- WOK 16-16
- Item
- [1962]
Part of W.O. Kupsch fonds
Class cephalopoda - 'Loligo'. (Shrock and Twenhofel, 1953, p. 485).
1974 results directly related Exclude narrower terms
Part of W.O. Kupsch fonds
Class cephalopoda - 'Loligo'. (Shrock and Twenhofel, 1953, p. 485).
Cirque-Transformation of a drainage basin into a cirque
Part of W.O. Kupsch fonds
Cirque-Transformation of a drainage basin into a cirque (Schneidegger 1962, p. 199).
Cirques, horns, aretes and cols
Part of W.O. Kupsch fonds
Cirques, horns, aretes and cols. Their progressive development. In the first diagram, valley glaciers have produced cirques but, since erosion had been moderate, much of the original mountain surface has been unaffected by the ice. The result of more extensive glacial erosion is shown in the second diagram. In the final drawing, glacial erosion ha affected the entire mass and has produced not only ciques but also a matterhorn, and jagged knife-edged aretes. Leet and Judson, 1958, p. 235.
Part of W.O. Kupsch fonds
Cirques with small glaciers. Grossglockner, Austria.
Circularly ridged recessional hummocky moraine
Part of W.O. Kupsch fonds
Circularly ridged recessional hummocky moraine due north of Regina, Saskatchewan, onnorth side of Qu'Appelle Valley, which can benoticed in extreme right. Photo taken, looking east, by Murray Harris.
Circular pattern of minor end moraines
Part of W.O. Kupsch fonds
Circular pattern of minor end moraines (Gwynne, 1951, fig. 2).
Part of W.O. Kupsch fonds
Chart of the Sunda Shelf with drowned river channels shown by the black lines. Note their relation to the island rivers. Shepard, 1960, p. 90.
Channeling of greenish-yellowish sand facies into dark clay facies of Frenchman Formation
Part of W.O. Kupsch fonds
Channeling of greenish-yellowish sand facies into dark clay facies of Frenchman Formation, both unconformably overlying the white Whitemud Formation. Ferris coal seam is base of Paleocene Ravenscrag Formation. Ravenscrag Butte, Saskatchewan. May 1964.
Channel structures in Saskatchewan gravels
Part of W.O. Kupsch fonds
Channel structures in Saskatchewan gravels. North Hill gravel pit, Calgary. July, 1965.
Channel deposits of gravel and silty alluvium
Part of W.O. Kupsch fonds
Channel deposits of gravel and silty alluvium. Note stone concentration on top of gravel and cross section of ripples in upper part of silty, laminated deposit. Gravel pit south of Floral along highway 11, Sask. Fall, 1962.
Channel cross bedding in ice-contact gravels
Part of W.O. Kupsch fonds
Channel cross bedding in ice-contact gravels. Gravel pit along highway 11 south of Floral, Saskatchewan. October 7, 1962.
Champlain Sea, map of areal extent
Part of W.O. Kupsch fonds
Champlain Sea, map of areal extent. (Clark and Stearn, 1960, p. 282).
Chain structures for amphiboles and pyroxenes
Part of W.O. Kupsch fonds
Chain structures for amphiboles and pyroxenes (left). Silicon-oxygen tetrahedra form simple or double chains in the inosilicates by sharing oxygen atoms with neighbouring tetrahedra.
Part of W.O. Kupsch fonds
Cervine deer or stag, the American Wapiti or 'elk' (Cervus). Different from the true 'elk' (Alces) of Old World, which is the moose of North America. Colbert, 1955, p. 392.
Part of W.O. Kupsch fonds
'Ceratites nodosus'. Triassic. Ward's slide LW 35-112.