Alumogel is not a formally recognized mineral species but rather an obsolete name applied to ill‑defined, gel‑like hydrous aluminum oxides. It is best thought of as a transitional or amorphous phase related to minerals like allophane and aluminite.
🌍 Origins and Naming
- Name Origin: From alum (aluminum) + gel, describing its soft, gelatinous appearance.
- Status: Not approved by the International Mineralogical Association (IMA).
- Historical Context: Used in older literature to describe fine-grained, hydrated aluminum oxides found in bauxite deposits and oxidation zones.
🔬 Chemical and Structural Properties
- Composition: Hydrous aluminum oxides, poorly defined.
- Structure: Amorphous or gel-like; lacks long-range crystallinity.
- Appearance: White to pale earthy masses, often resembling clays or gels.
- Associations: Frequently occurs with aluminite (Al₂SO₄(OH)₄·7H₂O) and allophane (Al₂O₃·(SiO₂)₁.₃–₂·2.5–3H₂O).
⚙️ Geological Occurrence
- Found in bauxite deposits and oxidized ore zones, where aluminum-bearing minerals undergo hydration and alteration.
- Localities: Reported from Zlaté Hory, Jeseník District, Olomouc Region, Czech Republic.
- Formation: Secondary product of weathering and alteration of aluminum-rich rocks.
📖 Scientific and Collector Significance
- Petrology: Illustrates transitional phases between crystalline aluminum hydroxides (like gibbsite) and amorphous aluminosilicates (like allophane).
- Collectors: Rarely collected; specimens are usually unattractive earthy masses.
- Modern Status: Considered a non-species or descriptive term rather than a valid mineral.
✨ Conclusion
Alumogel is an obsolete descriptive name for gel-like hydrous aluminum oxides, typically found in bauxite or oxidized deposits. It is scientifically interesting as a transitional phase but has no standing as a distinct mineral species today.
In short: Alumogel = obsolete name, gel-like hydrous aluminum oxides, related to allophane and aluminite, found in bauxite deposits.
Sources:
You can explore more details on Mindat’s alumogel entry.
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