
mineral
Carnelian Agate/Jasper blend
Silicon Dioxide (SiO2) - variety of Chalcedony
Hardness: 6.5–7 on Mohs scale; Color: Reddish-brown to orange; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Reddish-brown to orange
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Reddish-brown to orange; 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 in igneous rocks (usually volcanic) or sedimentary formations. The reddish tint is caused by iron oxide (hematite) impurities. These specimens can range in age from millions to hundreds of millions of years old.
Uses & applications
Commonly used in lapidary work for making cabochons, beads, and carvings. It is also used in the jewelry industry as a semi-precious gemstone and by crystal collectors for its aesthetic and alleged metaphysical properties.
Geological facts
Carnelian was highly prized in ancient times; it was used by the Romans to make seal rings and by ancient Egyptians as a symbol of life. It is often heat-treated to enhance its red color.
Field identification & locations
Identify in the field by its distinct waxy luster, conchoidal (shell-like) fracture, and translucent to opaque orange-red banding. Commonly found in Brazil, India, Madagascar, and the United States (specifically the Pacific Northwest). Look for smooth, water-worn nodules in riverbeds or gravel pits.
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