Abstract
This paper deals with the occurrence of two boulders of bituminous sandstone which have been found in the glacial deposits of central Alberta. They occur mixed with other material that was carried south by the Keewatin ice during glaciation. One boulder is a lens-shaped mass about 11 by 2 1/2 feet. These are now more than 200 miles from the source rock and were mistaken for local oil seepages.
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