
mineral
Green aventurine cabochon (probable)
Quartz, SiO₂, with green fuchsite or chlorite inclusions
AI-generated identification · may be incorrectPolished, domed cabochon with medium-to-dark green color and slight internal mottling; vitreous to waxy luster, no visible cleavage, Mohs hardness about 6.5–7, and specific gravity near 2.6–2.7. The rounded shape and polish indicate a cut geological material rather than a raw specimen.
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Physical properties
Polished, domed cabochon with medium-to-dark green color and slight internal mottling; vitreous to waxy luster, no visible cleavage, Mohs hardness about 6.5–7, and specific gravity near 2.6–2.7. The rounded shape and polish indicate a cut geological material rather than a raw specimen.
Formation & geological history
Aventurine forms when quartz-rich rock crystallizes with disseminated green mica (usually fuchsite) or chlorite, commonly in metamorphic environments. The image alone cannot establish a geological age or confirm the inclusion mineral.
Uses & applications
Used for inexpensive jewelry, carvings, ornaments, and metaphysical collectibles; cabochons are commonly set in pendants and rings.
Geological facts
Natural aventurine often shows subtle glitter (“aventurescence”) from reflective mica flakes, though this specimen appears relatively opaque and may also be dyed chalcedony or glass imitation.
Field identification & locations
Check for natural granular texture, tiny reflective mica flashes, and hardness sufficient to resist scratching with a steel blade; glass imitations may show bubbles, while dye can concentrate in fractures. Common sources include India, Brazil, Russia, and Tanzania.
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