochre.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to subadamantine.
  • 4
    Match the color range
    Compare against the expected color range: yellow, brownish yellow.
  • 5
    Look at form & habit
    Crystal 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.

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
PbZnFe₂(SO₄)₂(OH)₆
Mohs hardness
3.5
Density
4.25 g/cm³
Streak
Yellow ochre
Luster
Vitreous to subadamantine
Transparency
Transparent
Crystal system
Trigonal
Crystal habit
Microcrystalline aggregates, earthy crusts
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
A secondary mineral in the oxidized zone of a hydrothermal Cu-Pb-Zn ore deposit

Where rockhounds find beaverite-(zn)

Classic worldwide localities

  • Mikawa mine, Mikawa, Aga-machi, Higashikanbara-gun, Niigata Prefecture, Japan

Field-hunting tip

Where it forms: A secondary mineral in the oxidized zone of a hydrothermal Cu-Pb-Zn ore deposit. If you start seeing anglesite, galena, pyrite in float, you are in the right ground. Typical habit: microcrystalline aggregates, earthy crusts. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify beaverite-(zn)?+
Mohs hardness is 3.5. Luster: vitreous to subadamantine. The streak is yellow ochre. Common colors include yellow, brownish yellow.
Where is beaverite-(zn) found?+
Notable localities include Mikawa mine, Mikawa, Aga-machi, Higashikanbara-gun, Niigata Prefecture, Japan.
Is beaverite-(zn) safe to handle?+
Beaverite-(Zn) contains lead. Contains lead and copper, which can be toxic if ingested or inhaled as dust. Wash hands thoroughly after handling specimens.
What rocks look like beaverite-(zn)?+
Beaverite-(Zn) is most often confused with Jarosite, Beaverite-(Cu), Plumbojarosite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with beaverite-(zn)?+
Beaverite-(Zn) commonly co-occurs with Anglesite, Galena, Pyrite, Sphalerite, Quartz. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does beaverite-(zn) form in?+
Where it forms: A secondary mineral in the oxidized zone of a hydrothermal Cu-Pb-Zn ore deposit. Working float back to the host body is the standard way to chase a fresh occurrence.
What is beaverite-(zn) used for?+
Beaverite-(Zn) is used in collector.

Find beaverite-(zn) on the map

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