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dc.contributor.author Hanson, Michelle A.
dc.contributor.author Enkin, Randolph J.
dc.contributor.author Barendregt, René W.
dc.contributor.author Clague, John J.
dc.date.accessioned 2015-06-12T19:57:26Z
dc.date.available 2015-06-12T19:57:26Z
dc.date.issued 2015
dc.identifier.citation Hanson, M.A., Enkin, R.J., Barendregt, R.W. & Clague, J.J. (2015). Provenance and deposition of glacial Lake Missoula lacustrine and flood sediments determined from rock magnetic properties. Quaternary Research, 83, 166-177. DOI: https://doi.org/10.1016/j.yqres.2014.09.005 en_US
dc.identifier.uri https://hdl.handle.net/10133/3701
dc.description Sherpa Romeo green journal. Permission to archive accepted author manuscript. en_US
dc.description.abstract Repeated outburst flooding from glacial LakeMissoula,Montana, affected large areas of Washington duringMarine Oxygen Isotope Stage 2 (29–14 ka).We present the first high-resolution rock magnetic results from two sites that are critical to interpreting these outburst floods and that provide evidence of sediment provenance: glacial Lake Missoula, the source of the floods; and glacial Lake Columbia, where floodwaters interrupted sedimentation. Magnetic carriers in glacial LakeMissoula varves are dominated by hematite,whereas those in outburst flood sediments and glacial Lake Columbia sediments aremainly magnetite and titano-magnetite. Stratigraphic variation of magnetic parameters is consistent with changes in lithology. Importantly, magnetic properties highlight depositional processes in the flood sediments that are not evident in the field. In glacial Lake Columbia, hematite is present in fine silt and clay deposited near the end of each flood as fine sediment settled out of the water column. This signal is only present at the end of the floods because the hematite is concentrated in the finer-grained sediment transported from the floor of glacial LakeMissoula, the only possible source of hematite, ~240 km away. en_US
dc.language.iso en_CA en_US
dc.publisher Elsevier en_US
dc.subject Glacial Lake Missoula en_US
dc.subject Glacial Lake Columbia en_US
dc.subject Rock magnetic properties en_US
dc.subject Glacial outburst floods en_US
dc.subject Magnetic hysteresis en_US
dc.subject Thermomagnetic susceptibility en_US
dc.title Provenance and deposition of glacial Lake Missoula lacustrine and flood sediments determined from rock magnetic properties en_US
dc.type Article en_US
dc.publisher.faculty Arts and Science en_US
dc.publisher.department Department of Geography en_US
dc.description.peer-review Yes en_US
dc.publisher.institution Saskatchewan Geological Survey en_US
dc.publisher.institution Geological Survey of Canada en_US
dc.publisher.institution University of Lethbridge en_US
dc.publisher.institution Simon Fraser University en_US
dc.publisher.url https://doi.org/10.1016/j.yqres.2014.09.005


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