
mineral
Yellow Jasper
SiO2 (Microcrystalline Quartz)
Hardness: 6.5-7 on Mohs scale; Color: Yellow, mustard, ochre-brown with darker veins or mottling; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Yellow, mustard, ochre-brown with darker veins or mottling
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Yellow, mustard, ochre-brown with darker veins or mottling; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed when silica-rich fluids deposit microcrystalline quartz along with iron oxides and hydroxides (such as goethite or limonite) that impart the yellow-brown color. Typically found in sedimentary beds, alluvial gravels, or volcanic rock cavities.
Uses & applications
Used extensively as a lapidary material for cabochons, beads, carvings, tumbled stones, and decorative landscaping pebbles.
Geological facts
Yellow Jasper gets its distinct earthy mustard tone primarily from inclusions of iron hydrate minerals. In antiquity, jasper was widely used for seal stones, amulets, and ornamental items.
Field identification & locations
Can be identified by its smooth, stream-rounded surface, waxy luster when wet or polished, and inability to be scratched by steel. Commonly found in riverbeds, lake shores, and gravel deposits worldwide.
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