M.J. Hibbard

Anglesite

Anglesite   PbSO₄   Orthorhombic
o Supergene (low-T aqueous, weathering) environment. (chapter 13)
- Galena (metallic gray) partially replaced by microcrystalline anglesite (dull gray to white, locally colloform) and associated "limonite". The Fe-oxyhydroxides are probably residual after pyrite. View width is 8 mm. Keck Museum/MSM

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