Just within sands and gravels attributed by Hunt to Late or
Post-Wisconsin outwash, one fragmentary point and a few flakes were
found. Some charcoal, ash and burned bone occurred at the same level,
extending in a lens about 2 inches lower. The point appears to the
authors to be the basal section of what might be called morphologically
a Plainview point (Krieger, in Sellards, Evans and Meade, 1947).
Flaking was parallel. Another parallel-flaked point of a similar type
was found higher up in the fill, and was undoubtedly a re-used piece
(see Fig. 25). Both points are of quartzite, and both have ground
edges. Five of the associated flakes were of a flinty material, 2 of
grainy quartzite.
These artifacts probably represent a culture of the early Lithic Stage
in the area, and are perhaps the earliest evidence of its occupation.
The fill was so sparse, however, that no further evidence could be
obtained.