
sedimentary
Jasper
Jasper (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs scale); Color: Yellow, orange, and brown (iron oxide inclusions); Luster: Vitreous to waxy; Crystal Structure: Microcrystalline trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91
- Hardness
- 6
- Color
- Yellow, orange, and brown (iron oxide inclusions)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Yellow, orange, and brown (iron oxide inclusions); Luster: Vitreous to waxy; Crystal Structure: Microcrystalline trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91
Formation & geological history
Formed from the deposition of silica from mineral-rich water or hydrothermal fluids, often replacing organic materials or volcanic ash. This yellow-brown variety is often called 'Yellow Jasper' or 'Ochre Jasper' and is found in various geological ages alongside quartz-rich formations.
Uses & applications
Used in lapidary arts for cabochons, beads, and ornamental stones; historically used for seals and decorative items; popular for stone tumbling and collection specimens.
Geological facts
Jasper is an opaque variety of chalcedony. Its patterns and colors are caused by up to 20% mineral inclusions, predominantly iron oxides like goethite or limonite in yellow specimens. Famous ancient seal stones were often carved from jasper due to its durability.
Field identification & locations
Identify in the field by its opacity (does not transmit light like agate), high hardness (cannot be scratched by a steel knife), and characteristic smooth, waxy surface when wet or polished. Often found in riverbeds or coastal deposits.
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