Cerussite

Crystal system · Orthorhombic

Cerussite is a carbonate mineral prized by collectors for its exceptional color range, with several world-class Chinese localities.

About Cerussiteextended article

Elemental Composition (by mass)
ElementMass %Visual
Pb Lead77.54%
O Oxygen17.96%
C Carbon4.50%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Cer
→ Cerussite
Pb carbonate
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/sɪˈrʌsaɪt/
suh-RUS-site
Latin cerussa (white lead)
Lapidary & Faceting Recommendations
Recommended cut:
oval / cushion
Also seen:
cushion, pear
Typical yield:
20% of rough
High RI + dispersion give bright stones but too soft (Mohs 3.5) and brittle for jewelry.
⚠ Safety & Handling
toxicmoderate
Lead carbonate.
Handling: Same as galena.
Information provided in good faith. Consult local hazmat regulations for transport and disposal. Severely hazardous specimens may require special storage cabinets.
UV Fluorescence
SW (254 nm)
Yellow
moderate
LW (365 nm)
Yellow
weak
Pb carbonate; UV-active.
SW = shortwave (germicidal lamp). LW = longwave (blacklight). Response varies with locality, trace impurities, and treatment.
Pseudomorph Relationships
Replaces — this mineral is often a pseudomorph after:
Galena replacement
Common galena oxidation product — preserves cubic outline.
Mibladen, Morocco; Tsumeb.
A pseudomorph (Greek "false form") is a mineral with the external shape of another species — the chemistry has changed but the crystal habit is inherited.
Tenacity
Behavior:
brittle
Under stress:
Cleaves; cracks easily
Very brittle for a Pb carbonate.
Luster
adamantine
Diamond-like brilliance; high RI for a carbonate.
Diaphaneity (Transparency)
transparent-to-translucent
Adamantine luster; gem-grade transparent.
Type Locality
Tarnowitz — Poland
Described 1845 by Haidinger
Diagnostic Field Tests
HCl test→ Fizzes; white milky PbCl precipitate
Lead carbonate; high SG also confirms.
⚠ Use dilute HCl (~10%) only on inconspicuous spots; rinse promptly. Smell-tests should be brief and ventilated. Taste-test ONLY halite/sylvite — never lead, arsenic, or sulfur minerals.
Specific Gravity
6.50–6.57
g/cm³
very heavy
PbCO₃; characteristic high SG for a carbonate.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Streak Test
white / colorless
White streak; high SG ~6.5 confirms.
Streak = color of the powdered mineral. Drag specimen across unglazed white porcelain plate (Mohs 6.5). For minerals harder than the plate, crush a small flake into powder and observe color.
Twinning Laws
Cyclic / sixlingcontact
Pseudo-hexagonal star or wheel twin.
Market availability: Uncommon
Found at major shows and select dealers. Quality varies by locality.
Mohs 3–3.5
Vickers (~) 170 HV
Knoop (~) 185 HK
Nickel–Strunz 5.AB.15
Dana 14.01.03.04
Geological setting
Oxidation zone
Element composition by mass

Formula: PbCO₃ · molar mass: 267.21 g/mol

Pb 77.54%
O 17.96%
C 4.5%

Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.

Mohs Hardness 3–3.5

Cerussite sits at 3–3.5 on the Mohs scale — can be scratched by a steel knife.

Colors:
Streak
White
Crystal system
Orthorhombic
Type localityTsumeb, Namibia (modern best)
CarbonatesCarbonates
TL;DR · 1 min read
Cerussite (PbCO₃) is lead carbonate, the aragonite-group analog where Pb replaces Ca. It is the iconic secondary lead mineral of the oxidized cap zones of lead-zinc deposits, where it forms transparent adamantine-luster crystals with extraordinarily heavy specific gravity (6.

Cerussite (PbCO₃) is lead carbonate, the aragonite-group analog where Pb replaces Ca. It is the iconic secondary lead mineral of the oxidized cap zones of lead-zinc deposits, where it forms transparent adamantine-luster crystals with extraordinarily heavy specific gravity (6.5) for a transparent species. Tsumeb (Namibia) is the world standard, producing massive reticulated twin specimens, snowflake-pattern penetration twins, and gem-quality single crystals over 10 cm.

More minerals to explore

About Cerussite

Cerussite belongs to the carbonate class in the aragonite group and has the chemical formula PbCO3. It crystallizes in the orthorhombic system and is one of the most visually varied minerals in the collector market. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.

Identification & care

Crystals commonly develop as tabular, prismatic, bipyramidal; characteristic snowflake-like star-shaped pseudo-hexagonal twinned aggregates; also reticulated network twins. Its color range is broad, including colorless, white, gray, blue, or green, and colorless in transmitted light. The luster is adamantine, vitreous, resinous, pearly, dull, earthy, the streak is white, and specimens are typically transparent, translucent. The cleavage is distinct/good on {110} and {021}; traces on {010} and {012}. The fracture is conchoidal, which aids identification.

Collector context

How it forms

The geological setting for Cerussite is typically secondary mineral in oxidized zone of lead ore deposits; very common weathering product of galena; found with other lead secondaries in the 'iron hat' (gossan) of lead mines. It is commonly found in association with galena (parent mineral), anglesite, smithsonite, malachite, azurite, pyromorphite, wulfenite.

Classic Chinese localities

Documented Chinese occurrences are recorded at Jiama Cu-polymetallic deposit, Dexing Cu-Mo-Au ore field and Daoping Mine, among others.

Why collectors care

Cerussite is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.

What affects value

Value in Cerussite is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.

Naming history

The name Cerussite has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.