Cryogenian strata of the Windermere Supergroup were deposited in tectonically active basins throughout the North American Cordillera from Alaska to Mexico.
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Dry Creek component I and the Chindadn complex at the Village site may contain part of the early history of the fluted point complexes that became widespread in North America during those millennia, but additional recent finds of fluted points themselves have not appreciably aided the resolution of the many questions that pertain to their origins.
Finally, we comment on a number of themes concerning the peopling of the New World including the concepts of migration and colonization, the importance of the Bering land bridge and the ice-free corridor, and the likely role of mankind in late Wisconsin extinctions.
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