Material · lithic

Rhyolite

North America — Eastern Woodlands, North America — Southeast

Rhyolite is a fine-grained volcanic rock used for tools across the Carolina Piedmont, where the Uwharrie Mountains quarries supplied Hardaway, Morrow Mountain and Savannah River points, and in the Northeast and Southwest. It weathers to a chalky rind. Most Piedmont points are in rhyolite.

Kindlithic
RegionsNorth America — Eastern Woodlands, North America — Southeast

Sources

The Carolina Slate Belt of North Carolina, especially Morrow Mountain and the Uwharrie range, has extensive aboriginal quarries; other sources include the Blue Hills of Massachusetts and the Southwest. Quarry debris on the Uwharrie peaks covers hectares.

Identification

Rhyolite is grey, green, tan or black, fine-grained with a dull lustre, often porphyritic with visible feldspar crystals, and weathers to a pale chalky surface that fresh flaking cuts through. It is harder to flake than chert. Banded varieties occur.

Substitutes and fakes

Rhyolite is unattractive to reproducers but Piedmont points are occasionally made. The weathering rind on genuine pieces is difficult to fake.

Elsewhere

Cite this article

Stratum Study. "Rhyolite" (Material). Stratum Study pack 2026.09, as of 2026-09-21. https://stratum.black/study/materials/rhyolite. Accessed 2026-09-21.

@misc{stratum-rhyolite,
  title        = {Rhyolite},
  author       = {{Stratum Study}},
  howpublished = {\url{https://stratum.black/study/materials/rhyolite}},
  year         = {2026},
  note         = {Material article, Stratum Study pack 2026.09, as of 2026-09-21; sources: stratum, wikidata. Accessed 2026-09-21.}
}

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