Rock Identifier
Red Carnelian (Tumbled) (SiO2 (Silicon Dioxide) - variety of Chalcedony) — mineral
mineral

Red Carnelian (Tumbled)

SiO2 (Silicon Dioxide) - variety of Chalcedony

Hardness: 6.5-7 (Mohs); Color: Red to brownish-red; Luster: Vitreous to waxy; Structure: Cryptocrystalline; Transparency: Translucent to opaque; Specific Gravity: 2.58-2.64

Hardness
6
Color
Red to brownish-red
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 6.5-7 (Mohs); Color: Red to brownish-red; Luster: Vitreous to waxy; Structure: Cryptocrystalline; Transparency: Translucent to opaque; Specific Gravity: 2.58-2.64

Formation & geological history

Formed in volcanic and sedimentary environments through the deposition of silica from groundwater in rock cavities. The red color is caused by iron oxide impurities. Found in Precambrian to Cenozoic formations.

Uses & applications

Commonly used in jewelry (beads, cabochons, seals), decorative carvings, and as a popular tumbled stone for collectors and spiritual uses.

Geological facts

Ancient Egyptians called it the 'setting sun' and used it for amulets; it was also used in Roman signet rings because hot wax does not stick to it.

Field identification & locations

Identified by its waxy luster, lack of visible crystals, and warm translucent red color. Found globally with major deposits in India, Brazil, and Uruguay. Look for even coloration in tumbled pieces.