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Quaternary stratigraphy and geology of the Rocky Mountain Foothills, southwestern Alberta

https://doi.org/10.4095/224301
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inferred← citeshttps://doi.org/10.2139/ssrn.4676239openalex-extracted
inferred← citeshttps://doi.org/10.1007/978-3-319-44595-3_11openalex-snapshot
The Foothills Erratics Train Region
inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.106034openalex-snapshot
Proglacial lakes and the retreat pattern of the southwest Laurentide Ice Sheet across Alberta, Canada
inferred← citeshttps://doi.org/10.1016/j.scitotenv.2024.176969openalex-snapshot
Controls on regional sulphate distribution in shallow groundwater in the western Canadian Interior Plains
inferred← citeshttps://doi.org/10.1017/qua.2019.10openalex-snapshot
Beryllium-10 dating of the Foothills Erratics Train in Alberta, Canada, indicates detachment of the Laurentide Ice Sheet from the Rocky Mountains at ~15 ka
inferred← citeshttps://doi.org/10.1017/qua.2021.40openalex-snapshot
Glacial kettles as archives of early human settlement along the Northern Rocky Mountain Front
inferred← citeshttps://doi.org/10.1111/bor.12355openalex-snapshot
Sedimentary architecture of a glaciolacustrine braidplain delta: proxy evidence of a pre‐Middle Wisconsinan glaciation (Grimshaw gravels, Interior Plains, Canada)
inferred← citeshttps://doi.org/10.1139/cjes-2013-0106openalex-snapshot
Evidence for an Early Pleistocene glaciation in the Okanagan Valley, southern British Columbia
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