1974 results directly related Exclude narrower terms
Aerial view of parabolic and complex dunes in Great Sand Hills area
Part of W.O. Kupsch fonds
Dunes. Parabolic and complex dunes in Great Sand Hills area. Wind direction from west. Active dunes are white, stabilised dunes grey. Location: sec. 16, T. 20, R. 24, W. 3, Sask.
Part of W.O. Kupsch fonds
Aerial photograph of saline area. Note shallow saline lakes. Till derived largely from Cretaceous shales. Sec. 1, T. 10, R. 11, W. 2.
Aerial view of sand dunes north of Cypress Hills
Part of W.O. Kupsch fonds
Aerial photograph of sand dunes north of Cypress Hills. Sec. 14, T. 12, R. 24, W. 5.
Aerial view of slump area - Cypress Hills
Part of W.O. Kupsch fonds
Aerial photograph slump area near deep valley in the Cypress Hills. Sec. 29, T. 6, R. 23, W. 3.
Aerial view of Souris spillway
Part of W.O. Kupsch fonds
Aerial photograph of Souris spillway. Note stream is now a misfit; also note oxbow lakes and channel scars. Sec. 9, T. 1, R. 34, W. 1.
Aerial view of terminal moraine and esker
Part of W.O. Kupsch fonds
Aerial photograph of terminal moraine in the middle background, esker in the foreground, glacier's ridge and striation on right-hand side, Alaska.
Aerial view of tonal halo around Carnduff field
Part of W.O. Kupsch fonds
Aerial photograph showing tonal halo around Carnduff field
Aerial view of tonal halo of Nottingham field
Part of W.O. Kupsch fonds
Aerial photograph of tonal halo of Nottingham field. Notice stream adjustment.
Aerial view of volcanic area, Nudo Coropuna in background
Part of W.O. Kupsch fonds
Aerial view of volcanic area with Nudo Coropuna (21,696 feet) in background
Aerial view of washboard moraine forming a re-entrant
Part of W.O. Kupsch fonds
Aerial photograph of washboard moraine forming a re-entrant or V-shaped indentation, toward the retreating ice sheet. Note kame in the south part of sec. 19. Sec. 19, T. 8, R. 7, W. 2.
Aerial view of washboard moraine forming a re-entrant
Part of W.O. Kupsch fonds
Aerial photograph of washboard moraine forming a re-entrant or V-shaped indentation, toward the retreating ice sheet. Note kame in the south part of sec. 19. Sec. 19, T. 8, R. 7, W. 2.
Aerial view of washboard moraine re-entrant
Part of W.O. Kupsch fonds
Aerial photograph of a washboard moraine (minor recessional ridges or swells and swales) re-entrant as indicated by the V-shaped indentation of the ridges. Sec. 24, T. 12, R. 10, W. 2.
Aero Relief map of the world in colour
Part of W.O. Kupsch fonds
Aero Relief map of the world in colour.
Agate, Brazil. Banded grey agate, crystalline quartz and amethyst
Part of W.O. Kupsch fonds
Agate, Brazil. Banded grey agate, crystalline quartz and amethyst.
Part of W.O. Kupsch fonds
Age of Atlantic islands, as indicated by the oldest rocks found on them apparently tends to ncrease with increasing distance from the Mid-Atlantic Ridge. The numbers associated with the islands give these ages in millions of years. Geologists divide Iceland into three areas of different ages, the central one being the youngest. Islands that have active volcanoes are represented by black triangles: most of these lie on or near the Mid-Atlanric Ridge (J.T. Wilson, 1963, Sci. Amer.)