Late Prehistoric Oneota population movement into the central Plains

dc.citation.epage272en_US
dc.citation.issue173en_US
dc.citation.jtitlePlains Anthropologisten_US
dc.citation.spage257en_US
dc.citation.volume45en_US
dc.contributor.authorRitterbush, Lauren W.
dc.contributor.authorLogan, Brad
dc.contributor.authoreidlritterben_US
dc.contributor.authoreidbloganen_US
dc.date.accessioned2013-04-29T21:55:05Z
dc.date.available2013-04-29T21:55:05Z
dc.date.issued2000en_US
dc.date.published2000en_US
dc.description.abstractThe White Rock phase is an intrusive Late Prehistoric archaeological complex in the central Plains. It shows clear ties to the Oneota tradition of the upper Midwest. Population movement best explains the presence of this Oneota complex in the Plains. Interpretations of seasonal mobility or migration are evaluated through analysis of White Rock phase assemblages. Evidence for gardening and lithic material use patterns suggest permanent or year-round occupation of the central Plains resulting from the Oneota migration.en_US
dc.identifier.urihttp://hdl.handle.net/2097/15696
dc.language.isoen_USen_US
dc.relation.urihttp://www.jstor.org/stable/25669669en_US
dc.subjectWhite Rock phaseen_US
dc.subjectOneotaen_US
dc.subjectLate Prehistoricen_US
dc.subjectMigrationen_US
dc.subjectLithic raw materialsen_US
dc.titleLate Prehistoric Oneota population movement into the central Plainsen_US
dc.typeArticle (publisher version)en_US

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