
sedimentary
Yellow Jasper (Chert)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Yellowish-brown, ochre, mustard; Luster: Dull to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.6-2.9
- Hardness
- 6
- Color
- Yellowish-brown, ochre, mustard
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Yellowish-brown, ochre, mustard; Luster: Dull to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.6-2.9
Formation & geological history
Formed through the accumulation of silica-rich microfossils or chemical precipitation in sedimentary basins. The yellow color is typically due to iron (goethite or limonite) inclusions. Its geological age varies by location, often millions of years old.
Uses & applications
Used primarily in lapidary work for cabochons, beads, and ornemental carvings. Due to its hardness and density, it is also used in tumble polishing for aquarium decor.
Geological facts
Jasper is a microcrystalline variety of quartz. The name comes from the Greek word 'iaspis', meaning 'spotted stone'. In ancient times, it was considered a powerful protective stone.
Field identification & locations
Identify in the field by its hardness (cannot be scratched by a steel knife), conchoidal fracture (curved breaks), and smooth, waxy feel when wet. Found in riverbeds and mountainous regions globally.
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