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Lower stratified drift Swift Current Creek section
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September 1960 (Vervaardig)
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1 transparency : colour ; 35mm slide
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Lower stratified drift Swift Current Creek section along north side of tributary to Swift Current Creek in Sec. 10, T. 19, R. 13, W. 3 meridian. At this place the Lower stratified drift may possible represent a weathered till (cf. Wickenden 1931 C, Sec. C) as it is not stratified, non-sorted, contains some erratics, is highly calcareous but is not a marl (organic, mainly algal, deposit) as Christiansen (1959) reported. Spade is placed on gradational zone from Wymark Till to Lower Stratified drift. Peter David holds hand on sharp contact between Lower stratified drift and AIkins Till. Tuesday September 13, 1960.
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Photographer: Kupsch, Walter Oscar
Copyright holder: University of Saskatchewan
Copyright expires: Unknown
Other terms: Responsibility regarding questions of copyright that may arise in the use of any images is assumed by the researcher.