
mineral
Carnelian (Carnelian Agate)
Cryptocrystalline Quartz (SiO2 with Hematite impurities)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Orange, reddish-brown, semi-translucent; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (trigonal microcrystalline); Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Orange, reddish-brown, semi-translucent
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Orange, reddish-brown, semi-translucent; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (trigonal microcrystalline); Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.58-2.64.
Formation & geological history
Formed within volcanic cavities or sedimentary rocks through the precipitation of silica from groundwater at low temperatures. The red-orange color comes from iron oxide (hematite) impurities. Often found as water-worn pebbles in stream beds.
Uses & applications
Used primarily for lapidary work, jewelry (beads, cabochons, signet rings), and as a collector's specimen. Historically used for seals and amulets.
Geological facts
Carnelian is one of the oldest gemstones used in jewelry, dating back to at least 4500 BC. Ancient Romans and Egyptians used it extensively for signet rings and decorative carvings because wax does not stick to it.
Field identification & locations
Identified by its distinctive waxy luster, orange-red translucency, and conchoidal fracture. The coordinates provided (near El Paso, TX) are in an area geologically rich in agates and chert, particularly in the Rio Grande gravels and volcanic formations of the Chihuahua Desert.
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