
sedimentary
Jasper
Jasper (Silica/Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Multicolored with red, tan, and creamy white bands; Luster: Vitreous to waxy; Crystal structure: Microcrystalline (Trigonal); Cleavage: None (Conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Multicolored with red, tan, and creamy white bands
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Multicolored with red, tan, and creamy white bands; Luster: Vitreous to waxy; Crystal structure: Microcrystalline (Trigonal); Cleavage: None (Conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica in sedimentary environments or hydrothermal veins. This specimen shows a tumbled or polished surface, often found in ancient riverbeds or volcanic ash deposits where silica-rich fluids permeate porous rock.
Uses & applications
Commonly used in jewelry for cabochons and beads, as well as decorative items, ornaments, and pocket stones for collectors.
Geological facts
Jasper is an opaque variety of chalcedony. The red coloration seen in this specimen is typically caused by iron inclusions. It has been used since antiquity for seals, amulets, and architectural ornamentation.
Field identification & locations
Identify in the field by its opacity (unlike translucent agate), high hardness (cannot be scratched by a steel nail), and smooth, waxy feel when polished. Widely found in the Western United States, Brazil, and India.
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