James (Jimmy) Allen Point

This lanceolate point exhibits a slender, triangular profile with a cross-sectional shape that transitions from elliptical to flattened. The blade's curvature is subtly outward, giving it a faintly excurvate appearance. Notably, the point's maximum width is typically situated above its base, which is characterized by a pronounced concavity. Evidence of grinding is often observed in the hafting region, suggesting intentional shaping for attachment. The flaking pattern on this point is distinguished by parallel oblique scars, indicating a deliberate and controlled flaking technique.

The dimensions of the arrowheads are characterized by the following measurements: overall length ranges from 45 to 120 mm, with a typical average length of 55 to 65 mm. The width of the blade spans from 18 to 33 mm, averaging between 22 to 26 mm. Additionally, the basal concavity is measured to be between 3 to 7 mm.

This type is mainly discovered in the western grasslands and extending into the Rocky Mountain range. They appear to be linked with elevated terrain in these areas. These points are also discovered in the southern grasslands area and extending into northeastern New Mexico

In a notable comparison, the archaeological specimen at hand bears a resemblance to the Fredrick point, yet exhibits a distinctive characteristic that sets it apart. Specifically, the base of this point is more profoundly concaved, whereas the Fredrick point is typically marked by a base that is either straight or only slightly concave. This subtle yet significant difference highlights the nuanced variations that exist within the realm of Native American arrowhead typology, underscoring the importance of meticulous observation and detailed analysis in the classification and study of these ancient artifacts.