Rock Identifier
Carnelian (Chalcedony) (Silicon Dioxide (SiO2) with Iron Oxide impurities) — mineral
mineral

Carnelian (Chalcedony)

Silicon Dioxide (SiO2) with Iron Oxide impurities

Hardness: 6.5-7 (Mohs scale); Color: Translucent orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Hexagonal (microcrystalline); Cleavage: None; Fracture: Conchoidal.

Hardness
6
Color
Translucent orange to reddish-brown
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Translucent orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Hexagonal (microcrystalline); Cleavage: None; Fracture: Conchoidal.

Formation & geological history

Forms in pockets of volcanic rock, where silica-rich groundwater deposits minerals over time. Its color is derived from iron oxide (hematite) impurities. Often found as water-worn pebbles in stream beds.

Uses & applications

Used primarily in lapidary work, jewelry (beads, cabochons), and as a collector's stone. Historically used for signet rings and wax seals because hot wax does not stick to it.

Geological facts

Carnelian was revered by ancient Egyptians as the 'setting sun' and was mentioned as a protective stone for the heart. It is one of the oldest gemstones recorded in history, dating back to the Neolithic period.

Field identification & locations

Identify by its translucent, waxy appearance and orange color range. Found commonly in Brazil, India, Uruguay, and Madagascar. In the field, look for smooth, rounded pebbles that appear glowing or translucent when held to the light.