
mineral
Carnelian (Chalcedony)
Silicon Dioxide (SiO2) with trace Iron Oxide
Hardness: 6.5-7.0 (Mohs); Color: Orange to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Orange to reddish-brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7.0 (Mohs); Color: Orange to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
Formation & geological history
Formed through the deposition of silica from groundwater into cavities of volcanic rocks (basalt/rhyolite) or sedimentary formations. Its red/orange tint is caused by iron impurities that oxidize during formation.
Uses & applications
Predominantly used as a gemstone in jewelry, for lapidary work (beads, cabochons), and in metaphysical or spiritual practices. Historically used for signet rings and seals.
Geological facts
Ancient Egyptians called carnelian "the setting sun" and believed it possessed powers to revitalize the soul. It is one of the oldest gemstones used by humans, with evidence of its use dating back to the Neolithic period.
Field identification & locations
Identify by its characteristic waxy luster and translucent orange hue. Look for it in riverbeds or volcanic regions. Collectors often seek pieces with deep, uniform red-orange saturation without distracting inclusions.
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Mineral/Rock
Banded Gneiss (River Rock/Pebble)
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mineral