Geology of the Engigstciak Archaeological Site, Yukon Territory

dc.contributor.authorJenny Mackay
dc.contributor.authorW. H. Mathews
dc.contributor.authorRichard S. MacNeish
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T15:40:47Z
dc.date.available2026-03-22T15:40:47Z
dc.date.issued1961
dc.descriptionCitaciones: 32
dc.description.abstractReports geological investigations is 1956-1957 to aid in dating the archeological finds. Quaternary sediments in a clay and a sand sequence are described; their stratigraphic relationships have been disrupted by soil movements resulting from freezing and thawing and from downslope creep. These soil movements, their mechanisms and rates postulated, apparently buried an organic layer containing artifacts progressively between two layers of marine clay. Due to overturning and mixing of layers of different ages, further complicated by a possible upthrust of the marine clay by glacier ice, the artifacts cannot be dated by geological means. From evidence indicating only one marine invasion coincident with glacial advance however, the archeological material is concluded to postdate the last Pleistocene glaciation.
dc.identifier.doi10.14430/arctic3659
dc.identifier.urihttps://doi.org/10.14430/arctic3659
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/53777
dc.language.isoen
dc.publisherArctic Institute of North America
dc.relation.ispartofARCTIC
dc.sourceUniversity of British Columbia
dc.subjectGeology
dc.subjectGlacial period
dc.subjectPleistocene
dc.subjectQuaternary
dc.subjectGlacier
dc.subjectSequence (biology)
dc.subjectPaleontology
dc.subjectArchaeology
dc.subjectGeomorphology
dc.subjectOceanography
dc.titleGeology of the Engigstciak Archaeological Site, Yukon Territory
dc.typearticle

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