Quartzite erratic carried by glacier ice from Mount Edith Cavell in Jasper to current location in the Canadian prairies during the Pleistocene Epoch

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This glacial erratic, part of the Foothills Erratics Train, was carried by glacier ice from Mount Edith Cavell in the Rocky Mountains of Jasper National Park to the Canadian prairies.

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Size: 2020px × 3030px
Location: Calgary, Alberta, Canada
Photo credit: © Rosanne Tackaberry / Alamy / Afripics
License: Licensed
Model Released: No

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