GEOARCHAEOLOGY AND LANDSCAPE HISTORY AT THE MONONGAHELA PERIOD SQUIRREL HILL ARCHAEOLOGICAL SITE, WESTERN PENNSYLVANIA
Preliminary results of a ground penetrating radar survey in the northwest portion of the site revealed a large rectangular structure at 23-46 cmbs, along a paleochannel of the Conemaugh River, with a size and shape that does not conform to the typical circular Johnston-phase houses. Auger cores taken from the northern end of the site revealed a series of buried landscapes at depths of ~108, ~130, and ~163 cmbs, suggesting that earlier occupations at the site may exist. Interestingly, buried horizons do not appear in cores taken from the southern end of the site, but rather suggest substantial overbank deposition which decreased concomitant with the Johnston Phase occupation. Cores along the eastern edge of the site revealed alternating flood and gleyed deposits, suggesting and that the paleo-environment was more dynamic than previous researchers have previously thought. This paper will report on these field results, as well as recent radiocarbon, particle size and soil micromorphology analyses designed to refine the nature of occupation and past landscape history for the site.