
mineral
Amazonite in Quartz
K(AlSi3O8) - Potassium Feldspar with Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6-6.5 (Amazonite), 7 (Quartz). Color: Turquoise blue-green mixed with smoky-grey to white translucent quartz. Luster: Vitreous to pearly. Crystal Structure: Triclinic (Amazonite), Trigonal (Quartz). Cleavage: Perfect in two directions at nearly 90 degrees for amazonite.
- Hardness
- 6-6
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 (Amazonite), 7 (Quartz). Color: Turquoise blue-green mixed with smoky-grey to white translucent quartz. Luster: Vitreous to pearly. Crystal Structure: Triclinic (Amazonite), Trigonal (Quartz). Cleavage: Perfect in two directions at nearly 90 degrees for amazonite.
Formation & geological history
Formed in granitic pegmatites and hydrothermal veins through late-stage magmatic crystallization. The distinctive blue-green color of Amazonite is caused by trace amounts of lead and water within the feldspar structure.
Uses & applications
Used primarily as lapidary material, decorative carvings, cabochons, wire-wrapping jewelry, and as educational/collection specimens.
Geological facts
Amazonite is named after the Amazon River, though no deposits exist there. It is a green-blue variety of microcline feldspar often associated with smoky quartz in famous pegmatite regions like Pikes Peak, Colorado.
Field identification & locations
Identified by its distinctive robin-egg blue to teal color paired with translucent quartz matrix. Commonly found in pegmatite deposits worldwide including Brazil, Madagascar, Russia, and Colorado, USA. Collectors value contrast between the blue amazonite and dark quartz.
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