{"id":{"repo_id":"central-wash","oai_identifier":"oai:digitalcommons.cwu.edu:etd-1802"},"canonical_url":"https://search.dev.ndltd.org/etd/central-wash/oai:digitalcommons.cwu.edu:etd-1802","repository":{"repo_id":"central-wash","name":"Central Washington University","base_url":"https://digitalcommons.cwu.edu/do/oai/"},"display":{"title":"Stratigraphy and Site Formation at the Sanders Site (45 KT 315), Kittitas County, Washinton","abstract":"The Sanders site (45KT315) was excavated in 1971 and 1972 by Central Washington State College under the direction of Dr. William Smith, then Associate Professor of Anthropology at CWSC. A total of 88 1 x 1 meter units were excavated up to 270 cm below surface. During the initial excavations and in subsequent student work, there was investigation of what would now be called site geoarchaeology, but this work was not reported in detail. In this thesis, I synthesize existing records on site stratigraphy and completed new field characterization and laboratory analyses to build a geoarchaeological summary for the site. The site stratigraphy is characterized by episodic deposition and is the result of the interaction of fluvial, aeolian and colluvial processes. Periods of landform stability are marked by soil formation. Sediments preserved on-site appear to contain a relatively complete record of the Holocene, whereas across the creek at 45KT726, the earlier Holocene sediments have been stripped away by fluvial processes. Periods of landform stability and soil formation at Sanders roughly match the alluvial cycles presented for the Fogoil Project on the Yakima Training Center.","abstract_html":"The Sanders site (45KT315) was excavated in 1971 and 1972 by Central Washington State College under the direction of Dr. William Smith, then Associate Professor of Anthropology at CWSC. A total of 88 1 x 1 meter units were excavated up to 270 cm below surface. During the initial excavations and in subsequent student work, there was investigation of what would now be called site geoarchaeology, but this work was not reported in detail. In this thesis, I synthesize existing records on site stratigraphy and completed new field characterization and laboratory analyses to build a geoarchaeological summary for the site. The site stratigraphy is characterized by episodic deposition and is the result of the interaction of fluvial, aeolian and colluvial processes. Periods of landform stability are marked by soil formation. Sediments preserved on-site appear to contain a relatively complete record of the Holocene, whereas across the creek at 45KT726, the earlier Holocene sediments have been stripped away by fluvial processes. Periods of landform stability and soil formation at Sanders roughly match the alluvial cycles presented for the Fogoil Project on the Yakima Training Center.","abstract_has_math":false,"creators":["McLean, James"],"institution":null,"degree_name":"Master of Science (MS)","degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":["Steven Hackenberger","Patrick M. Lubinski","William Smith"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2017,"date_issued":"2017-01-01T08:00:00Z","date_published":"2017-01-01T08:00:00Z","updated_at":"2026-07-24T01:37:09Z","subjects":["Geoarchaeology","Stratigraphy","Site Formation","Sanders","Johnson Creek","YTC","Earth Sciences","Physical Sciences and Mathematics"],"languages":["English"],"rights":[],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://digitalcommons.cwu.edu/etd/911","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Steven Hackenberger","Patrick M. Lubinski","William Smith"]},{"key":"dc:creator","label":"Author","values":["McLean, James"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.available","label":"Dc Date Available","values":["2017-12-27T08:00:00Z"]},{"key":"dc:type","label":"Dc Type","values":["Text"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Science (MS)"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Geoarchaeology","Stratigraphy","Site Formation","Sanders","Johnson Creek","YTC","Earth Sciences","Physical Sciences and Mathematics"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["English"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["https://digitalcommons.cwu.edu/etd/911"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["The Sanders site (45KT315) was excavated in 1971 and 1972 by Central Washington State College under the direction of Dr. William Smith, then Associate Professor of Anthropology at CWSC. A total of 88 1 x 1 meter units were excavated up to 270 cm below surface. During the initial excavations and in subsequent student work, there was investigation of what would now be called site geoarchaeology, but this work was not reported in detail. In this thesis, I synthesize existing records on site stratigraphy and completed new field characterization and laboratory analyses to build a geoarchaeological summary for the site. The site stratigraphy is characterized by episodic deposition and is the result of the interaction of fluvial, aeolian and colluvial processes. Periods of landform stability are marked by soil formation. Sediments preserved on-site appear to contain a relatively complete record of the Holocene, whereas across the creek at 45KT726, the earlier Holocene sediments have been stripped away by fluvial processes. Periods of landform stability and soil formation at Sanders roughly match the alluvial cycles presented for the Fogoil Project on the Yakima Training Center."]},{"key":"dc:title","label":"Title","values":["Stratigraphy and Site Formation at the Sanders Site (45 KT 315), Kittitas County, Washinton"]}]}],"canonical_facts":{"dc:contributor":["Steven Hackenberger","Patrick M. Lubinski","William Smith"],"dc:creator":["McLean, James"],"dc:date.available":["2017-12-27T08:00:00Z"],"dc:description.abstract":["The Sanders site (45KT315) was excavated in 1971 and 1972 by Central Washington State College under the direction of Dr. William Smith, then Associate Professor of Anthropology at CWSC. A total of 88 1 x 1 meter units were excavated up to 270 cm below surface. During the initial excavations and in subsequent student work, there was investigation of what would now be called site geoarchaeology, but this work was not reported in detail. In this thesis, I synthesize existing records on site stratigraphy and completed new field characterization and laboratory analyses to build a geoarchaeological summary for the site. The site stratigraphy is characterized by episodic deposition and is the result of the interaction of fluvial, aeolian and colluvial processes. Periods of landform stability are marked by soil formation. Sediments preserved on-site appear to contain a relatively complete record of the Holocene, whereas across the creek at 45KT726, the earlier Holocene sediments have been stripped away by fluvial processes. Periods of landform stability and soil formation at Sanders roughly match the alluvial cycles presented for the Fogoil Project on the Yakima Training Center."],"dc:identifier":["https://digitalcommons.cwu.edu/etd/911"],"dc:language":["English"],"dc:subject":["Geoarchaeology","Stratigraphy","Site Formation","Sanders","Johnson Creek","YTC","Earth Sciences","Physical Sciences and Mathematics"],"dc:title":["Stratigraphy and Site Formation at the Sanders Site (45 KT 315), Kittitas County, Washinton"],"dc:type":["Text"],"thesis:degree_name":["Master of Science (MS)"]},"updated_at":"2026-07-24T01:37:09Z"}