
Flint/chert projectile point
Microcrystalline quartz (SiO₂), archaeologically worked into a bifacial point
AI-generated identification · may be incorrectVery fine-grained, dark brown to black, waxy-to-dull luster; Mohs hardness about 7, conchoidal fracture, no visible cleavage, and typically composed of chalcedony/quartz with minor iron-oxide staining. The flaked edges and symmetrical triangular form indicate deliberate knapping rather than a natural crystal.
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