MemorySask

Some stages in rhinocerous evolution showing woolly rhinocerous

WOK 5-91
Pièce
[1948-58]

Some stages in rhinocerous evolution showing woolly rhinocerous.

Relief diagram and map of small fold - Jackfork formation near Amity, Arkansas

WOK 5-98
Pièce
[1948-58]

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
Pièce
[1948-58]

Fait partie de 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
Pièce
[1948-58]

Fait partie de 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
Pièce
1953

Fait partie de 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
Pièce
1953

Fait partie de 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
Pièce
1951

Fait partie de W.O. Kupsch fonds

Breached anticline (anitclinal valley) of oil producing structure (Turner Valley, Alberta).

Drilling rig near Weyburn SK

WOK 5-116
Pièce
1958

Fait partie de W.O. Kupsch fonds

Drilling rig near Weyburn SK.

Territory between Chesterfield Inlet and Wagner Bay

WOK 5-124
Pièce
[1948-58]

Fait partie de 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