
mineral
Carnelian (Tumbled)
Carnelian (SiO2 with Iron Oxide impurities)
Hardness: 6.5-7 Mohs; Color: Orange, reddish-brown, pinkish-orange; Luster: Waxy to vitreous; Crystal system: Trigonal (microcrystalline); Cleavage: None; Fracture: Conchoidal; Translucent to semi-opaque.
- Hardness
- 6
- Color
- Orange, reddish-brown, pinkish-orange
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Orange, reddish-brown, pinkish-orange; Luster: Waxy to vitreous; Crystal system: Trigonal (microcrystalline); Cleavage: None; Fracture: Conchoidal; Translucent to semi-opaque.
Formation & geological history
Formed in volcanic and sedimentary environments through the deposition of silica from groundwater into cavities. Its orange color is caused by hematite (iron oxide) inclusions. Most specimens are from the Recent to Mesozoic eras.
Uses & applications
Extensively used in jewelry making (beads, cabochons), lapidary arts, decorative items, and historical artifacts such as signet rings and amulets.
Geological facts
Carnelian was used widely in ancient Rome and Egypt for seals and jewelry because hot wax does not stick to it. It has been a prized gemstone for over 4,500 years, found in the Royal Tombs of Ur.
Field identification & locations
Identify by its translucent waxy luster and consistent orange-red hue. Commonly found in Brazil, India, Uruguay, Madagascar, and the US. Collectors look for uniform color and lack of heavy inclusions.
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