1974 results directly related Exclude narrower terms
Exposure to Dwyka conglomerate with erratic
Part of W.O. Kupsch fonds
Exposure to Dwyka conglomerate with erratic. Durban, Natal, Cape Province of South Africa.
Exposure of till - Dempster's clay pit, Eastend, Sask
Part of W.O. Kupsch fonds
Exposure of till. Vertical markings made by bulldozer. Dempster's clay pit, Eastend, Sask. (Stu Jordan in picture)
Exposure of Precambrian tillite
Part of W.O. Kupsch fonds
Exposure of Precambrian tillite. Stust Valley, S. Australia.
Exposure of marl along shore of Sturgeon Lake, Sask.
Part of W.O. Kupsch fonds
Exposure of marl along shore of Sturgeon Lake, Sask. Notice stratification. About 1/4 mile east of narrows in bay south side of Sturgeon Lake, Sask.
"Exposed tidal flats from Apex Community"
Part of W.O. Kupsch fonds
"Exposed tidal flats from Apex Community, Frobisher Bay, N.W.T. August 8, 1965."
"Exposed tidal flats from Apex Community"
Part of W.O. Kupsch fonds
Citation reads: "Exposed tidal flats from Apex Community, Frobisher Bay, N.W.T. August 8, 1965."
Exposed known nuclei of the world
Part of W.O. Kupsch fonds
Exposed known nuclei of the world. Jacobs et al., 1959, fig. 15-8.
Part of W.O. Kupsch fonds
Citation reads: "Exposed iron ore, Mary River, N.W.T. August 15, 1965."
Experimental formation of drumlin
Part of W.O. Kupsch fonds
Experimental formation of drumlin.
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.
Excavation at work near Gull Lake, Saskatchewan.
Part of W.O. Kupsch fonds
Excavation at work near Gull Lake, Saskatchewan.
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.
Part of W.O. Kupsch fonds
Evolution of the vertabrates.
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).
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.