
sedimentary
Red Jasper (River-worn)
Silicon Dioxide (SiO2) with Hematite inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Reddish-brown with dark inclusions; Luster: Dull to sub-vitreous; Crystal Structure: Microcrystalline; Cleavage: None/Conchoidal fracture; Opaque.
- Hardness
- 6
- Color
- Reddish-brown with dark inclusions
- Luster
- Dull to sub-vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown with dark inclusions; Luster: Dull to sub-vitreous; Crystal Structure: Microcrystalline; Cleavage: None/Conchoidal fracture; Opaque.
Formation & geological history
Formed when silica-rich fluids permeate through volcanic ash or sediment, often enriched with iron oxide (hematite) which provides the red color. This specific piece is a river-rounded cobble or pebble.
Uses & applications
Commonly used in lapidary work for cabochons, beads, and tumbled stones. Historically used for seals, talismans, and ornamental carvings.
Geological facts
Jasper is a dense variety of microcrystalline quartz. The name comes from the Greek word 'iaspis', meaning spotted stone. It is known for its extreme toughness due to its interlocking crystal structure.
Field identification & locations
Identify by its hardness (cannot be scratched by a steel knife) and its smooth, waxy texture when wet. Commonly found in riverbeds, gravel pits, and glacial till throughout North America, especially in the Great Lakes region and the Pacific Northwest.
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