
mineral
Carnelian
Carnelian (Chalcedony / SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Orangish-red to brownish-red due to iron impurities; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Orangish-red to brownish-red due to iron impurities
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Orangish-red to brownish-red due to iron impurities; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.58-2.64
Formation & geological history
Formed in volcanic and sedimentary environments when silica-rich fluids permeate cavities in host rock. Its distinctive color is primarily caused by iron oxide (hematite) inclusions.
Uses & applications
Widely used for lapidary work, jewelry (beads, cabochons), carvings, and seals. Primarily valued by collectors and crystal healing enthusiasts.
Geological facts
Carnelian was used by the Romans to make signet rings because hot wax does not stick to it. It has been a significant gemstone since the Neolithic period.
Field identification & locations
Identifiable by its translucent to semi-opaque orange-red hue and waxy luster. Commonly found in Brazil, India, Uruguay, and Madagascar. In the field, look for conchoidal fractures and a smooth, waxy surface.
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