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Galenobismutite
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Galenobismutite

PbBi2S4
Orthorhombic IMA grandfathered

Galenobismutite is a sulfosalt mineral composed of lead, bismuth, and sulfur, with the chemical formula PbBi2S4. It crystallizes in the orthorhombic system and is classified within the sulfosalt group of minerals. This mineral is typically metallic in luster and exhibits a lead-gray to steel-gray color. It has a hardness of approximately 2.5 to 3 on the Mohs scale and a relatively high density. Galenobismutite is often found in association with other sulfide minerals and is of interest for its composition and crystal structure.

Composition

Composizione (% in peso)
Bi
Pb
S
  • BiBismuth55.5%
  • PbLead27.5%
  • SSulfur17.0%

Overview

Galenobismutite is a sulfosalt mineral composed of lead, bismuth, and sulfur, with the chemical formula PbBi2S4. It crystallizes in the orthorhombic system and is classified within the sulfosalt group of minerals. This mineral is typically metallic in luster and exhibits a lead-gray to steel-gray color. It has a hardness of approximately 2.5 to 3 on the Mohs scale and a relatively high density. Galenobismutite is often found in association with other sulfide minerals and is of interest for its composition and crystal structure.

Etymology

Galenobismutite is named after bismuth, reflecting its significant bismuth content. The mineral's name also alludes to its relation to galena, a lead sulfide, due to its lead content.

How to recognize it

Galenobismutite can be identified by its metallic luster, lead-gray to steel-gray color, and relatively low hardness of 2.5 to 3 on the Mohs scale. It has a high density and does not exhibit a distinct streak. Due to its softness and metallic appearance, it can be confused with other lead- or bismuth-bearing sulfides, but its chemical composition and crystal system help distinguish it.

Frequently asked questions

Galenobismutite is considered a rare mineral, typically found in limited localities where lead and bismuth-rich hydrothermal conditions exist.