Interpreters in Churchill, Manitoba
- WOK 19-66
- Item
- 1965
Part of W.O. Kupsch fonds
Citation reads: A.W.R. Carrothers (centre) with Eskimo interpreters (Simonee Michael at right), Churchill Manitoba. August 1, 1965.
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Interpreters in Churchill, Manitoba
Part of W.O. Kupsch fonds
Citation reads: A.W.R. Carrothers (centre) with Eskimo interpreters (Simonee Michael at right), Churchill Manitoba. August 1, 1965.
TransAir Canson CF-IEE, Churchill Manitoba
Part of W.O. Kupsch fonds
TransAir Canson CF-IEE, Churchill Manitoba. August 1, 1965.
Loading TransAir Canson CF-IEE, Churchill Manitoba
Part of W.O. Kupsch fonds
Loading TransAir Canson CF-IEE, Churchill Manitoba. August 1, 1965.
Part of W.O. Kupsch fonds
Eskimo museum, Churchill, Manitoba. July 31, 1965.
Part of W.O. Kupsch fonds
Gun in front of Eskimo museum, from old Fort Churchill, Manitoba. July 31, 1965.
Grain elevator and lodging docks
Part of W.O. Kupsch fonds
Grain elevator and lodging docks, Churchill, Manitoba. July 31, 1965.
Part of W.O. Kupsch fonds
From left to right: Fred Carrothers, Ron Hodghinson, Stuart Lake, Lyle Gillespie at Lynn Lake airport. July 31, 1965.
Part of W.O. Kupsch fonds
Lake deltas (schematic cross sections). A. stable level. B. fluctuating level. Dunbar and Rodgers, 1957, p. 41.
Channel structures in Saskatchewan gravels
Part of W.O. Kupsch fonds
Channel structures in Saskatchewan gravels. North Hill gravel pit, Calgary. July, 1965.
Part of W.O. Kupsch fonds
Floodplain deposits. A. Schmetic plan of deposits alonf Mississippi River near Lake Providence, Louisiana. B. Schematic cross section of floodplain deposits of a meandering river, showing lenses of deposits of channel deposits (dotted, clay plugs in solid black) in matrix of interchannel deposits. Length of area shown, several tens of miles; large vertical exaggeration. Dunbar and Rodgers, 1957, p. 34.
Role of turbulence in keeping sediment in suspension
Part of W.O. Kupsch fonds
Role of turbulence in keeping sediment in suspension. The concentration of sediment is greater near the bottom and progressively less upward. The ascending eddy (A) therefore carries more sediment per unit volume than the descending eddy (b). Dunbar and Rodgers, 1957, p. 6.
Velocities at which different size grades of sediment erode, transport and deposit
Part of W.O. Kupsch fonds
Graph showing velocities at which different size grades of sediment will be eroded, transported or deposited, plotted on double logarithmic scale. Dunbar and Rodgers, 1957, p. 5.
Laminar and turbulent flow in streams
Part of W.O. Kupsch fonds
Laminar and turbulent flow in stream. Velocity is indicated by the relative length of the flow lines. Dunbar and Rodgers, 1957, p. 5.
Settling velocity of quartz particles in still water
Part of W.O. Kupsch fonds
Settling velocity of quartz particles in still water, plotted on double logarithmic scale. Experimentally determined velocities are represented by small circles. Dunbar and Rodgers, 1957, p. 5.
Map of California showing topographic provinces and the principal faults
Part of W.O. Kupsch fonds
Map of California showing topographic provinces and the principal faults. 1. Ocean, with approximate edge of continental crust indicated by dotted line. 2. Major mountain areas. 3. Lowlands and minor mountain areas. 4. San Andreas fault. 5. Other high angle faults, active or recently active. 6. Inactive high-angle faults of earlier systems. King 1959, p. 165.