
sedimentary
Banded Jasper / Yellow Jasper with Chlorite or Epidote inclusions
Silicon Dioxide (SiO2) with iron oxide and silicate impurities
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Mustard yellow, yellowish-brown, dark green to greenish-grey bands. Luster: Waxy to vitreous when polished. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline quartz). Cleavage: None (conchoidal fracture). Specific Gravity: ~2.6.
- Hardness
- 6
- Luster
- Waxy to vitreous when polished
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Mustard yellow, yellowish-brown, dark green to greenish-grey bands. Luster: Waxy to vitreous when polished. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline quartz). Cleavage: None (conchoidal fracture). Specific Gravity: ~2.6.
Formation & geological history
Formed through the deposition of silica-rich fluids in sedimentary or low-grade metamorphic environments, often with iron oxide minerals providing yellow hues and chlorite or epidote creating green banding.
Uses & applications
Polished tumbled stone used in lapidary arts, jewelry, cabochons, metaphysical collections, and ornamental carvings.
Geological facts
Jasper is an opaque variety of chalcedony. The name comes from the Greek word 'iaspis', meaning spotted stone.
Field identification & locations
Identify by its hardness (scratches steel), smooth waxy feel, opacity, and distinctive yellow and green banding. Commonly found in riverbeds, gravel deposits, and volcanic terrains worldwide (e.g., USA, Madagascar, India, Brazil).
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