1974 results directly related Exclude narrower terms
Shore line of terraces along Old Wives Lake
Part of W.O. Kupsch fonds
Shore line of terraces along Old Wives Lake.
Shingled pebbles on bar in Sungaruyacu River
Part of W.O. Kupsch fonds
Shingled pebbles on bar in Sungaruyacu River.
Shelf off San Diego, California
Part of W.O. Kupsch fonds
Somewhat haphazard distribution of sediment types on the shelf off San Diego, California. Shepard, 1960, p.86.
Sheep track slumping near Eastend, Sask
Part of W.O. Kupsch fonds
Sheep track slumping near Eastend, Sask.
Part of W.O. Kupsch fonds
Shear strength of minerals common to quick clay declines rapidly as a water content rises (Kerr, P.F., 1963, Sci. Amer. Nov., p. 140).
Shale Shaker, Rapdan oil field, Saskatchewan
Part of W.O. Kupsch fonds
Close up of a shale Shaker, Rapdan oil field, Saskatchewan
Shadow zone of the earth's core for an earthquake originating in Japan
Part of W.O. Kupsch fonds
Earthquakes. The shadow zone cast by the earth's core in the case of an earthquake originating in Japan. Holmes, 1953, p. 375.
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.
Service rig. Acidizing truck, Eastend oil field, Saskatchewan
Part of W.O. Kupsch fonds
Service rig. Acidizing truck, Eastend oil field Saskatchewan.
Sequence in the development of a kame terrace
Part of W.O. Kupsch fonds
Sequence in the development of a kame terrace. Ice wasting from an irregular topography lingers longest in the valleys. While the ice still partially fills one of these valleys, outwash may be deposited between it and the valley walls. The final disappearance of the ice leaves the outwash in the form of terraces along the sides of the valley (Leet and Judson, 1958, p. 249).
Seljalandsfoss - waterfall plunges from edge of cliff
Part of W.O. Kupsch fonds
Seljalandsfoss. Waterfall plunges from the edge of overhanging cliff, 80 m high. August 9, 1960.
Seismic structure map on top of palaeozoics, Mooze Jaw area, SK
Part of W.O. Kupsch fonds
Seismic structure map on top of palaeozoics, Mooze Jaw area, SK.
Seismic structure map on top of Palaeozoic rocks - Cantaur field
Part of W.O. Kupsch fonds
Seismic structure map (Carter Oil Co., 1944, reconnaissance)on top of Palaeozoic rocks, Cantaur field.
Part of W.O. Kupsch fonds
Sediments in the ocean. Location of cores with sand and silt layers (shaded areas) found on the deep floor of the Atlantic Ocean. Shepard, 1960, fig. 84.
Sections to illustrate current bedding
Part of W.O. Kupsch fonds
Cross bedding. Sections to illustrate current bedding and its values in determining whether a bed is right way up or upside down. A) the current-bedding structure is complete B) the upper part has been eroded off down to AB. The truncated current-bedding pattern is right way up C) the truncated cross-bedding pattern is upside down. Holmes, 1953, p. 95.