
sedimentary
Jasper with Quartz Veining
Silicon Dioxide (SiO2) - Microcrystalline Quartz
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown with white/tan veins; Luster: Vitreous to waxy; Crystal structure: Trigonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Reddish-brown with white/tan veins
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown with white/tan veins; Luster: Vitreous to waxy; Crystal structure: Trigonal (Microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from water-rich fluids in volcanic or sedimentary environments. The veins represent secondary silica (Quartz) infilling fractures in the host rock. Geological age can range from Precambrian to Cenozoic.
Uses & applications
Used primarily for lapidary work, jewelry (cabochons), interior decoration, and as a popular specimen for rock hounds and collectors.
Geological facts
Jasper is an impure variety of silica, usually containing iron oxides which give it the red/brown color. The 'brecciated' or veined appearance occurs after the original rock fractures and is 'healed' by new mineral growth.
Field identification & locations
Identify in the field by its high hardness (it will scratch glass), smooth waxy feel when wet, and lack of visible grains. Commonly found in riverbeds, desert washes, and volcanic deposits in the Western United States and India.
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