We wish to address the contention that the physical remains described by Bettinger are the only possible manifestations of pinyon exploitation. If such is the case, one would expect to find similar manifestations in other areas of the Great Basin. Fortunately, a similar surface survey has been accomplished. Thomas's (1971) study of the Reese River Valley employs an almost identical sampling design based on 500-meter random transect tracts which crosscut biotic communities.