
sedimentary
Chert (Jasper/Agate variety)
Microcrystalline Quartz (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown, gray, and blue-green; Luster: Vitreous to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Reddish-brown, gray, and blue-green
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Reddish-brown, gray, and blue-green; Luster: Vitreous to waxy; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich fluids in limestone or volcanic rock cavities. Often occurs as nodules or replacement deposits. Geological age varies greatly from Precambrian to Cenozoic.
Uses & applications
Used historically for stone tools and weapons due to its sharp edges; modern uses include lapidary work, jewelry, and landscaping. High-quality specimens are popular among rockhounds.
Geological facts
This specimen shows transitions between opaque jasper and translucent chalcedony. Historically, chert was a primary material for making arrowheads and spear points because of its predictable fracturing patterns.
Field identification & locations
Identify by its 'shell-like' shell-like (conchoidal) fracture and its ability to scratch glass. Commonly found in stream beds, gravel pits, and sedimentary rock outcrops. Collectors should look for unique banding or color inclusions.
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