
sedimentary
Jasper
Jasper (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs scale); Color: Reddish-brown, tan, and earthy tones; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None; Fracture: Conchoidal; Specific gravity: 2.58–2.91
- Hardness
- 6
- Color
- Reddish-brown, tan, and earthy tones
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Reddish-brown, tan, and earthy tones; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None; Fracture: Conchoidal; Specific gravity: 2.58–2.91
Formation & geological history
Usually forms when fine particulate materials (often silica-rich) settle in volcanic ash or sedimentary environments. It is a variety of chalcedony that contains impurities such as iron oxides, which give it its distinctive earthy colors.
Uses & applications
Used primarily as a gemstone for jewelry (cabochons), ornamental stone, and in lapidary art. Historically used for making tools and seals.
Geological facts
Jasper has been used by ancient civilizations for thousands of years. It is mentioned in various historical texts and was often used in the seals of ancient Babylon and Egypt. Pieces are often uniquely patterned, earning nicknames like 'Picture Jasper'.
Field identification & locations
Identify in the field by its hardness (it can scratch glass), its opaque nature, and its smooth, waxy fracture surface. It is extremely common in desert environments and river beds in the Western United States and India.
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