
mineral
Green aventurine quartz point
Quartz, SiO₂, with green fuchsite inclusions (aventurescent quartz)
AI-generated identification · may be incorrectThe small, faceted green point appears opaque to translucent with a vitreous polish. Quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and specific gravity near 2.65; the photo does not establish its exact identity or treatments.
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Physical properties
The small, faceted green point appears opaque to translucent with a vitreous polish. Quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and specific gravity near 2.65; the photo does not establish its exact identity or treatments.
Formation & geological history
Aventurine forms when quartz crystallizes with reflective mineral inclusions, commonly fuchsite mica; it occurs in metamorphic settings and quartz veins. The specimen has been cut and polished, and its geological age cannot be determined from the image.
Uses & applications
Used for carvings, beads, jewelry, and decorative pieces; this appears shaped as a small point, sometimes sold for collecting or spiritual practices.
Geological facts
Aventurine’s characteristic shimmer, called aventurescence, comes from light reflecting off tiny platy inclusions; it is not clearly visible in this image.
Field identification & locations
Green color and a quartz-like glassy polish suggest aventurine, but dyed or other green minerals can look similar. Common sources include India, Brazil, and Russia; confirm with hardness and examination of inclusions.
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