
sedimentary
Breciated Jasper
Brecciated Jasper (Silicon Dioxide, SiO2)
Hardness: 6.5-7 Mohs; Color: Brick red with white or cream inclusions; Luster: Vitreous to dull; Crystal Structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red with white or cream inclusions
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brick red with white or cream inclusions; Luster: Vitreous to dull; Crystal Structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through a process of fragmentation and re-cementation. Original jasper beds are shattered by tectonic activity and then filled in or 'glued' back together by subsequent infusions of silica (quartz or chalcedony) or hematite.
Uses & applications
Primary uses are in jewelry making (cabochons, beads), decorative ornaments, and lapidary arts. It is also popular in the metaphysical community as a grounding stone.
Geological facts
The word 'brecciated' comes from the Italian word 'breccia', meaning 'broken stones'. The red color is typically caused by high iron oxide (hematite) content within the stone.
Field identification & locations
Identifiable by its 'broken' appearance where angular fragments of red jasper are held together by a lighter-colored matrix. Commonly found in desert environments or areas with ancient tectonic activity. Collectors should look for sharp color contrast between the clasts and the matrix.
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