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Roed, Murray A., Barendregt, René W., Benowitz, Jeff A., Smith, C.A.S., Sanborn, P.T., Greenough, John D., Huscroft, Crystal, Layer, Paul W., Mathewes, Rolf W., Tessler, Dez (2014) Evidence for an Early Pleistocene glaciation in the Okanagan Valley, southern British Columbia. Canadian Journal of Earth Sciences, 51 (2) 125-141 doi:10.1139/cjes-2013-0106

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Reference TypeJournal (article/letter/editorial)
TitleEvidence for an Early Pleistocene glaciation in the Okanagan Valley, southern British Columbia
JournalCanadian Journal of Earth Sciences
AuthorsRoed, Murray A.Author
Barendregt, René W.Author
Benowitz, Jeff A.Author
Smith, C.A.S.Author
Sanborn, P.T.Author
Greenough, John D.Author
Huscroft, CrystalAuthor
Layer, Paul W.Author
Mathewes, Rolf W.Author
Tessler, DezAuthor
Year2014 (February)Volume51
Issue2
PublisherCanadian Science Publishing
DOIdoi:10.1139/cjes-2013-0106Search in ResearchGate
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Mindat Ref. ID485007Long-form Identifiermindat:1:5:485007:0
GUID0
Full ReferenceRoed, Murray A., Barendregt, René W., Benowitz, Jeff A., Smith, C.A.S., Sanborn, P.T., Greenough, John D., Huscroft, Crystal, Layer, Paul W., Mathewes, Rolf W., Tessler, Dez (2014) Evidence for an Early Pleistocene glaciation in the Okanagan Valley, southern British Columbia. Canadian Journal of Earth Sciences, 51 (2) 125-141 doi:10.1139/cjes-2013-0106
Plain TextRoed, Murray A., Barendregt, René W., Benowitz, Jeff A., Smith, C.A.S., Sanborn, P.T., Greenough, John D., Huscroft, Crystal, Layer, Paul W., Mathewes, Rolf W., Tessler, Dez (2014) Evidence for an Early Pleistocene glaciation in the Okanagan Valley, southern British Columbia. Canadian Journal of Earth Sciences, 51 (2) 125-141 doi:10.1139/cjes-2013-0106
In(2014, February) Canadian Journal of Earth Sciences Vol. 51 (2) Canadian Science Publishing
Abstract/Notes Depositional evidence of Early Pleistocene glaciations in British Columbia are documented at only a few sites. Near Kelowna, in southern British Columbia, a construction project exposed glacial sediments beneath Lambly Creek Basalt, providing a minimum age for this glaciation. The basalt is composed of a number of flows yielding ages that range from 0.76 ± 0.11 to 1.5 ± 0.1 Ma. The sediments consist of a diamicton, interpreted to be till, up to 3 m thick mantled by a weakly developed paleosol. The diamicton is underlain by fluvial sands up to 5 m thick, in places revealing injection features, and minor faulting. A unit of stratified gravel underlain by grey clay is inferred to underlie the exposed sediments, based on nearby outcrops and excavations. Sediments and overlying basalts are normally magnetized and are assigned to the Jaramillo normal subchron (1.069–0.987 Ma). The till is here referred to as the Westbank First Nation Till. It is Early Pleistocene in age and represents the earliest evidence of glaciation in the Okanagan Valley. Stone fabric analysis and clast lithologies suggest that ice movement was from northwest to southeast, and is here referred to as the West Kelowna Advance; we infer that this advance was part of a larger regional glaciation. Other Early Pleistocene glaciations in the Cordillera are briefly reviewed.


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