
sedimentary
Yellow Jasper
Silicon Dioxide (SiO2) with Goethite or Iron Hydroxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Yellow to mustard/mustard brown; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Yellow to mustard/mustard brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Yellow to mustard/mustard brown; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or sedimentary beds. The yellow color results from ferric iron (goethite) impurities during the mineralization process. It is found in rocks of various ages, commonly ranging from Precambrian to Cenozoic.
Uses & applications
Used primarily as decorative gemstones, lapidary cabochons, and in jewelry. Historically used for making tools and weapons due to its sharp conchoidal fracture.
Geological facts
Jasper is an opaque variety of chalcedony. The name 'jasper' is derived from the Greek word 'iaspis', meaning 'spotted stone'. In ancient times, it was considered a stone of protection and endurance.
Field identification & locations
Identify in the field by its distinctive waxy appearance, extreme hardness (it will scratch glass), and shell-like (conchoidal) fracture pattern. Common locations include South Africa, India, Brazil, and the Western United States.
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