1974 results directly related Exclude narrower terms
EllesmereGr. View of anticline in which Pennsylvanian Canyon Fiord beds dip westward
Part of W.O. Kupsch fonds
Ellesmere Gr. Looking north from station 63 K 79 to show western limb of anticline in which reddish and yellowish Pennsylvanian Canyon Fiord beds dip westward at 20 degrees. They are overlain by greenish-grey Assistance beds of Permian age. In far distance, Canyon Fiord can be seen frozen over.
Part of L.G. Saunders fonds
Two docks are seen empty on a northern Saskatchewan lake.
Saunders, Leslie Gale
End moraine south of Horton Lake
Part of W.O. Kupsch fonds
End moraine south of Horton Lake as seen from the air (station WK70). Looking north. The ice moved from east to west. Note steeper proximal (east) side of end moraine and gentler distal (west) side grading into outwashplain. Thursday, August 6, 1959.
End moraines, structural. Dirt Hills area, Sask.
Part of W.O. Kupsch fonds
End moraines, structural. Dirt Hills area, Sask.
Endmoraine in buried channel. Northeast of Leinan, Sask.
Part of W.O. Kupsch fonds
Endmoraine in buried channel. Northeast of Leinan, Sask.
Endmoraine in buried channel. Northeast of Leinan, Sask.
Part of W.O. Kupsch fonds
Endmoraine in buried channel. Northeast of Leinan, Sask.
Endmoraine in buried channel. Northeast of Leinan, Sask.
Part of W.O. Kupsch fonds
Endmoraine in buried channel. Northeast of Leinan, Sask.
Enlarged portion of geological map of the Grand Canyon
Part of W.O. Kupsch fonds
Enlarged portion of geological map of the Grand Canyon, Arizona, showing the fault controlled Bright Angel Canyon.
Entrance to Mission Canyon, Little Rocky Mountains
Part of W.O. Kupsch fonds
Entrance to Mission Canyon, Little Rocky Mountains.
Equipment for laying of Trans-Canada pipeline
Part of W.O. Kupsch fonds
Equipment for laying Trans-Canada 34-inch gas pipeline at Leinan Saskatchewan
Equus, early Pleistocene to Recent
Part of W.O. Kupsch fonds
Equus, early Pleistocene to Recent: (a) front foot; (b) crown surface and side views of upper premolar; (c) restoration. Stirton, 1959, p. 480.
Part of W.O. Kupsch fonds
Eroded anticline. Breached anticline, limestone, in semi-arid climate at 6000 feet above sea level. Near Asmara, Eritrea. Monkhouse, 1959, p. 5.
Eroded moraine with lag concentrate
Part of W.O. Kupsch fonds
Eroded moraine with lag concentrate. Upper terrace of South Saskatchewan River north of Sutherland.
Erosion and the wearing down of land surface
Part of W.O. Kupsch fonds
Erosion surface. Wearing down of land surface from youth (a) through maturity (b) to old age (c) to give it a peneplain. Holmes, 1953, p. 187.
Part of W.O. Kupsch fonds
Erosion surface, slightly tilted to the East and which truncates the gneiss and granite of the Hercynian floor of the Cevannes. It is in fact a post-Hercynian erosion surface bearing superficial Triassic deposits. It is noticeably rejuvenated by the valley of the Chassezac and its tributaries. The floor has reacted to this rejuvenation as a homogenous mass, except for some harder seam that may be seen in the foreground. France Institut Geographique National. Relief form atlas, 1956, p. 101.