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Blocks of Red-River type Ordovician dolomite
Part of W.O. Kupsch fonds
Blocks of Red-River type Ordovician dolomite collected from drift to be used as building stone. Campus, University of Saskatchewan. Unidentified person in picture.
Lemon shaped concretion in Belly River sandstone - near Outlook, SK
Part of W.O. Kupsch fonds
Lemon shaped concretion in Belly River sandstone Bank of South Sasktachewan River near Outlook, SK.
Drilling rig and pumping well - near Weyburn, SK
Part of W.O. Kupsch fonds
Drilling rig and pumping well. These closely spaced wells produce from different horizons. Near Weyburn, SK.
Folded upland of Liddon Gulf and Sabine Bay, Melville Island
Part of W.O. Kupsch fonds
Looking across folded upland of Liddon Gulf (left) and Sabine Bay, Melville Island. In the foreground is a syncline with strata dipping inwards. Erosion here has left a central ridge. Note how the large river has cut right across the fold. 1 Aug. 1950; 20,000 feet.
One solution to problem in slide 131
Part of W.O. Kupsch fonds
One solution to problem in slide 131.
Second solution to problem in slide 131
Part of W.O. Kupsch fonds
Second solution to problem in slide 131.
Topography of Moosejaw area, SK
Part of W.O. Kupsch fonds
Topography of Moosejaw area, SK.
Block diagram showing possible development of Missouri Coteau
Part of W.O. Kupsch fonds
Block diagram showing possible development of Missouri Coteau.
Distribution and thickness of Devonian prairie Evaporites
Part of W.O. Kupsch fonds
Distribution and thickness of Devonian prairie Evaporites. Black wells are salt free.
Students hunting for fossils near Hungry Hollow, W. Ontario
Part of W.O. Kupsch fonds
Students hunting for fossils near Hungry Hollow, W. Ontario. July, 1949.
Badlands, South Dakota, Oligocene
Part of W.O. Kupsch fonds
Badlands, South Dakota, Oligocene.
Part of W.O. Kupsch fonds
Grand Canyon, Arizona. September 1947. W.O.K. and Rob Scholten in photograph.
Glory hole, Ruby Gulch Mine, Little Rock Mountains
Part of W.O. Kupsch fonds
Glory hole, Ruby Gulch Mine, Little Rock Mountains. Dark yellow green rock under trees to the left is Precambrian amphibolite schist. To the right of this is white veined syenite (Tertiary), to right of this is the Ruby shear zone (gold) in the syenite and farther to the right is syenite with pyrite.
Diagrams related to peneplain, panplain and pediplain
Part of W.O. Kupsch fonds
Diagrams to suggest the differences in the modes of origin of (A) a peneplain, (B) a panplain, and (C) a pediplain (Thornbury, 1956, p. 182).
Present topography and geologic structure - Dominguez Hills oil field, California
Part of W.O. Kupsch fonds
Map showing the close correlation between present topography and geologic structure in the Dominguez Hills oil field, California (Thornbury, 1956, p.583)