Esker, showing till cover over distorted sand
- WOK 15-113
- Item
- 1962
Part of W.O. Kupsch fonds
Esker, showing till cover over distorted sand. Fred Schwertner. About 5 miles southwest of Rackham, Manitoba. October 6, 1962.
1974 results directly related Exclude narrower terms
Esker, showing till cover over distorted sand
Part of W.O. Kupsch fonds
Esker, showing till cover over distorted sand. Fred Schwertner. About 5 miles southwest of Rackham, Manitoba. October 6, 1962.
Esker, showing till cover over sand
Part of W.O. Kupsch fonds
Esker, showing till cover over sand. Rudy Klassen. About 5 miles southwest of Rackham, Manitoba. October 6, 1962.
Part of W.O. Kupsch fonds
Eskimo museum, Churchill, Manitoba. July 31, 1965.
Esso sign at Anticona Pass between La Oroya and Casapalca
Part of W.O. Kupsch fonds
Esso sign at Anticona Pass between La Oroya and Casapalca readinf 4820 metres (15,749 feet). Glacier in the background.
Part of W.O. Kupsch fonds
Etna, Sicily, air photo by Jim Stuart. Winter 1957
Evolution of the Canadian Rockies
Part of W.O. Kupsch fonds
Evolution of the Canadian Rockies. The upper diagram shows the Rocky Mountain trough filling with sediments during the late Mesozoic. The middle diagram shows the compressional deformationof the Rocky Mountain trough to form the the Canadian Rockies. The lower diagram shows erosion ofrming the present topgraphy. The numbers show the corresponding beds in successive stages. (Stokes, 1960, p. 164).
Part of W.O. Kupsch fonds
Evolution of the Coleoidea. Umbgrove 1943, p. 98.
Evolution of the ocean bottom - expanding earth hypothesis
Part of W.O. Kupsch fonds
Evolution of the ocean bottom according to the expanding earth hypothesis is represented by these diagrams. Top layer of material is sedimentary rock of continents. Below it is the type of material that makes up the crust of the oceans. Bottom layer (vertical hatching) is the earth's mantle. In top diagram, continents are close together; rift between is just opening up. Next, material from mantle comes through rift, creating mid-ocean ridge seen in third diagram. Bottom diagram represents Atlantic ocean bottom as it is today, with ridge and rift in center and continents at far right and left. Heezen, 1960.
Evolution of the paleozoic Nautiloidea
Part of W.O. Kupsch fonds
Evolution of the paleozoic Nautiloidea. A. Orthoceras, B. Cyrtoceras, C. Gyroceras, D. Ophidioceras, E. Nautilus. (Umbrove, 1943, p. 96).
Part of W.O. Kupsch fonds
Evolution of the vertabrates.
Excavated watertank in front of temple at Mohenjo Daro, Indus Valley
Part of W.O. Kupsch fonds
Photograph of a watertank in front of excavated temple at Mohenjo Daro. Oldest known use of bitumen as a damp cource, 3,000 BC. Photograph copied from a book.
Excavation at work near Gull Lake, Saskatchewan.
Part of W.O. Kupsch fonds
Excavation at work near Gull Lake, Saskatchewan.
Exfoliation of coarse grained basic igneous rock
Part of W.O. Kupsch fonds
Exfoliation of coarse grained basic igneous rock as a free-lying erratic and forming part of a laf concentrate along the South Saskatchewan River west of Saskatchewan Landing. Fall, 1962.