Uncovering Huber Lifeways: An Overview of Findings from Four Years of Excavations at the Huber Phase Middle Grant Creek Site (11WI2739) in Northern Illinois

ABSTRACT

This article reports on recent findings from the ongoing archaeological project at the single- component early seventeenth-century Huber phase site, Middle Grant Creek (11WI2739), located at Midewin National Tallgrass Prairie in Will County, Illinois. Excavations and geophysical surveys conducted over the past four years are yielding valuable data that are expanding our understandings of this critical period just prior to European colonialism. Findings have revealed a wide range of protohistoric activities, including foodways, skilled craft production, and ceremonial activities as well as far-flung trade relationships that illustrate the endurance of Indigenous trade networks into at least the early seventeenth-century. This article introduces the latest findings from Middle Grant Creek and brings them into discussions of this key period in Midwestern archaeology.     

Archaeological sedimentology of overbank silt deposits on the floodplain of the Ohio river near Louisville,Kentucky

The surface of the floodplain of the Ohio River about 20km southwest of Louisville, Kentucky, is a series of linear ridges and swales that are subparallel to the channel of the river, which here is relatively straight and flows southward. Numerous prehistoric occupational sites are located on these ridges. The sediments that underlie the ridges, which were examined in four archaeological excavations as deep as 8 m, are predominantly sandy silt and silty fine to very fine sand and appear to be mainly the product of overbank deposition from suspended load. Abundant cultural material and occupational sites dating as early as 10,000 years BP are found in the sediments at depths as great as 6·5 m. The fine sediments of the floodplain are underlain by sand and gravel.The context of the cultural materials and the stratigraphy and morphology of the deposits indicate that the ridged deposits began as linear riverside sand and gravel bars. These were succeeded upward by fine-grained overbank deposits in which the ridged morphology was maintained because the overbank silt and fine sand were deposited as prograding elongate bars at high water. As the floodplain ridge built upward, the sedimentation rate decreased and the sand content of the sediments diminished, and as the river channel occasionally shifted, the ridged deposits were built in successive subparallel sequences.Two archaeological consequences are implicit in this depositional model of orderly growth of the floodplain. First, available archaeological data from floodplain segments along other parts of the river should confirm the model; and second, the model should make it possible to search the floodplains of the Ohio River for stratified sites of any desired age.     

Looking ‘The Gift’ in the mouth: Russia as donor (Respond to this article at http://www.therai.org.uk/at/debate)

While the Soviet Union was a significant donor of international development aid, since the 1990s, a generation of Russians has experienced the subject position of ‘recipient’ in the global political economy. However, following its G8 presidency in 2006, Russia officially signalled its intention to (re‐)emerge as an aid donor. Should the Russian government's efforts to join the global community of donors be understood as a defence mechanism against what Mauss called the ‘wounding’ experience of being treated as a perpetual recipient? International development aid is seen here as a cultural phenomenon whose underlying assumptions are both challenged and affirmed by the arrival of ‘emerging donors’ such as Russia.