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Abstract
AbstractA collection from a small Late Wisconsin site is described. This assemblage exhibits a distinctive coreworking technique and a distinctive variety of fluted points. It is dated on geological grounds to between 11,000 B.C. and 9000 B.C. at a time when spruce stands were probably becoming established in the area. The contrasts between this assemblage and others described from Northeastern North America suggest a number of hypotheses not testable with the available data.
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