Applying dilute acid to see if a mineral fizzes (effervesces), indicating carbonate content; commonly used to distinguish calcite and other carbonates from look‑alikes.
A star-shaped light pattern (often 4 or 6 rays) produced by oriented inclusions; typically visible on cabochon-cut stones and used as a descriptive/valuing feature.
Double refraction where light splits into two rays, sometimes producing doubled edges through transparent crystals; an optical clue tied to crystal structure.
A moving ‘cat’s‑eye’ band of light caused by aligned fibers or needle-like inclusions; commonly seen on cabochons and used to describe gemstone appearance.
A mineral’s tendency to break along flat, repeating planes controlled by its crystal structure; used to recognize species and predict how a specimen will split.
Bands or patches of different color within one crystal caused by changing growth conditions or chemistry; reveals growth history and can affect appearance and value.
A visible glow under UV light (longwave/shortwave) caused by trace activators in the mineral; useful for identification and for evaluating fluorescent specimens.
Internal crystals, fluids, fractures, or growth features trapped inside a mineral; used to interpret formation conditions and to judge clarity, stability, and aesthetics.
How a mineral reflects light from its surface (metallic, vitreous, pearly, etc.), a quick visual property collectors use to narrow identification and describe specimens.
A check for attraction to a magnet (or effect on a compass), which quickly flags strongly magnetic minerals like magnetite and some weakly magnetic species.
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