
mineral
Red Jasper
Silicon dioxide (SiO2)
Hardness: 6.5-7 (Mohs); Color: Red, often with streaks of brown or gray; Luster: Dull to vitreous; Crystal Structure: Microcrystalline quartz (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Red, often with streaks of brown or gray
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Red, often with streaks of brown or gray; Luster: Dull to vitreous; Crystal Structure: Microcrystalline quartz (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Forms in hydrothermal veins or as a secondary mineral in volcanic rocks. The red color is caused by iron (hematite) inclusions within the silica matrix. Generally found in Precambrian to Tertiary formations.
Uses & applications
Used primarily in lapidary work for cabochons, beads, and stone carvings. Also used as decorative stone in mosaics and as an ornamental gemstone in jewelry.
Geological facts
Jasper is an opaque variety of chalcedony. It has been used for centuries by ancient civilizations for seals, talismans, and as the 'blood of Mother Earth' in indigenous cultures.
Field identification & locations
Identify in the field by its hardness (cannot be scratched by a steel knife), opaque red appearance, and smooth, water-worn texture if found in riverbeds. Common in the Western USA, Brazil, South Africa, and India.
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