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Home / The Crystal Guide / Descloizite
A stone guide

Descloizite

Very heavy brown-black to cherry crystal crusts and fern-like aggregates with greasy luster and orange streak.
VanadatesNew MexicoSee treatment disclosure

Descloizite is vanadates, PbZn(VO4)(OH). In the hand, it rates 3 to 3.5 on the Mohs scale, and it runs brownish red and blackish brown. Very heavy brown-black to cherry crystal crusts and fern-like aggregates with greasy luster and orange streak, classic from Namibian vanadium mines.

Family
Vanadates
Mohs
3 to 3.5
System
Orthorhombic
Luster
Greasy to vitreous
Gravity
6.1 to 6.2
Light
Translucent to opaque
What it is

The geology.

Descloizite carries the formula PbZn(VO4)(OH). It belongs to the orthorhombic system. The trade files it under vanadates.

It sits at 3 to 3.5 on the Mohs scale. The surface reads greasy to vitreous. Light behaviour is translucent to opaque. Specific gravity runs 6.1 to 6.2. The streak is orange to brownish red. It breaks with no cleavage; uneven to conchoidal fracture.

Very heavy brown-black to cherry crystal crusts and fern-like aggregates with greasy luster and orange streak, classic from Namibian vanadium mines.

Common cuts are plumose and arborescent crystal groups, drusy crusts or stalactitic forms.

Where it comes from

The origins.

Oxidized lead-zinc-vanadium deposits: Berg Aukas and Abenab (Namibia, world classics), Arizona and New Mexico (USA), Mexico, Argentina.

On value, the database notes: collector mineral; lustrous Berg Aukas groups are sought after.

What people work with it for

Traditional associations.

In energy work traditions, associated with stamina and committing to practical goals.

Included for completeness. Tradition is worth knowing about, and it is worth keeping separate from the mineralogy.

What to look for

Spotting the real thing.

Very heavy brown-black to cherry crystal crusts and fern-like aggregates with greasy luster and orange streak, classic from Namibian vanadium mines.

Not faked; mislabeled mottramite is the usual mix-up.

Looks like How to tell them apart
Vanadinite Vanadinite forms bright orange-red hexagonal barrels; descloizite is darker plumose crusts
Mottramite Mottramite is the copper-dominant green sibling; descloizite runs brown-red (zinc-dominant)
Goethite crust Goethite streaks yellow-brown and is lighter (SG 4.3) than descloizite's 6+
Check it yourself

At-home tests.

These checks cost nothing. Daylight, a 10x loupe and a little patience are the whole kit for descloizite.

Test What you should see
By weight Remarkable heft (SG over 6)
By eye Orange-brown streak
Scratch check Soft, a copper coin scratches it

Anything that scratches, burns or dissolves the piece is a lab job. Get it appraised rather than testing it apart.

How to live with it

Care & handling.

At 3 to 3.5 on the Mohs scale this is a soft material. Keep it as a display piece, store it apart from harder stones, and skip daily-wear settings.

It breaks with no cleavage; uneven to conchoidal fracture, which is worth knowing before you set it or drop it.

Warm water and a soft cloth clean almost everything. Ultrasonic tanks, steamers and household cleaners are where pieces get ruined.

Safe handling

Contains lead and vanadium: wash hands after handling, keep away from children, no elixirs.

For the serious reader

A deeper look.

Extended detail on composition, sourcing, authentication and market value.

The physical record

The formula on record is PbZn(VO4)(OH). Crystal system: Orthorhombic. Specific gravity: 6.1 to 6.2. Streak: Orange to brownish red. Cleavage and fracture: No cleavage; uneven to conchoidal fracture.

How it reaches the market

Oxidized lead-zinc-vanadium deposits: Berg Aukas and Abenab (Namibia, world classics), Arizona and New Mexico (USA), Mexico, Argentina.

What it gets confused with

Vanadinite: Vanadinite forms bright orange-red hexagonal barrels; descloizite is darker plumose crusts. Mottramite: Mottramite is the copper-dominant green sibling; descloizite runs brown-red (zinc-dominant). Goethite crust: Goethite streaks yellow-brown and is lighter (SG 4.3) than descloizite's 6+.

What it is worth

Collector mineral; lustrous Berg Aukas groups are sought after.

Where buyers get caught

Not faked; mislabeled mottramite is the usual mix-up.

One more thing

Namibia's descloizite ores were once mined as a strategic vanadium source for hardening steel, leftover crystal pockets now feed the specimen market.

From the Beyond Bohemian library

An education-first guide.

No product links here. We do not sell descloizite, and a guide that only covers our own shelves would not be much of a guide.

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