View south from station 62-K-77 to show outcrops of white sandstone, some carbonaceous shale in left foreground and some brown ironstone concretionary layer in immediate foreground, all belonging to the Heiberg formation. August 2, 1962.
View up Jura Creek near Exshaw, Alberta to show along skyline from left to right Rundle (grey), Banff (brownish grey, also on left side of of creek in middle foreground), Exshaw (along which the creek has eroded the subsequent valley shown in the picture), Palliser (grey, on right hand side of the creek). May, 1961.
Wandering dune landscape. 1. Moraine landscape. 2. Former lake bottom. 3. Dune landscape. a. Erosion slope. b. ditto. c. Dune hill. d. Parabola-dune. e. Filso. 4. Deflation-plain. 5. Littoral dunes. 6. Beach. A. Moraine. B. Marine deposits. C. Lake deposits. D. Blown sand. Source: Atlas of Denmark.
Wandering the north magnetic pole through geologic time. although students of ancient rock magnetism regard this path as fairly well established, there is no conclusive proof that the geographic pole followed the same path or that the continents maintained their same positions during this lengthy period. Notice also that there are no signs of frigid conditions or glacial action in northeastern Asia during the periods when the pole was supposed to be in that vicinity. Stokes, 1960, p. 168.