2002 Denver Annual Meeting (October 27-30, 2002)

Paper No. 10
Presentation Time: 8:00 AM-12:00 PM

PRELIMINARY ANALYSIS ON SOURCING CLAY SEDIMENTS USED IN POTTERY PRODUCTION AT KUKULIK, SAINT LAWRENCE ISLAND


JOZWIK, Diana, Department of Geology and Geophysics, Univ of Alaska Fairbanks, Fairbanks, AK 99701, ftdj@uaf.edu

This project employs geological methods to characterize the archaeological site of Kukulik, on Saint Lawrence Island in the Bering Strait region. This site was excavated by Otto Geist from 1931-1935 (Geist 1936) and includes pottery, wood, bone and ivory artifacts. Clay pottery fragments are one of the most abundant artifacts found at the site. The clay source of the clay remains a matter of debate. Geist, in his report, stated that the clay source for the Kukulik pottery was located on the west side of Niyrakpak lagoon, approximately 30 miles from the archaeological site. I suggest that the people of Kukulik were utilizing local sources of clay to produce their pottery, rather than transporting clay or finished products from the distant lagoon site to their homes. To test this hypothesis, I will be employing geological methods consisting of X-ray Diffraction, Electron Microprobe analysis, X-ray Fluorescence and petrographic slides to fingerprint the source of clay utilized in the Kukulik pottery. Currently, X-ray Fluorescence is being used to determine indications of trace elements that can be used to fingerprint the different clay sediments collected from sites around the island. The results will be compared to data acquired from the analysis of the pottery sherds. Upon completion of this project, I will be able to produce a chronology of the pottery and its constituents over the time period of the site. Trends in the mineralogical data related to the depth of the artifacts have two possible explanations. Either the source area for the clay changed over time, or outside influences such as trade or the influx of new peoples from other regions or cultures led to changes in pottery production. Recognition of these trends has implications to the study of other prehistoric sites in the arctic and the movement of prehistoric people within the Bering Sea area.