
sedimentary
Red Jasper
Microcrystalline Quartz (Chalcedony), SiO2 with iron oxide inclusions
Hardness: 6.5 to 7 on the Mohs scale. Color: Brick red to brownish-red due to iron oxide impurities. Luster: Vitreous to dull. Crystal structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (exhibits conchoidal fracture). Specific gravity: 2.58 to 2.91.
- Hardness
- 6
- Color
- Brick red to brownish-red due to iron oxide impurities
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale. Color: Brick red to brownish-red due to iron oxide impurities. Luster: Vitreous to dull. Crystal structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (exhibits conchoidal fracture). Specific gravity: 2.58 to 2.91.
Formation & geological history
Formed through the deposition of silica-rich sediments in marine environments, often associated with banded iron formations, heavily permeated and colored by iron oxide particles during diagenesis.
Uses & applications
Used primarily in lapidary arts, ornamental carvings, cabochons, beads, and as a popular specimen for mineral collectors.
Geological facts
Jasper has been used since ancient times for talismans, seals, and jewelry. Red jasper specifically was valued by ancient Egyptians and Native Americans for its protective and grounding symbolism.
Field identification & locations
Can be identified in the field by its opaque reddish color, hardness that can scratch glass, and smooth conchoidal fracture. Found worldwide, with notable deposits in India, Russia, Brazil, and the USA.
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