Marine-shell beads have been recovered from numerous
archaeological sites throughout the Intermountain West.
Direct radiocarbon determinations and typological
cross-dating indicate that groups conveyed beads long
distances inland throughout the Holocene. Because the
oxygen and carbon isotopic signatures of Callianax
(previously Olivella) sp. snail shells reflect local sea
surface temperature, researchers over the past 15
years have started to assign beads to source regions
(stretches of the coast from which people collected
shells). We report radiocarbon and stable isotope data
for a Callianax biplicata bead from Oregonís Hawksy
Walksy Valley, the only bead that has been recovered
from this archaeologically important region. These data
indicate that the bead was conveyed ~400 km. inland at
480ñ285 cal B.P. from somewhere along the Oregon or
northern California coasts. We place these results within
the context of other provenance studies of beads in the
northern Great Basin to add to our understanding of
how, when, and from where coastal producers conveyed
shell beads to inland consumers.