Aligned coal pebbles and streaks in till - Eastend, Sask
- WOK 2-138
- Item
- 1954
Part of W.O. Kupsch fonds
Aligned coal pebbles and streaks in till. Dempster's clay pit, Eastend, Sask.
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Aligned coal pebbles and streaks in till - Eastend, Sask
Part of W.O. Kupsch fonds
Aligned coal pebbles and streaks in till. Dempster's clay pit, Eastend, Sask.
"Alkali" salt flat near Cantuar, Saskatchewan
Part of W.O. Kupsch fonds
"Alkali" salt flat at shore of a saline lake near Cantuar, Saskatchewan; note abundance of salt wort (Salicornia rubra).
Kupsch, Walter Oscar
Alluvial fan at the mouth of gully entering South Saskatchewan River
Part of W.O. Kupsch fonds
Alluvial fan at the mouth of gully entering South Saskatchewan River just west of bridge at Saskatchewan Landing. November 7, 1962.
Alluvial fan from tributary into Qu'Appelle Valley - Katepwa, Saskatchewan
Part of W.O. Kupsch fonds
Alluvial fan from tributary into Qu'Appelle Valley near Katepwa, Saskatchewan.
Kupsch, Walter Oscar
Alluvial fan of tributary cut - Frenchman River
Part of W.O. Kupsch fonds
Alluvial fan of tributary cut by Frenchman River north of Knollys, Sask. Notice slumping.
Almost vertical beds of Chonta limestone.
Part of W.O. Kupsch fonds
Almost vertical beds of Chonta limestone. Boqueron del Padre Abad.
Altiplano with Cordillera de Apolobamba in Peru
Part of W.O. Kupsch fonds
Altiplano with Cordillera de Apolobamba in Peru and Bolivia in the background. Taken from near Cajata.
Part of W.O. Kupsch fonds
Amber, Baltic. A clear brownish-yellow polished pendant with an insect (flying ant) enclosed.
Part of W.O. Kupsch fonds
American mastodon. Note the long jaw and low forehead compared with those of the mammoth. (Clark and Stearn, 1960, p. 376).
Amphipora in slab of Fairholme fm.
Part of W.O. Kupsch fonds
Amphipora in slab of Fairholme fm. Tributary of Jura Creek near Exshaw, Alberta. May, 1961.
Ancient river systems of the Great Lakes Basins after Spencer 1891
Part of W.O. Kupsch fonds
Ancient river systems of the Great Lakes Basins after Spencer 1891 (Mozola, 1962, p. 21).
Part of W.O. Kupsch fonds
Angular unconformity. Zechstein above folded Carbiniferous. Carboniferous rocks (folded intensely) were leveled down by erosion; and on the erosion surface Permian strata (Zechstein) were horizontally deposited. The whole sequence was then raised, and again attacked by erosion. Cloos, 1954, p1. 44.
Part of W.O. Kupsch fonds
Angular unconformity. Pennsylvanian rocks lie with well developed angular unconformity on older folded rocks. Location: Melville Island at N. lat. 76 degrees, 00': W. long. 113 degrees 20'. For geology see G.S.C. Map 13-1959. Airphoto T416C-75.
Part of W.O. Kupsch fonds
Antarctica, Ross Ice Shelf. Top: Ice in the Bay of Whales, a reentrant in the Ross Ice Shelf, protected in part by islands. The bay ice, 30 to 50 feet thick is folded by the pressure of the advance of the much thicker shelf ice around the protecting islands. The indvidual folds are several tens of feet high. Similar folds nearby are caused by the drag of the shelf ice over its own morainal deposits. Bottom: Sections through the Ross Shelf Ice abd Bay of Whales. The thickness of the ice has been determined by seismic methods. (Gilluly et al., 1959, p. 226).
Part of W.O. Kupsch fonds
Anticlinal valley near (notice the opposite dips) Pisac.