Amazonite is a green variety of microcline feldspar (KAlSi₃O₈), prized both as a gemstone and for its striking color.
🌍 Origins and Naming
- Name Origin: Named after the Amazon River, though no deposits are actually found there. The name reflects its vivid green color reminiscent of tropical landscapes.
- Mineral Group: Feldspar (alkali feldspar, specifically microcline).
- Discovery: Known since antiquity; used in jewelry and ornamental objects.
🔬 Chemical and Structural Properties
- Formula: KAlSi₃O₈ (microcline feldspar).
- Crystal System: Triclinic.
- Color: Bright green to bluish-green, sometimes mottled with white.
- Cause of Color: Trace amounts of lead and water in the feldspar lattice, plus possible iron content.
- Habit: Blocky crystals, massive aggregates.
- Hardness: ~6–6.5 on Mohs scale.
- Specific Gravity: ~2.56–2.58.
- Cleavage: Perfect in two directions, typical of feldspars.
- Luster: Vitreous.
⚙️ Geological Occurrence
- Found in granitic pegmatites, often associated with quartz, albite, and smoky quartz.
- Localities:
- Colorado, USA (classic locality, especially Pikes Peak region).
- Brazil.
- Madagascar.
- Russia (Ural Mountains).
- Namibia.
📖 Scientific and Collector Significance
- Gemstone Use: Cut into cabochons, beads, and ornamental carvings. Rarely faceted due to cleavage.
- Collectors: Valued for its vivid green color and association with pegmatite minerals.
- Industrial Note: No major industrial use; significance lies in gemology and mineral collecting.
✨ Conclusion
Amazonite is a green variety of microcline feldspar, treasured for its vivid color and ornamental use. Found in pegmatites worldwide, it bridges mineralogical interest and gemstone appeal.
In short: Amazonite = green microcline feldspar, triclinic, gemstone from pegmatites, famous in Colorado and worldwide.
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