Abstract
Radiocarbon dates from single-component prehistoric sites often span temporal sequences too long to be accounted for by spatial overlap in the patterning of features. One such example is the SunWatch site, which was long interpreted as a single-component occupation of relatively short duration (15–20 years), although the radiocarbon sequence comfortably spans a 500-year period (ca. A.D. 1000 to 1500). This study compares spatial contexts of the SunWatch radiocarbon dates with other temporal indicators, including architectural rebuilding, feature form and volume, and diagnostic artifact attributes. Two distinct portions of the radiocarbon sequence can be accounted for by reference to these other lines of evidence. Village growth is linked with internal and external processes, including the arrival of a small Mississippian group and the possibility of site reoccupation, common among shifting agricultural systems.
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