Outline is Representative of Size and Shape:
Name Details:
Identified By:
Named For: City of St. Louis
Date Identified:
Type Site:
Point Validity:
Valid type
This sub-type has limited professional references. This is considered a valid sub-type
Description of Physical Characteristics and Flaking Pattern:
This is a medium to large lanceolate point with a flattened cross section. The blade is excurvate constricting towards the base. The widest part of the blade is the top one third to one half. The blade constricts narrowest at the base. The base is concave. This point is fluted on one or both faces. This point has a parallel to horizontal transverse flaking pattern.
Size Measurements:
See
Clovis for similar sizes
Commonly Utilized Material:
Additional Comments:
There is great debate over the classification of Clovis style points. It is argued that the same characteristics of any single type can be seen through-out the distribution of the Clovis type and represent normal variations of the Clovis point. Others argue that specific areas specialized the type and are seen with greater frequency in those areas. Therefore, these represent later variants and unique subtypes to the Clovis point.
Distribution:
Distribution Comments:
This point is primarily found in the Ohio River valley, Tennessee River Basin, and the mid to upper Mississippi River valley.
Age / Periods:
Date: 14,000 - 10,000 B.P.
Cultural Period: Paleo
Glacial Period: Late Pleistocene
Culture:
Age Details:
Similar Points:
Agate
Basin,
Angostura,
Barnes,
Beaver Lake,
Browns Valley,
Conerly,
Copena Articulated, Crowfield,
Cumberland,
Dalton,
Golondrina,
Fayette,
Northumberland,
Red Stone,