AbstractThe Fourth of July valley site (5BL 120), a singlecomponent hunting camp at timberline in the Colorado Front Range, was occupied approximately 6000 radiocarbon years ago. Projectile points from the occupation area are typologically intermediate between James Allen and McKean Lanceolate points, and between Pryor Stemmed and Duncan points. The age and timberline location of the site, together with the transitional nature of the projectile points, support Husted's (1968) hypothesis that the McKean complex developed from Plano progenitors in high-mountain Altithermal refuge areas.
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Benedict et al. (1973) studied this question.
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