- LGS IX 3-2
- Item
- 1959 - 1964
Part of L.G. Saunders fonds
Beaver Creek's calm waters are seen as they wind though a autumn trees and grasses.
Saunders, Leslie Gale
1974 results directly related Exclude narrower terms
Part of L.G. Saunders fonds
Beaver Creek's calm waters are seen as they wind though a autumn trees and grasses.
Saunders, Leslie Gale
Part of W.O. Kupsch fonds
Beaver dam. Mission Canyon, Little Rocky Mountains. October, 1961.
Part of L.G. Saunders fonds
A tree is seen with its trunk partially chewed through by a beaver.
Bedding in Mississippian Lodegpole limestone
Part of W.O. Kupsch fonds
Bedding in Mississippian Lodegpole limestone. Mission Canyon, Little Rocky Mountains. October, 1961.
Bedding in Mississippian Lodegpole limestone
Part of W.O. Kupsch fonds
Bedding in Mississippian Lodegpole limestone. Mission Canyon, Little Rocky Mountains. October, 1961.
Bedrock high, distorted into ridges by ice shove
Part of W.O. Kupsch fonds
Nose Hills part of Neutral Hills; bedrock high, distorted into ridges by ice shove. East of Coronation, Alberta.
Bedrock surface, Dreghorn district
Part of W.O. Kupsch fonds
Bedrock surface, Dreghorn district, after Christiansen (1961, pl. II). From Kupsch, 1964, fig. 1.
Bedrock surface, Dreghorn district
Part of W.O. Kupsch fonds
Bedrock surface, Dreghorn district (Kupsch, 1964, fig. 2).
Part of W.O. Kupsch fonds
Topography, McLean area (Kupsch, 1964, fig. 5).
Part of W.O. Kupsch fonds
Topography, McLean area after Christiansen 1961, pl. II, from Kupsch, 1964, p. 277.
Bedrock surface, Regina-Wynyard area
Part of W.O. Kupsch fonds
Bedrock surface, Regina-Wynyard area (Kupsch, 1964, fig. 7).
Bedrock surface, Regina-Wynyard region
Part of W.O. Kupsch fonds
Bedrock surface, Regina-Wynyard region (Kupsch, 1964, fig. 8).
Bedrock topographic map of the Weyburn area
Part of W.O. Kupsch fonds
Bedrock topographic map of the Weyburn area, southeastern Saskatchewan, showing the periglacial surface. Contours are dashed where their position is uncertain. A - A^1 indicates line of section. All ranges west of the second meridian.(Meneley et al., 1957).
Part of W.O. Kupsch fonds
Bedrock Valley. Dissected miniature pediments on terraces in front of bedrock outcrops. Red Deer River near Drumheller, AB. November 10, 1962.
Bedrock valleys in southern Saskatchewan
Part of W.O. Kupsch fonds
Bedrock valleys in southern Saskatchewan (Christiansen 1962, fig. 1).