Rock Identifier
Yellow Jasper (Silicon Dioxide (SiO2) with iron oxide inclusions) — sedimentary
sedimentary

Yellow Jasper

Silicon Dioxide (SiO2) with iron oxide inclusions

Hardness: 6.5-7 (Mohs); Color: Yellow to brownish-yellow; Luster: Vitreous to waxy; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91

Hardness
6
Color
Yellow to brownish-yellow
Luster
Vitreous to waxy
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs); Color: Yellow to brownish-yellow; Luster: Vitreous to waxy; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91

Formation & geological history

Formed through the deposition of silica from water-rich solutions into volcanic ash or sedimentary rocks. The yellow coloration is caused by the presence of goethite or other iron hydroxide minerals. It can form in any age range from Precambrian to recent.

Uses & applications

Primarily used for lapidary work, jewelry (cabochons and beads), ornamental carvings, and as a collector's specimen. It is also historically used for physical and spiritual protection in various cultures.

Geological facts

Jasper is an opaque variety of chalcedony. Yellow jasper specifically was historically revered by ancient civilizations as a stone of endurance and perseverance. Some specimens are so dense they can take a mirror-like polish.

Field identification & locations

Identify in the field by its waxy appearance, extreme hardness (it will scratch glass), and its lack of transparency even on thin edges. It is commonly found in desert regions, riverbeds, and volcanic outflows throughout the American West and Madagascar.