Southwestward dipping Ravenscrag sandstone
- WOK 4-3
- Item
- 1956
Part of W.O. Kupsch fonds
Southwestward dipping Ravenscrag sandstone along Souris River Valley fault. (Keith Knox)
1974 results directly related Exclude narrower terms
Southwestward dipping Ravenscrag sandstone
Part of W.O. Kupsch fonds
Southwestward dipping Ravenscrag sandstone along Souris River Valley fault. (Keith Knox)
Part of W.O. Kupsch fonds
Southeastern Asia, the East Indies, and Australia showing area within approximately 600 feet of sea level. During the stages of maximum glacial accumulation, these tracts were laid bare and became routesd of travel between what are now islands. This explains the presence of rhinoceros in Java and of many large fossil mammals on other islands. New Guinea and Australia were connected and their plants and animals are similar. The deep water between Australia and the large islands to the northwest has effectively halted the passage of most plants and animals. Present land areas are shown in grey, oceans deeper than about 600 feet in black, and shallowly submerged areas in white (Stokes, 1960, p. 406).
Part of W.O. Kupsch fonds
South Saskatchewan River dam. Drainage map showing sites under construction and other sites investigated (Pollock, 1962).
Part of W.O. Kupsch fonds
South Saskatchewan River dam. Geologic profile across deltaic sediments on west side of main damsite (Pollock, 1962).
South Saskatchewan River valley near and west of Saskatchewan Landing
Part of W.O. Kupsch fonds
South Saskatchewan River valley near and west of Saskatchewan Landing. Note incised terrace and lag concentrate of boulders. Fall, 1962.
South Saskatchewan River near Prelate Ferry
Part of W.O. Kupsch fonds
South Saskatchewan River and Pleistocene section near Prelate Ferry, Saskatchewan.
South Saskatchewan River at Saskatoon
Part of W.O. Kupsch fonds
South Saskatchewan River at Saskatoon looking toward Nutana. Note the low terrace, present day flood plain, rising to higher level beyond.
South Saskatchewan River at Elbow
Part of W.O. Kupsch fonds
South Saskatchewan River at Elbow. Qu'Appelle River dry valley at left.
South Saskatchewan River at Elbow
Part of W.O. Kupsch fonds
South Saskatchewan River at Elbow.
South Saskatchewan River at break up
Part of W.O. Kupsch fonds
South Saskatchewan River at break up.
Part of W.O. Kupsch fonds
South Fiord Dome. Axel Heiberg Island. Airphoto A 16186-73.
Some stages in rhinocerous evolution showing woolly rhinocerous
Part of W.O. Kupsch fonds
Some stages in rhinocerous evolution showing woolly rhinocerous.
Solifluction disturbance of upper drift layers and filled-in ice wedge
Part of W.O. Kupsch fonds
Solifluction disturbance of upper drift layers and filled-in ice wedge. Trans Canada pipeline trench.
Solheimajokull, outlet glacier of Myrdalsjokull
Part of W.O. Kupsch fonds
Solheimajokull, outlet glacier of Myrdalsjokull. Note ice left by recent hlaup. August 11, 1960.
Soil profile developed in till
Part of W.O. Kupsch fonds
Soil profile developed in till, diagram. (Clark and Stearn, 1960, p. 282).