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Mineral exploration in large parts of Canada is difficult because the bedrock is hidden beneath thick layers of glacially derived sediments. One technique to overcome this, called drift prospecting, identifies high concentrations of economically significant minerals or elements in the glacial sediments and helps to identify their bedrock sources. This project was designed to interpret Quaternary geology to assist in mineral development. This report shows how the geochemistry and lithology of the glacial sediments vary across the region and how the stratigraphy and provenance of those sediments can be interpreted so that geochemical anomalies or mineralized boulders may be traced back to their bedrock sources.
1919/28 cumulation includes material previously issued in the 1919/20-1935/36 issues and also material not published separately for 1927/28. 1929/39 cumulation includes material previously issued in the 1929/30-1935/36 issues and also material for 1937-39 not published separately.