![Green Apatite on Albite (Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]) — mineral](https://media.rockidentification.com/724eea15-790f-45d8-a8c6-a343d5fb3f53-compressed.jpg)
mineral
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
Hardness: 5 (Apatite) and 6 (Albite); Color: Sea-green to olive greenish crystals on white/tan matrix; Luster: Vitreous to sub-resinous; Crystal Structure: Hexagonal prisms (Apatite) on triclinic blades (Albite); Cleavage: Poor; Specific Gravity: 3.1-3.2 (Apatite).
- Hardness
- 5 (Apatite) and 6 (Albite)
- Color
- Sea-green to olive greenish crystals on white/tan matrix
- Luster
- Vitreous to sub-resinous
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Physical properties
Hardness: 5 (Apatite) and 6 (Albite); Color: Sea-green to olive greenish crystals on white/tan matrix; Luster: Vitreous to sub-resinous; Crystal Structure: Hexagonal prisms (Apatite) on triclinic blades (Albite); Cleavage: Poor; Specific Gravity: 3.1-3.2 (Apatite).
Formation & geological history
Formed in granitic pegmatites through late-stage hydrothermal processes. The apatite crystals grew upon a pre-existing matrix of bladed feldspar (cleavelandite variety of albite).
Uses & applications
Primary source of phosphorus for fertilizer in its massive form; however, crystallized specimens like this are highly valued for mineral collecting and display. Occasionally used as a gemstone, though soft.
Geological facts
Apatite is the mineral that defines index 5 on the Mohs scale of mineral hardness. It is the same material that makes up human tooth enamel and bone mineral.
Field identification & locations
Identify by the distinctive hexagonal prism shape of the green crystals and the bladed texture of the white albite. Commonly found in pegmatite districts of Brazil, Pakistan, and Maine (USA). Collectors should look for sharp crystal terminations and color clarity.
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