Chronology and extent of Late Cenozoic ice sheets in North America: A magnetostratigraphic assessment
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Glacial landforms and sediments (landsystem) of the Smoking Hills area, Northwest Territories, Canada: Implications for regional Pliocene – Pleistocene Laurentide Ice Sheet dynamics
2021, Quaternary Science ReviewsCitation Excerpt :They maintained that Canadian Shield erratics (i.e. granitic or gneissic material), indicative of a continental-style Laurentide glaciation, were only found scattered on the uppermost surface of the section (HR 1). In their absence, they argued that all underlying diamictons originated from a local “Horton Ice Cap” source (Melville Hills; Fig. 1a; Barendregt and Duk-Rodkin, 2004; Duk-Rodkin et al., 2004; Duk-Rodkin and Barendregt, 2011) and that Laurentide ice was responsible for depositing only the uppermost surface lag. Geomorphological mapping was undertaken on ArcticDEM hillshade imagery (Porter et al., 2018), viewed under oblique and vertical perspectives using various illumination aspects and elevations, in combination with stereo aerial photographs and Google Earth imagery.
Global chronostratigraphical correlation table for the last 2.7 million years, version 2019 QI-500
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2018, Proceedings of the Geologists' Association