
sedimentary
Red Jasper (with Chert/Quartz)
Silicon Dioxide (SiO2)
Hardness: 6.5-7 (Mohs scale); Color: Brick red to brownish-orange; Luster: Dull to Vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to brownish-orange
- Luster
- Dull to Vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brick red to brownish-orange; Luster: Dull to Vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed when silica-rich fluids permeate sedimentary or volcanic rocks. The red color is caused by the inclusion of iron oxides (hematite) during the crystallization process. Found in hydrothermal veins and as nodules in sedimentary layers.
Uses & applications
Used extensively as a gemstone, for decorative carvings, lapidary work, and historically as an architectural stone. It is also a popular collector's specimen.
Geological facts
Red jasper has been used since antiquity; it was known as the 'stone of endurance' in many cultures. It is a variety of chalcedony that contains up to 20% foreign materials which account for its color and opacity.
Field identification & locations
Identify in the field by its waxy to dull luster, smooth conchoidal (shell-like) fractures, and its ability to scratch glass. Commonly found in riverbeds or desert regions of India, Brazil, and the Southwestern United States.
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