Abstract
A geochronological approach is used to examine the temporal and spatial parameters of terminal Late Fort Ancient (∼1450 –1750 CE) habitation sites in the Little Miami-Ohio Rivers confluence area. We use a Bayesian analysis of radiocarbon dates, microtephrochronology, a biostratigraphic indicator (Bison bison), and ethnohistorical records to examine terminal Late Fort Ancient sites in this region. Circular, stockaded villages (≤ 5 ha), consisting of single-family dwellings were replaced with large linear villages (≤ 8 ha), consisting of multifamily longhouses constructed parallel to the Little Miami and Ohio rivers. Smaller contemporary habitations and a plethora of underground maize silos suggest a seasonal pattern of population fission and fusion. At the time of Hernando de Soto's military conquests, ∼350 km to the south, terminal Late Fort Ancient villages in this region were increasing in number and size.
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