Convento Point

This triangular point features a slender profile with a broadening stem, exhibiting a flattened cross-sectional morphology. The blade edge is predominantly straight, although subtle variations may occur, ranging from a gentle outward curve to a slight inward curvature. The shoulder regions are characterized by barbed formations, which can be less pronounced in smaller specimens. The stem itself expands toward the base, forming a convex terminus. The flaking pattern observed on this point is irregular and non-directional, lacking a discernible orientation or sequence.

This type is mainly discovered in Chihuahua and Coahuila, Mexico, and extends into the Big Bend area of Texas and New Mexico