1974 results directly related Exclude narrower terms
Pike's Pimple, smoke against orange sky
Part of L.G. Saunders fonds
The Observatory of the University of Saskatchewan is seen at sunset during the winter.
Picea Glauca, white spruce, Forestry Farm, Sutherland
Part of W.O. Kupsch fonds
Picea Glauca, white spruce, Forestry Farm, Sutherland.
Physiographic divisions of Cordilleran Region
Part of W.O. Kupsch fonds
Physiographic divisions of Cordilleran Region. G.S.C, Econ. Geol. 1, p. 284.
Phylogeny of mastodonts and elephants
Part of W.O. Kupsch fonds
Phylogeny of mastodonts and elephants. Stirton, 1959, p. 11.
Part of W.O. Kupsch fonds
Petrified tree on display in front of museum in Drumheller, AB. Collected from the Edmonton (Upper Cretaceous) formation. From left to right Earl Christiansen, HAnk Wolbeer, Al Lissey and Jim Murray. November 10, 1962.
Part of W.O. Kupsch fonds
Photograph taken on a windy day on Peter Pond Lake (Big Buffalo Lake), Saskatchewan
Permo-Carboniferous glaciation without continental drift
Part of W.O. Kupsch fonds
Permo-Carboniferous glaciation without continental drift. Geographic reconstruction during Upper Palaeozoic ice ages. Glaciated regions indicated by horizontal directions of ice flow by arrows. Note land bridges (Umbgrove, 1942, p. 140).
Part of W.O. Kupsch fonds
Peneplains and pediplains. Suggested comparison between the sequence of erosional stages in an arid climate and those in a humid climate. Leet and Judson, 1958, p. 285.
Part of W.O. Kupsch fonds
Pegmatite dike cutting lit-par-lit injection gneiss, Chesterfield Inlet, N.W.T.. August 3, 1965.
Pediments of Little Rocky Mountains
Part of W.O. Kupsch fonds
Pediments of Little Rocky Mountains. Note increase in gradient wheree pediments is located at the base of Camp Creek Butte to the right. Further distant are West and East Coburn Buttes. Photo from Zortman Butte looking east.
Pediment surface, dissected, developed on Cretaceous strata
Part of W.O. Kupsch fonds
Pediment surface, dissected, developed on Cretaceous strata, covered by Tertiary-Quaternary gravels. Looking north from Morrison Butte, Little Rocky Mountains. October, 1961.
Part of W.O. Kupsch fonds
Pediment surface, dissected. Looking north from Morrison Butte, Little Rocky Mountains. October, 1961.
Pediment surface developed over slump blocks
Part of W.O. Kupsch fonds
Pediment surface developed over slump blocks. Frenchman Valley near Neighbor, Sask.
Part of W.O. Kupsch fonds
Pediment near Hidalgo, Mexico.