Novaculite — Novaculite
Novaculite National Park Service Picture – Courtesy of Hot Springs National Park Archives, Wikimedia Commons, Public domain (US)

Material · lithic

Novaculite

North America — Southeast

Novaculite is the dense, white to grey microcrystalline quartz rock of the Ouachita Mountains of Arkansas, quarried for tools from Paleoindian times and later for whetstones, and traded to Poverty Point and across the Caddo area. Its quarries near Hot Springs are extensive. Dalton, Gary and Caddo Gahagan bifaces in novaculite are collected.

Kindlithic
RegionsNorth America — Southeast

Sources

The Arkansas Novaculite formation crops out in the Ouachita Mountains around Hot Springs and Magnet Cove, Arkansas, and into southeastern Oklahoma, with aboriginal quarries on Indian Mountain and elsewhere. Cobbles occur in Ouachita and Saline river gravels.

Identification

Novaculite is white, grey, cream or occasionally black or red, opaque to slightly translucent, with a fine granular texture and a dull to waxy lustre; it is harder and less glossy than chert. Heat treatment adds gloss and pink tones. Weathering is minimal.

Substitutes and fakes

Arkansas knappers produce novaculite points, and the stone does not patinate strongly, which makes age hard to judge. Edge wear and provenance are the guides.

Elsewhere

Cite this article

Stratum Strata. "Novaculite" (Material). Stratum Strata pack 2026.09, as of 2026-09-21. https://stratum.black/strata/materials/novaculite. Accessed 2026-09-21.

@misc{stratum-novaculite,
  title        = {Novaculite},
  author       = {{Stratum Strata}},
  howpublished = {\url{https://stratum.black/strata/materials/novaculite}},
  year         = {2026},
  note         = {Material article, Stratum Strata pack 2026.09, as of 2026-09-21; sources: stratum, commons, wikidata. Accessed 2026-09-21.}
}

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Sources for this article: Stratum editorial (Stratum editorial);Wikimedia Commons (CC-BY-4.0);Wikidata (CC0). As of 2026-09-21; Strata pack 2026.09. Data reproduced under the licences shown; text in Stratum's own words unless a section names its source.

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