
mineral
Carnelian
Carnelian (a variety of Chalcedony, SiO2) colored by iron oxide
Hardness: 6.5-7 (Mohs scale); Color: Orange, reddish-brown, brownish-red; Luster: Waxy to Vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Orange, reddish-brown, brownish-red
- Luster
- Waxy to Vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Orange, reddish-brown, brownish-red; 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 or sedimentary rocks. The orange hue comes from hematite impurities. It can found in volcanic lavas and as water-worn pebbles in riverbeds.
Uses & applications
Used primarily in jewelry-making (beads, cabochons), carvings, and ornamental lapidary work. Historically used for signet rings and cylinder seals because hot wax does not stick to it.
Geological facts
Carnelian was highly valued in Ancient Egypt, where it was believed to give spirits energy for the afterlife. In Islamic tradition, the Prophet Muhammad was said to have worn a carnelian seal ring.
Field identification & locations
Identify by its waxy luster, translucency, and warm orange heat. In the field, look for a 'glow' when held up to the light. Commonly found in Brazil, India, Uruguay, and along riverbanks/beaches in the Pacific Northwest of the USA.
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