Incised meanders of meltwater stream on glacier, Ellesmere Island
- WOK 18-36
- Item
- [1963]
Part of W.O. Kupsch fonds
Incised meanders of meltwater stream on glacier, Ellesmere Island, north of Greeley Fiord. Air photo A 16706-46.
1974 results directly related Exclude narrower terms
Incised meanders of meltwater stream on glacier, Ellesmere Island
Part of W.O. Kupsch fonds
Incised meanders of meltwater stream on glacier, Ellesmere Island, north of Greeley Fiord. Air photo A 16706-46.
Index map - Moose Mountain area
Part of W.O. Kupsch fonds
Index map - Moose Mountain area.
Index map of southeastern SK and adjacent areas showing periglacial drainage
Part of W.O. Kupsch fonds
Index map of southeastern Saskatchewan and adjacent areas. Of the periglacial drainage, only the channels of the Missouri and Yellowstone rivers are shown. The Weyburn area is indicated by marginal ruling (Meneley et al., 1957).
Index map of southwestern Saskatchewan
Part of W.O. Kupsch fonds
Index map of southwestern Saskatchewan and adjacent regions showing the Dollard area.
Index to maps covering Moose Mountain area
Part of W.O. Kupsch fonds
Index to maps covering Moose Mountain area.
Influence of lithological differences on topography and vegetation
Part of W.O. Kupsch fonds
Influence of lithological differences on topography and vegetation. Lookiing north along outcrop ledges of Edmonton formation exposed near Trans-Canada Highway between Calgary and Banff. Dip is to the left, west. Saturday, May 28, 1960.
Inoceramus nebrascensis and Bacilites compressus
Part of W.O. Kupsch fonds
Inoceramus nebrascensis (S.E. corner sec. 30, T. 21, R. 22, W. 2) and Bacilites compressus (no location) from the Bearpaw formation, Sask.
Inselbergs of batholithic rocks on a rejuvenated erosion surface
Part of W.O. Kupsch fonds
Inselbergs of batholithic rocks on a rejuvenated erosion surface, Madagascar. The crystalline floor has been bevelled by a vast erosion surface that is slightly rejuvenated as indicated by the rivers which begin to cut down. On the surface lies a group of Inselbergs whose steep slopes form a clearly visible angle with the erosion surface. They are residual hills of harder rocks belonging to an oval shaped batholith the outline of which is indicated by the drainage. Erosion of this group was clearly fracture-controlled. In places the erosion surface penetrates into the group and all the batholithic rock has been removed. France Institut Geographique National. Relief form atlas, 1956, p. 103.
Intensely fractured syentite in road cut
Part of W.O. Kupsch fonds
Intensely fractured syentite in road cut at station F-1, Alder Gulch near Zortman Butte, Little Rocky Mountains, Montana. May, 1964.
Intercontinental migration across the Bering Strait
Part of W.O. Kupsch fonds
Intercontinental migration between Asia and North American across the Bering Strait (Kay and Colbert, 1964, fig. 24-12).
Interglacial and pre-glacial deposits, Canadian Arctic
Part of W.O. Kupsch fonds
Interglacial and pre-glacial deposits, Canadian Arctic(Raasch et al., 1961, v. 1, p. 407).
International Potash Technology Conference fonds
This collection contains unpublished papers presented at the Second International Potash Technolgy Conference, Hamburg, Germany, 26-29 May 1991. The Conference attracted scientists from various countries, including Canada, France, Germany, Brazil, Jordan, Spain, and the [then] USSR.
International Potash Technology Conference
Interpreters in Churchill, Manitoba
Part of W.O. Kupsch fonds
Citation reads: A.W.R. Carrothers (centre) with Eskimo interpreters (Simonee Michael at right), Churchill Manitoba. August 1, 1965.
Intersecting crevasse fillings near Kindersley, Sask
Part of W.O. Kupsch fonds
Intersecting crevasse fillings near Kindersley, Sask.
Iron mountain, Mary River, N.W.T.
Part of W.O. Kupsch fonds
Citation reads: "Iron mountain, Mary River, N.W.T. August 15, 1965."