Sand‐wedge and ventifact palaeoenvironmental indicators in North‐West Saskatchewan, Canada, 11 ka to 9.9 ka BP

Exhumed sand wedges and ventifacts in the upper Churchill watershed of north‐western Saskatchewan indicate that aeolian and periglacial processes were dominant from c. 11 to c 10.5 ka BP. Nineteen sand wedges were identified that display vertical foliation, form polygonal nets, and penetrate either...

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Bibliographic Details
Main Author: Timothy G. Fisher
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Ice
Online Access:https://doi.org/10.1002/(SICI)1099-1530(199610)7:43.0.CO;2-W