- WOK 18-139
- Item
- [1964]
Part of W.O. Kupsch fonds
Amber, Baltic. A clear brownish-yellow polished pendant with an insect (flying ant) enclosed.
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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.
Anticline and adjacent tight syncline in Carboniferous rocks
Part of W.O. Kupsch fonds
Anticline and adjacent tight syncline in Carboniferous rocks. Devonian rocks to the right are light coloured. Near Rocky Creek crossing on Jasper-Edmonton highway. Sunday, May 29, 1960.
Part of W.O. Kupsch fonds
Anticline. Peace River. G.S.C. Photo.
Approximate extent of Arctic and Eastern faunal realms
Part of W.O. Kupsch fonds
Approximate extent of Arctic and Eastern faunal realms. (Nelson, 1959, p. 47).
Arboreal pollen and ratio of arboreal to non-arboreal pollen
Part of W.O. Kupsch fonds
Arboreal pollen and ratio of arboreal to non-arboreal pollen, Herbert Site.
Archaeologists at work near Gull Lake, Saskatchewan
Part of W.O. Kupsch fonds
Archaeologists at work near Gull Lake, Saskatchewan.
Part of W.O. Kupsch fonds
Archaeology. Sequence of human fossils and of Eurasian cultures during the Pleistocene epoch. Dunbar, 1960, p. 444.
Part of W.O. Kupsch fonds
Archaeology. Some weapon points of early big-game hunters, from 7 to 12 thousand years ago. Top row (left to right) Scottsbluff, Eden, Angostura; bottom row (left to right) Clovis Fluted, Folsom Fluted, Plainsview. After Wedel, 1961.