This paper presents a description and analysis of an
obsidian fluted point recently discovered within the
bounds of the Nevada Test and Training Range (NTTR)
in southern Nevada. Analyses include physical and
technological descriptions of the point and source
analysis of the obsidian from which it is made. These
analyses are followed by a discussion of the typological
attribution of the point based on a recent comparison by
Beck et al. (2019) of 462 Far Western fluted points with 95
Clovis points from the Southwest, Plains, and Northwest.
We conclude with a discussion of where the NTTR point
fits in the regionís prehistory, and what its raw material
source suggests about population mobility during the
terminal Pleistocene.