Aluminite is a rare hydrous aluminum sulfate mineral, Al₂SO₄(OH)₄·7H₂O. It is soft, earthy, and typically forms as a secondary mineral in oxidized environments.
🌍 Origins and Naming
- Name Origin: From its aluminum content.
- Discovery: First described in 1807.
- Type Locality: Likely from England, where early specimens were studied.
🔬 Chemical and Structural Properties
- Formula: Al₂SO₄(OH)₄·7H₂O
- Mineral Group: Sulfates.
- Crystal System: Monoclinic (though crystals are extremely rare; usually earthy masses).
- Color: White, grayish, sometimes pale yellow.
- Habit: Earthy, clay-like masses; rarely fibrous or compact.
- Hardness: ~1.5–2 on Mohs scale (very soft).
- Specific Gravity: ~1.7–1.8 (light due to hydration).
- Luster: Dull to earthy.
- Streak: White.
⚙️ Geological Occurrence
- Forms as a secondary mineral in clay deposits, lignite beds, and oxidized sulfide veins.
- Associated Minerals: Gibbsite, alunogen, gypsum, halotrichite, and other hydrated sulfates.
- Localities:
- England (classic occurrences).
- Germany.
- USA (notably in coal-bearing regions).
📖 Scientific and Collector Significance
- Petrology: Illustrates hydration and alteration processes of aluminum-bearing sulfates.
- Collectors: Rarely aesthetic; valued academically for its rarity and paragenesis.
- Industrial Note: No commercial use; too soft and unstable.
✨ Conclusion
Aluminite is a soft, hydrous aluminum sulfate, usually forming earthy white masses in oxidized environments. It is scientifically interesting as a secondary mineral but remains a collector’s curiosity rather than an economic resource.
In short: Aluminite = Al₂SO₄(OH)₄·7H₂O, soft earthy sulfate, rare, first described in 1807.
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