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Creators/Authors contains: "Butler, Brian"

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  1. null (Ed.)
    The presence of Dover chert artifacts at the Mississippian Kincaid site was established in the 1930s and recent work has shown that Dover, or something very much like it, was being brought into the Black Bottom as early as the late Middle Archaic. There has been a growing concern that some of what has been traditionally identified as Dover chert in the Kincaid area is actually a variety of Fort Payne chert. Samples of Dover-like chert from Archaic and late Early-to-Middle Woodland (Baumer) components at Kincaid have been tested for geological provenance, and the results suggest that a preference for local Fort Payne chert existed during both occupations. 
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