During the 1980 excavation of the Lightning Spring site in the North C
ave Hills of South Dakota, a group of Tongue River silicified sediment
bifaces was discovered in one of the deeper McKean levels of the site
. In addition to these bifaces, a large suite of Duncan projectile poi
nts was recovered from the four McKean occupations. The seven bifaces
provide significant insight into the McKean phase lithic technological
system used in this area of the Northwestern Plains, and the associat
ed Duncan points help explicate the projectile point rejuvenation syst
em used by these McKean hunters.