
sedimentary
Chert (Jasper)
Cryptocrystalline Quartz (SiO2)
Hardness: 7 Mohs scale; Color: Reddish-brown, tan, and gray; Luster: Dull to waxy; Texture: Fine-grained, microcrystalline; Breakage: Conchoidal fracture with sharp edges; Opacity: Opaque.
- Hardness
- 7 Mohs scale
- Color
- Reddish-brown, tan, and gray
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 Mohs scale; Color: Reddish-brown, tan, and gray; Luster: Dull to waxy; Texture: Fine-grained, microcrystalline; Breakage: Conchoidal fracture with sharp edges; Opacity: Opaque.
Formation & geological history
Formed primarily through the accumulation of silica-rich organic remains (like radiolaria or diatoms) or by chemical precipitation from brine in sedimentary basins. This specimen likely contains iron oxide inclusions giving it the reddish jasper-like hue.
Uses & applications
Historically used for making stone tools (arrowheads, scrapers) due to its sharp conchoidal fracture. Modern uses include decorative gravel, lapidary work (tumbled stones), and as a silica source in glassmaking.
Geological facts
Chert is so durable that it often survives as rounded pebbles in riverbeds long after surrounding limestone has eroded away. High-quality red chert is often referred specifically as Jasper in jewelry circles.
Field identification & locations
Identified in the field by its superior hardness (cannot be scratched by a steel knife) and its glass-like, curved fracture surfaces. Commonly found in limestone and dolomite formations or as loose nodules in stream beds.
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