Anglesite

PbSO4

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

Elemental Composition (by mass)
ElementMass %Visual
Pb Lead68.33%
O Oxygen21.10%
S Sulfur10.57%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
Pseudomorph Relationships
Replaces — this mineral is often a pseudomorph after:
Galena replacement
Anglesite (PbSO₄) coats galena in sulfate-rich environments.
Cornwall; Italy.
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.
Mohs 2.5–3
Vickers (~) 170 HV
Knoop (~) 185 HK
Element composition by mass

Formula: PbSO₄ · molar mass: 303.26 g/mol

Pb 68.33%
O 21.1%
S 10.57%

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

Mohs Hardness 2.5–3
1
Talc
2
Gypsum
3
Calcite
4
Fluorite
5
Apatite
6
Orthoclase
7
Quartz
8
Topaz
9
Corundum
10
Diamond

Anglesite sits at 2.5–3 on the Mohs scale — can be scratched by a steel knife.

Colors:
Streak
White
Crystal system
Orthorhombic
SulfatesSulfates
TL;DR · 1 min read
Anglesite (PbSO₄) is the secondary lead sulfate of the oxidized cap zones of galena-bearing Pb-Zn deposits. Named after Anglesey (Wales) where it was first described, Anglesite is famous for adamantine transparent crystals from Touissit (Morocco), Tsumeb (Namibia), and Sardinia.

Anglesite (PbSO₄) is the secondary lead sulfate of the oxidized cap zones of galena-bearing Pb-Zn deposits. Named after Anglesey (Wales) where it was first described, Anglesite is famous for adamantine transparent crystals from Touissit (Morocco), Tsumeb (Namibia), and Sardinia. It forms by oxidation of galena, often as paramorphic pseudomorphs preserving galena cube outlines.

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