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The evolution of elephants showing the Mastodon and Mammoth
- WOK 5-86
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
The evolution of elephants showing the Mastodon and Mammoth.
Restoration of Pleistocene Wooly Mammoth and Mastodon
- WOK 5-88
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Restoration of a Pleistocene mastodon (above) and a Pleistocene Woolly mammoth (below). A tooth of each is shown with a hand for scale. The crowned tooth of the mastodon was suitable for diet of twigs, branches and cones, whereas the infolded structure of the mammoth tooth was more adapted to a grass diet (Zumberge 1958, p. 362).
Some stages in rhinocerous evolution showing woolly rhinocerous
- WOK 5-91
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Some stages in rhinocerous evolution showing woolly rhinocerous.
Relief diagram and map of small fold - Jackfork formation near Amity, Arkansas
- WOK 5-98
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Relief diagram and geologic map of a small fold - Jackfork formation near Amity, Arkansas (Gilluly, Waters, and WOodford, 1952, p. 204)
Diagram of a fault cutting horizontal strata
- WOK 5-99
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Diagram of a fault cutting horizontal strata. A, the fracture before displacement; B, after displacement but before erosion; C, after erosion of fault scarp (Emmons, Thiel, Stauffer, Allison, 1955, p. 461).
Effects of transverse normal faults upon anticlines and synclines
- WOK 5-100
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Schematic diagram to show the effects of transverse normal faults upon the topographic expression of the noses of plunging anticlines and synclines (Thornbury, 1956, p. 229).
Wind erosion affecting Frenchman sandstone
- WOK 5-106
- Stuk
- 1953
Part of W.O. Kupsch fonds
Wind erosion affecting Frenchman sandstone along highway 37 south of bridge across near Frenchman River. Stu Jordan in photograph.
Close up of Red-River type Ordovician and Tyndall dolomite
- WOK 5-110
- Stuk
- 1953
Part of W.O. Kupsch fonds
Close up showing Red-River type Ordovician and Tyndall dolomite as building stone. Medical building, University of Saskatchewan.
Breached anticline of oil producing structure - Turner Valley, AB
- WOK 5-115
- Stuk
- 1951
Part of W.O. Kupsch fonds
Breached anticline (anitclinal valley) of oil producing structure (Turner Valley, Alberta).
- WOK 5-116
- Stuk
- 1958
Part of W.O. Kupsch fonds
Drilling rig near Weyburn SK.
Territory between Chesterfield Inlet and Wagner Bay
- WOK 5-124
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Territory between Chesterfield Inlet and Wagner Bay, looking east at about 64 degrees, 35'N, 90 degrees, 50' W showing fractures. 20 June, 1948; 20,000 feet.
Topography of Touchwood Hills area
- WOK 5-126
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Topography of Touchwood Hills area.
Structure contour map on top of Lower Cretaceous, Touchwood Hills area
- WOK 5-130
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Structure contour map on top of Lower Cretaceous, Touchwood Hills area, SK.
Real solution to problem in slide 131
- WOK 5-134
- Stuk
- [1948-58]
Part of W.O. Kupsch fonds
Real solution to problem in slide 131; map of Indonesia.