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Beaver Lake Paleo Indians


G-9 Beaver Lake From Flint Michigan

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Also See: Arkabutla, Barber, Bat Cave, Candy Creek, Cumberland, Dalton, Golondrina, Midland, Pike County, Quad, Simpson, Suwannee
Location: Midwestern to Eastern United States and Florida
Associated Dates: 11,000 – 8500 B.P. – Paleo – Early Archaic
Morphology: Auriculate
General Description: The Beaver Lake projectile point is a medium to large sized lanceolate unfluted, blade with flairing basal ears or auricles on the stem base. The basal edges and stem sides are typically ground smooth and the base is concave and is rarely straight. The basal edge often has short basal thinning flakes removed. The blade edges are recurved and constrict towards the base to form an extended stem or hafting area. The Beaver Lake type is comparable to the Cumberland point type but the Beaver Lake totally lacks fluting and specimens typically show only moderate basal thinning. At one time, Beaver Lake points were called Unfluted Cumberland. Beaver Lake points are usually much thinner in cross section that Cumberland points and can have broader width proportions. The Beaver Lake’s cross section is typically biconvex, sometimes with a median ridge exhibited on one or both blade faces.
The Beaver Lake points were knapped with a combination of controlled percussion and pressure flaking techniques. They have a late Paleo-Indian affiliation and are considered part of the Dalton Cluster of projectile points. Beaver Lake points are rare but do occur throughout the Tennessee River Valley in northern Alabama, northeastern Mississippi, Tennessee, Kentucky and Missouri. They can sporadically occur over much of the South since Beaver Lake points have been identified from northern Florida, South Carolina, North Carolina and Georgia. A few points have been recovered in the Ohio Valley from Illinois, southern Indiana, West Virginia and Ohio.
The size of Beaver Lake point can range from 45 mm to 86 mm in length. The average size is 64 mm in length, with a typical width of 24 mm. Thickness averages 8 mm. The type has been called the Unfluted Cumberland in some papers. The point was named in 1962 by David L. DeJarnette, James W. Cambron, David C. Hulse and Edward B. Kurjack for examples that were recovered from the Stanfield-Whorley Bluff Shelter, Colbert County, Alabama. It was named for the the Beaver Lake area of Limestone County, Alabama.


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