
sedimentary
Flint (chert) hand axe
Cryptocrystalline silica (SiO₂), worked into a bifacial stone tool
AI-generated identification · may be incorrectThe dark gray, opaque specimen has sharp conchoidal edges and a matte-to-waxy luster; flint is about 7 on the Mohs scale and has no visible crystals or cleavage. The image appears to show a chipped, shaped artifact rather than an unworked rock.
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Physical properties
The dark gray, opaque specimen has sharp conchoidal edges and a matte-to-waxy luster; flint is about 7 on the Mohs scale and has no visible crystals or cleavage. The image appears to show a chipped, shaped artifact rather than an unworked rock.
Formation & geological history
Flint forms as silica-rich nodules in sedimentary rocks, commonly limestone or chalk. The tool’s age cannot be determined from the image; prehistoric examples were made by repeatedly striking flint to shape cutting edges.
Uses & applications
Flint was widely used for prehistoric cutting, scraping, and hunting tools; today it is mainly of archaeological and collector interest.
Geological facts
Flint’s conchoidal fracture produces exceptionally sharp edges. Stone tools are often dated and interpreted by their archaeological context, not appearance alone.
Field identification & locations
Look for a hard, fine-grained surface, curved impact scars, and deliberate flake-removal patterns. Flint occurs widely in sedimentary deposits, especially in Europe and parts of North America; provenance is essential for assessing an artifact.
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