![Pyromorphite on Epidote (Pyromorphite [Pb5(PO4)3Cl] and Epidote [Ca2(Al2,Fe3+)(SiO4)3(OH)]) — mineral](https://media.rockidentification.com/50b83959-f538-4cd0-a7ea-ef2ac79d6ebc-compressed.jpg)
mineral
Pyromorphite on Epidote
Pyromorphite [Pb5(PO4)3Cl] and Epidote [Ca2(Al2,Fe3+)(SiO4)3(OH)]
Hardness: 3.5-4 (Pyromorphite), 6-7 (Epidote); Color: Olive to grass green; Luster: Resinious to adamantine; Structure: Hexagonal crystals; Cleavage: Subconchoidal; Specific Gravity: 6.5-7.1
- Hardness
- 3
- Color
- Olive to grass green
- Luster
- Resinious to adamantine
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Physical properties
Hardness: 3.5-4 (Pyromorphite), 6-7 (Epidote); Color: Olive to grass green; Luster: Resinious to adamantine; Structure: Hexagonal crystals; Cleavage: Subconchoidal; Specific Gravity: 6.5-7.1
Formation & geological history
Secondary mineral formed in the oxidation zones of lead ore deposits, often associated with phosphate-rich fluids. Commonly found in hydrothermal veins and metamorphic rocks.
Uses & applications
Primarily used as a minor lead ore and highly valued by mineral collectors for its vibrant color and crystal habits.
Geological facts
The name Pyromorphite comes from the Greek words for 'fire' and 'form' because the mineral turns back into its crystal shape after being melted. It is part of the apatite group.
Field identification & locations
Identified by high density, green color, and hexagonal crystal shapes. Key locations include China, Germany, and Idaho, USA. Collectors should look for luster and crystal definition.
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