
mineral
Brecciated Agate / Jasper
Silicon Dioxide (SiO2) with iron oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs. Luster: Waxy to vitreous. Color: Orange, reddish-brown, tan, cream, and grey mottling. Crystal structure: Trigonal (microcrystalline/cryptocrystalline quartz). Cleavage: None, exhibits conchoidal fracture.
- Hardness
- 6
- Color
- Orange, reddish-brown, tan, cream, and grey mottling
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs. Luster: Waxy to vitreous. Color: Orange, reddish-brown, tan, cream, and grey mottling. Crystal structure: Trigonal (microcrystalline/cryptocrystalline quartz). Cleavage: None, exhibits conchoidal fracture.
Formation & geological history
Formed when existing agate or jasper rock fractured due to tectonic activity or hydrothermal pressure, and was subsequently cemented together by secondary silica deposition, often enriched with iron oxides.
Uses & applications
Popular in jewelry making (cabochons, ring settings, beads), lapidary art, wire wrapping, and crystal collections.
Geological facts
Brecciation occurs when rocks are broken into angular fragments and re-cemented. The striking angular pattern creates unique, one-of-a-kind patterns in each tumbled stone.
Field identification & locations
Identified by its distinctive angular fragments (clasts) cemented in a finer silica matrix. Common in volcanic regions and ancient sedimentary beds, such as in the Western US, Brazil, and Madagascar.
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