
mineral
Likely rough carnelian (orange-brown chalcedony)
Chalcedony, microcrystalline quartz (SiO₂); variety possibly carnelian
AI-generated identification · may be incorrectHardness 6.5–7 Mohs; reddish-brown with lighter mottling and a waxy to dull luster. Quartz has a trigonal crystal structure, but its microscopic crystals are too small to see; it typically has no cleavage and breaks with a curved, conchoidal fracture.
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Physical properties
Hardness 6.5–7 Mohs; reddish-brown with lighter mottling and a waxy to dull luster. Quartz has a trigonal crystal structure, but its microscopic crystals are too small to see; it typically has no cleavage and breaks with a curved, conchoidal fracture.
Formation & geological history
Forms when silica-rich fluids deposit microcrystalline quartz in cavities and fractures, often in volcanic rocks. The specimen’s age and exact origin cannot be determined from the image.
Uses & applications
Used for beads, cabochons, carvings, and other jewelry; rough pieces are also collected.
Geological facts
Carnelian is a traditional name for red to orange chalcedony, with color often caused by iron oxides.
Field identification & locations
The small opaque, waxy-looking reddish-brown piece is consistent with chalcedony, but visual identification alone is uncertain. Common sources include India, Brazil, Uruguay, and Madagascar; check for glassy conchoidal breaks and lack of visible grains.
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