Carnelian (Red Chalcedony)
Silicon Dioxide (SiO2) with iron oxide impurities
Rock Type: mineral

Physical Properties
Hardness: 6.5-7 (Mohs); Color: translucent orange to reddish-brown; Luster: waxy to vitreous; Crystal structure: Trigonal (cryptocrystalline); Cleavage: none; Specific gravity: 2.58–2.64
Formation & Geological History
Formed in low-temperature hydrothermal environments where silica-rich fluids permeate cavities in volcanic rocks. The color comes from iron oxide (hematite) impurities.
Uses & Applications
Used primarily in jewelry (cabochons, beads), decorative carvings, and seal stones. Highly valued in lapidary arts and as a collector's gemstone.
Geological Facts
Carnelian was famously used in Ancient Egypt for amulets and scarabs, and it was used in Roman seal rings because hot wax does not stick to it.
Field Identification & Locations
Identified by its waxy luster and translucent orange-red glow when held to a light source. Found globally in Brazil, India, Madagascar, and Uruguay.
Identified on: 4/18/2026
Mode: Standard