
sedimentary
Yellow Jasper with Red Inclusion
Silicon Dioxide (SiO2) with Iron Oxides
Hardness: 6.5-7 on Mohs scale; Color: mustard yellow with brownish-red spots/mottling; Luster: waxy to vitreous when polished; Crystal Structure: microcrystalline trigonal; Cleavage: none; Fracture: conchoidal; Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- mustard yellow with brownish-red spots/mottling
- Luster
- waxy to vitreous when polished
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: mustard yellow with brownish-red spots/mottling; Luster: waxy to vitreous when polished; Crystal Structure: microcrystalline trigonal; Cleavage: none; Fracture: conchoidal; Specific Gravity: 2.58-2.91.
Formation & geological history
Formed when silica-rich waters precipitate microcrystalline quartz along with iron oxides and clay impurities in sedimentary or volcanic environments over millions of years, leading to a opaque, colorful chalcedony rock.
Uses & applications
Used primarily as lapidary material, tumbled stones, pocket stones, beads, carved cabochons, and decorative items.
Geological facts
Yellow jasper owes its bright mustard color to goethite or iron oxide inclusion, while red mottling is usually due to hematite. Native American cultures and ancient Egyptians used jasper for amulets, seals, and tools.
Field identification & locations
Identify by its hardness (scratches glass), waxy luster, opacity, smooth tumbled surface, and characteristic mottling of yellow and reddish-brown. Common in riverbeds, desert pavements, and gravel deposits worldwide.
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