Chilcotin Plateau Point

This triangular corner notch point exhibits a medium to large size profile, characterized by an elliptical cross-sectional shape. The blade's curvature can vary, displaying a subtle excurvate or incurvate profile. The shoulders of the point can range from being slightly barbed, where they curve outward, to a more horizontal orientation. The stem expands in width, creating a distinctive silhouette. The base of the point is generally straight, although it can exhibit a slight convex or concave curvature. The flaking pattern observed on this point is random, lacking a consistent or deliberate arrangement of flakes.

This type is mainly located in the central region of British Columbia, Canada. Refer to notes on its presence in Oregon

In their 1979 publication, Sturtevant and Walker brought attention to a distinctive medium to large corner notch point, predominantly discovered on the Chilcotin Plateau in British Columbia. This geographic region is notably associated with the presence of this particular point type. Notably, a thorough review of professional literature reveals no documented instances of this point being found within the United States. Although some collector-oriented sources, including Overstreet, suggest the presence of this point in Oregon, these claims are not substantiated by peer-reviewed references. Furthermore, a 2013 report by William Hranicky also mentions this point, but unfortunately, the source of his information remains unclear. It is essential to acknowledge that any contradictory evidence or reliable references that could confirm the presence of this point type in Oregon, beyond the aforementioned collector-based sources, would be a valuable contribution to the field and are eagerly sought.