Rock Identifier
Translucent yellow-green chalcedony, possibly common opal (Microcrystalline quartz (SiO₂), potentially mixed with opaline silica (SiO₂·nH₂O)) — mineral
mineral

Translucent yellow-green chalcedony, possibly common opal

Microcrystalline quartz (SiO₂), potentially mixed with opaline silica (SiO₂·nH₂O)

AI-generated identification · may be incorrect

Waxy to vitreous luster, pale yellow-green color, translucent edges, and cloudy orbicular/veined internal texture; quartz hardness is about 7 Mohs, while opal is about 5.5–6.5. The strong blue glow is likely ultraviolet fluorescence from included minerals or a UV-reactive coating, not inherent blue coloration.

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Physical properties

Waxy to vitreous luster, pale yellow-green color, translucent edges, and cloudy orbicular/veined internal texture; quartz hardness is about 7 Mohs, while opal is about 5.5–6.5. The strong blue glow is likely ultraviolet fluorescence from included minerals or a UV-reactive coating, not inherent blue coloration.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures, precipitating chalcedony or opal in volcanic rocks and sediments; ages range from recent to millions of years. Exact identification requires daylight inspection, UV wavelength testing, and hardness or specific-gravity tests.

Uses & applications

Used as a lapidary stone for cabochons, carvings, and decorative specimens; attractive translucent material may have modest gemstone appeal.

Geological facts

The visible pattern resembles orbicular chalcedony or “flower agate,” though the yellow-green coloration may reflect iron-bearing inclusions, dye, or treatment.

Field identification & locations

Common sources include Brazil, Madagascar, Mexico, Turkey, and the western United States. Check for conchoidal fracture, lack of cleavage, uniformity of color, and whether fluorescence persists after washing; avoid scratching until treatment is known.