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dc.contributor.advisorWaters, Michael
dc.creatorKeene, Joshua L.
dc.date.accessioned2010-10-12T22:31:06Z
dc.date.accessioned2010-10-14T16:00:13Z
dc.date.available2010-10-12T22:31:06Z
dc.date.available2010-10-14T16:00:13Z
dc.date.created2009-08
dc.date.issued2010-10-12
dc.date.submittedAugust 2009
dc.identifier.urihttps://hdl.handle.net/1969.1/ETD-TAMU-2009-08-855
dc.description.abstractThe archaeological literature warns against trusting the context of artifacts found within a vertisol due to the constant mixing of sediments caused by the shrink/swell properties of clays. These churning processes were thought to be the defining characteristic of vertisols until only the past few decades. It is now apparent that vertisols vary drastically based on a wide spectrum of variables and are fully capable of forming without churning processes. The Buttermilk Creek Site, Block A represents a prime example of a minimally developed vertisol. In addition, the site itself is a heavily occupied lithic quarry that has been almost continuously inhabited since Clovis and possibly Pre-Clovis times. This thesis takes a detailed look at the sediments and distribution of lithic artifacts from Block A of the Buttermilk Creek site to address the two following research objectives: 1) to determine if the archaeological context within the floodplain sediments at Block A has been disturbed by post-depositional processes, and 2) to identify discrete occupation surfaces within the vertic floodplain sediments at the site. These objectives are addressed using a variety of methods, including: 1) plotting the stratigraphic position of diagnostic artifacts, 2) determining the size distribution of debitage and artifact quantities throughout the floodplain deposits, 3) examining the distribution of cultural versus non-cultural lithic material, 4) recording the presence or absence of heat alteration in the deposits, 5) creating maps showing the degree of fissuring across the site, 6) analyzing differences in patination on artifacts, and 7) analyzing the presence of calcium carbonate on artifacts from all levels. Results from these analyses show that, despite the classification of sediments at Block A as a vertisol, vertical displacement of artifacts is largely absent. Chronologically ordered diagnostic points, consistently size sorted artifacts, and a lack of constant mixing of calcium carbonate throughout the profile suggest that artifacts found as deep as 20 cm below the Clovis-aged horizon represent intact cultural horizons. These oldest components found in Block A may represent some of the earliest known evidence of people in the New World.en
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.subjectButtermilk Creeken
dc.subjectvertisolen
dc.subjectpedoturbationen
dc.subjectarchaeologyen
dc.subjectlithicsen
dc.subjectsize sortingen
dc.subjectClovisen
dc.subjectpre-clovisen
dc.subjectsite formationen
dc.subjectargilliturbationen
dc.subjectclay cracksen
dc.subjectslickensideen
dc.subjectGaulten
dc.subjectgeoarchaeologyen
dc.subject41BL1239en
dc.subjectgrumusolen
dc.subjectedwards plateauen
dc.subjectgilgaien
dc.subjectfolsomen
dc.subjectgolondrinaen
dc.subjectangosturaen
dc.subjectpleistocene holocene transitionen
dc.titleSite Formation Processes at the Buttermilk Creek Site (41BL1239), Bell County, Texasen
dc.typeBooken
dc.typeThesisen
thesis.degree.departmentAnthropologyen
thesis.degree.disciplineAnthropologyen
thesis.degree.grantorTexas A&M Universityen
thesis.degree.nameMaster of Artsen
thesis.degree.levelMastersen
dc.contributor.committeeMemberGoebel, Ted
dc.contributor.committeeMemberTchakerian, Vatche
dc.type.genreElectronic Thesisen
dc.type.materialtexten


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