Site 48CR11356 is located west of the bank of Fillmore Creek and approximately 350 feet southwest of the earthen dike of Seaverson Reservoir. AMS Radiocarbon analysis on charcoal recovered from eight of the thermal features indicates multiple occupations spanning the Opal phase of the Archaic period (5690 ±30 years B.P. 4070 ±30 years B.P.), with more intensive use from approximately 5300–5200 years B.P. Soil samples representing Cultural Stratum II and the base of a feature beneath a piece of burned sandstone were submitted for pollen analysis.
Linda Scott Cummings (Sat,) studied this question.
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