
sedimentary
Chert (with Manganese Dendrites)
Chert (Cryptocrystalline Quartz, SiO2)
Hardness: 7 (Mohs); Color: White to grey with dark brown/black surface staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); SG: 2.65.
- Hardness
- 7 (Mohs)
- Color
- White to grey with dark brown/black surface staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs); Color: White to grey with dark brown/black surface staining; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); SG: 2.65.
Formation & geological history
Formed from the accumulation of silica-rich microfossils (like radiolarians or diatoms) or chemical precipitation of silica in ocean floor sediments. The dark patterns are manganese oxides that precipitated into cracks or onto the surface.
Uses & applications
Historically used for stone tools/arrowheads. Currently used as industrial abrasive, landscaping gravel, and as educational or decorative lapidary specimens.
Geological facts
This specimen shows manganese oxide staining which often creates 'dendrites'—branching tree-like patterns that are frequently mistaken for plant fossils. Chert is the parent material for jasper and flint.
Field identification & locations
Identify by its hardness (will scratch glass), conchoidal (shell-like) fracture, and smooth, waxy texture. Commonly found in riverbeds and coastal regions where ancient sedimentary layers have eroded.
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