
sedimentary
Likely weathered chert or flint nodule
Microcrystalline quartz (SiO₂), possibly chalcedony-rich chert
AI-generated identification · may be incorrectDark gray to brown, dull-to-waxy luster, rounded nodule with a lighter weathering rind and pale speckles. Hardness about 7 Mohs; conchoidal fracture; no obvious cleavage; specific gravity roughly 2.6.
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Physical properties
Dark gray to brown, dull-to-waxy luster, rounded nodule with a lighter weathering rind and pale speckles. Hardness about 7 Mohs; conchoidal fracture; no obvious cleavage; specific gravity roughly 2.6.
Formation & geological history
Chert forms when silica replaces or fills pores in sedimentary rocks, commonly limestone or chalk, during diagenesis. The rounded shape suggests erosion and transport; its exact geological age cannot be determined from the photograph.
Uses & applications
Used historically for sharp tools and fire-starting, and occasionally as decorative or lapidary material. Ordinary nodules generally have little commercial value.
Geological facts
The dark interior and lighter rind are typical of flint/chert weathering. A fresh break should be curved and glassy rather than granular.
Field identification & locations
Consistent with sedimentary terrains around the lower Volga region near 48.5°N, 44.5°E, where transported chert and flint nodules can occur. Test carefully with a steel file or glass: genuine chert should scratch ordinary glass; avoid striking unknown specimens because sharp flakes can form.
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