Redeposition of vertebrate specimens is a significant concern on the Canadian plains because of the presence of faunas of immediately pre-Late Glacial Maximum and post-Late Glacial Maximum ages, separated by a hiatus of about 8 millennia representing presence or influence of glacial ice.
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The last pre-Late Glacial Maximum fluvial cycle gave rise to widespread valley fills assigned to the Empress Formation Saskatchewan Gravels and Sands , dating before about 20 14 C ka Rutherford, ; Stalker, a; Burns and Young, ; Rutter et al. Widespread terminal Pleistocene valley fills are assigned to the Bighill Creek Formation and equivalents, dated between about 12 and 10 14 C yrs BP Churcher, , , ; Stalker, b; Jackson et al. Upstream from eastern Edmonton, the North Saskatchewan Valley is narrow and steep-walled with Cretaceous bedrock exposures, marking postglacial incision through a preglacial upland.
Downstream from Edmonton, through the Fort Saskatchewan area, the valley widens abruptly and has less steep walls as it follows the trend of the preglacial Beverly Valley Farvolden, ; Rutter et al. Farther downstream, near Waskatenau, the river turns southeastward and leaves the Beverly Valley.
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In the Beverly reach of the river valley, postglacial gravel fills are inset into and superimposed upon preglacial deposits. Empress Formation deposits are dominated by clasts of quartzite, or quartzose sandstone, and black chert, with lesser amounts of arkosic sandstone, jasper, and locally derived coal fragments, wood, and clay ironstone.
Their relatively high compositional maturity likely reflects multiple cycling of resistant materials from the Rocky Mountains through Tertiary upland conglomerates to the Quaternary fills Westgate, Early postglacial North Saskatchewan River alluvium, on the other hand, is poorly sorted and compositionally less mature, with abundant Shield-derived clasts reworked from till. Vertebrate fossils are known from both deposits.
A diverse Pleistocene fauna was reported from pits in the Beverly east Edmonton area by Fuller and Bayrock , who argued that it dated from post-Late Glacial Maximum times. Yet it included not only bison referred to Bison occidentalis and B. A similar conclusion was reached by Guthrie and Harington Burns and Young , p. These findings remain in need of further testing through direct dating of specimens. Westgate described the terrace sequence along the North Saskatchewan in the Edmonton area. Fort saskatchewan singles are online now at InterracialDatingCentral, all you need to do is join.
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