Foothills Erratics Train
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The Foothills Erratics Train is a 580 miles long, narrow, linear scatter of thousands of typically angular boulders of distinctive quartzite and pebbly quartzite that lie on the surface of a generally
Big Rock
Gog Group
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The Gog Group is a stratigraphic unit in the Western Canada Sedimentary Basin. It is present in the eastern and western main ranges of the Canadian Rockies in Alberta and British Columbia. It was name
Foothills Erratics Train
…Lower Cambrian shallow marine quartzite and conglomeratic quartzite, that are not native to this region of Alberta. These rocks only occur within the Gog Group that is exposed in the Tonquin Valley in the Rocky Mountains of central western Alberta. Their specific source has been identified as being near Mount…
Trace fossils in a slab from the Gog Group