Kom W and X Basin: Erosion, Deposition, and the Potential for Village Occupation

The twentieth-century excavations of stratified deposits at Kom W, adjacent to Lake Qarun in Fayum north shore, Egypt, led to a variety of interpretations, including the argument for the presence of a Neolithic village. This has influenced the evaluation of early to mid-Holocene occupation in Egypt. Here, we report our recent study of the erosion and deposition processes at the site and its environs in order to reassess these interpretations. Changes in the level of Lake Qarun, evidence for wind erosion, deflation, and deposition, and analyses of artifact density provide a geomorphic context for Kom W and its immediate environs. Radiocarbon determinations from surface hearths that surround the Kom are reported. From the time of its initial formation, Kom W was subject to post-depositional processes, particularly wind erosion, which have affected the site’s current form, and the preservation of features and artifact within the deposits. These changes need to be considered when deriving behavioral interpretations from the archaeological record at Kom W and in the surrounding area. The composition of deflated deposits that surround Kom W suggests that the site is not as unique as once imagined. Remains that might have allowed interpretations of a village occupation have not survived. Instead, deposits are consistent with other early to mid-Holocene occupations interpreted as locations with the use of domesticates but without villages.