Rock Identifier
Flint/chert projectile point (Microcrystalline quartz (SiO₂), archaeologically worked into a bifacial point) — sedimentary
sedimentary

Flint/chert projectile point

Microcrystalline quartz (SiO₂), archaeologically worked into a bifacial point

AI-generated identification · may be incorrect

Very 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.

Identified More sedimentary
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Physical properties

Very 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.

Formation & geological history

Chert formed when silica-rich groundwater replaced or precipitated within sedimentary deposits, commonly limestone, during diagenesis; its exact geological age cannot be determined from the photograph. The specimen was later shaped by prehistoric flintknapping, likely as a projectile or spear point.

Uses & applications

Historically used as a cutting tool, arrowhead, or spear point; today it is primarily an archaeological artifact or collector’s object rather than an industrial stone.

Geological facts

Step-like flake scars, a pointed tip, notched/contracting base, and edge retouch are characteristic of a bifacially worked point. Cultural age and authenticity require archaeological context and expert examination.

Field identification & locations

Common source materials include Texas, Oklahoma, the Great Lakes, and many regions worldwide. Avoid acid and abrasion; provenance is essential, and unauthorized collecting of artifacts may be illegal.