CAMP CREEK, Kneberg (Kneberg, 1956): A-16
GENERAL DESCRIPTION: This is a small to medium, triangular point with incurvate base.
MEASUREMENTS: The measurements of the illustrated example are: length, 35 mm.; width at base, 16 mm.; thickness, 7 mm.; depth of basal concavity, 2 mm.
FORM: The cross-section is usually biconvex. The blade is usually straight; rarely, incurvate or excurvate. The distal end is acute. The base is incurvate and usually thinned with some fine retouch.
FLAKING: The flaking used to shape the blade and hafting area is random and fairly well executed. Some fine retouch is in evidence along the blade edges. Much of the flint and quartzite used at the Camp Creek Site has poor flaking qualities, resulting in a poorly manufactured point.
COMMENTS: The type was named from the Camp Creek Site (Cambron Site 284) on the Nolichucky River in Greene County, Tennessee. The illustrated specimen is from Zone A of the Camp Creek Site (Lewis and Kneberg, 1957). This example was selected by Cambron from his collection from Camp Creek (Site 284) as typical of the type. Although a minority type in all levels at this site, it is found with burials more frequently than are other types. It comprises about 15% of the stemless points in Level D, but in other levels does not exceed 6% (Lewis and Kneberg, 1957). The type appears to be a part of the Greeneville complex, found along the western edge of the Appalachians southwest from the Greeneville, Tennessee, area into south-central Alabama. It is usually associated with the early to middle Woodland period. Some other points that appear in this complex are Greeneville, Nolichucky, Triangular Copena, Coosa, and possibly Ebenezer. At the Stanfield-Worley Bluff Shelter (DeJarnette, Kurjack and Cambron, 1962) Zone A, four examples were found in Level 1, five in Level 2, one in Level 3 and three in Level 4. This indicates a Woodland association at this site. Most of the examples recovered from Flint Creek Rock Shelter (Cambron and Waters, 1961) were in the lower three-quarters of Stratum I (Woodland). One example was recovered from Level 1 and one from Level 2 at Rock House Shelter in Marshall County, Alabama (University of Alabama Site Ms 201). Ten examples were recovered from Zones A and B (Woodland) and two from Zone D (Archaic) at Flint River Mound (Webb and DeJarnette, 1948a). Kneberg suggests a date of from about 1000 B.C. to 500 A.D.