Alluaudite is a rare phosphate mineral, part of the triphylite–lithiophilite group, notable for its complex chemistry and occurrence in granitic pegmatites.
🌍 Origins and Naming
- Name Origin: Named after French naturalist François Alluaud (1778–1866).
- Discovery: First described in 1848.
- Type Locality: Skardu, Gilgit-Baltistan, Pakistan (though early descriptions also reference French localities).
🔬 Chemical and Structural Properties
- Formula: (Na,Ca)(Fe²⁺,Mn²⁺)₂(Fe³⁺,Mn³⁺)(PO₄)₃
- Mineral Group: Phosphates (alluaudite group).
- Crystal System: Monoclinic.
- Color: Black, brownish-black, sometimes greenish-black.
- Habit: Massive, granular; crystals are rare.
- Hardness: ~5–5.5 on Mohs scale.
- Specific Gravity: ~3.5–3.6.
- Luster: Submetallic to vitreous.
- Streak: Brownish-black.
⚙️ Geological Occurrence
- Found in granitic pegmatites and phosphate-rich environments.
- Associated Minerals: Triphylite, lithiophilite, vivianite, heterosite, and other phosphates.
- Localities:
- Skardu, Pakistan.
- Varuträsk, Sweden.
- Hagendorf, Germany.
- Other pegmatite localities worldwide.
📖 Scientific and Collector Significance
- Petrology: Important for understanding phosphate mineralization in pegmatites.
- Collectors: Rare, usually massive and dark-colored, valued for its rarity and association with classic pegmatite localities.
- Economic Note: No industrial use; mainly of academic and collector interest.
✨ Conclusion
Alluaudite is a complex phosphate mineral first described in the mid-19th century, found in pegmatites and phosphate-rich deposits. It is scientifically significant for illustrating phosphate mineral chemistry, though it remains a collector’s curiosity rather than an economic resource.
In short: Alluaudite = phosphate mineral, dark-colored, rare, first described in 1848, found in pegmatites.
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