Abstract
The Phillips Spring Site is situated on a Holocene terrace of the Pomme de Terre River in northern Hickory County, Missouri. Eleven radiocarbon dates provide a good chronologic framework for the four cultural components recognized at the site. There are three Archaic components which span the period 4280 to 1990 BP. The initial Archaic occupation coincides with the establishment of the present vegetation pattern in the area. A single Late Woodland assemblage, dating from 1410 to 1000 BP, is comparable in cultural content to components of the Highland Aspect.
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