New PDF release: Mississippian Community Organization: The Powers Phase in

By Michael J. O'Brien

The Powers part undertaking, a multiyear archaeological application undertaken in southeastern Missouri through the college of Michigan in the past due Nineteen Sixties and early Nineteen Seventies, represents a milestone in Americanist archaeology. This quantity reinterprets a few of the previous conclusions from the long term excavations of the Turner and Snodgrass websites and complements the usefulness of the findings for archaeologists attracted to the past due prehistory of the Mississippi River Valley.

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Extra info for Mississippian Community Organization: The Powers Phase in Southeastern Missouri (Interdisciplinary Contributions to Archaeology)

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But as the present volume demonstrates, the successes of the project far outweighed any deficiencies. In attempting to summarize the results of archaeological work conducted several decades earlier, one constantly runs the risk of taking the work out of context. Anyone, through hindsight, can denigrate an older effort, even if only to note wistfully that, “If the excavators had only. . ” Given that the Powers Phase Project began over three decades before this volume was written, it stands to reason that some of its goals and objectives might seem outdated by today’s standards—or if not outdated, perhaps a bit naive.

The driving force behind the Powers Phase Project was Price, a local Ripley County, Missouri, native who did his undergraduate work in archaeology at the University of Missouri and his doctoral work at the University of Michigan. As an undergraduate, Price excavated several test units at Powers Fort in 1964 and 1965, uncovering at least two houses and several burials. 1). Concurrent with the survey, Price excavated a small portion of the Turner site, which was being looted by local residents, and determined that the village had burned, effectively sealing the house floors and the items that were on them (Price, 1969).

Dots represent locations of pollen cores mentioned in the text (after O’Brien and Dunnell, 1998). , 1991:167–168). At least two northeast–southwest-trending braided surfaces connected with the displaced Mississippi River are exposed in the Eastern Lowlands. 1). Primary drainage of the surface today is provided by the St. Francis River. 2). When the Mississippi River shifted its course out of the Western Lowlands and began to drain east of Crowley’s Ridge, it created its own outwash fan and braided drainage pattern, in the process reworking earlier sediments and eradicating previous northeast–southwest-trending Ohio channels.

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