1974 results directly related Exclude narrower terms
Straight ice marginal channel - west of Wawota, Sask.
Part of W.O. Kupsch fonds
Straight ice marginal channel. Along highway 16, about 4 miles west of Wawota, Sask.
Stratification and cross stratification in delta deposits
Part of W.O. Kupsch fonds
Stratification and cross stratification in delta deposits exposed oin gravel pit near Rivers, Manitoba. Rudy Klassen. October 6, 1962.
Stratigraphic section in Pleistocene strata - Minnedosa River
Part of W.O. Kupsch fonds
Stratigraphic section in Pleistocene strata on the north side of Minnedosa River at highway 83 crossing. From top to bottom, the following units can be recognised: till 4, till 3, stratified sand and gravel about ten feet thick forming recessive slope, till 2 in sloping contact with till 1. October 6, 1962.
Stratigraphic table of southwestern Saskatchewan
Part of W.O. Kupsch fonds
Stratigraphic table of southwestern Saskatchewan (Upper Cretaceous and Tertiary only)
Stratigraphic table of southwestern Saskatchewan
Part of W.O. Kupsch fonds
Stratigraphic table of southwestern Saskatchewan (Upper Cretaceous and Tertiary only)
Stratigraphic table of southwestern Saskatchewan
Part of W.O. Kupsch fonds
Stratigraphic table of southwestern Saskatchewan (Upper Cretaceous and Tertiary only)
Strawberry Hills moraine, east of Saskatoon
Part of W.O. Kupsch fonds
Strawberry Hills moraine, east on Highway 5, Saskatoon, Sask.
Stream valleys antedating at least one glaciation in Western Canada
Part of W.O. Kupsch fonds
Stream valleys antedating at least one glaciation in Western Canada and adjacent parts of the United States (Kupsch 1964, fig. 9).
Striated dolomite boulder in place in till at top
Part of W.O. Kupsch fonds
Striated dolomite boulder in place in till at top, where overlain by younger till. Swift Current Creek, near Powerhouse, Swift Current.
Strike ridges and valleys as developed in arid and humid climates
Part of W.O. Kupsch fonds
Strike ridges and valleys as developed in an arid climate (top) and in a humid climate (bottom) on identical open-fold rock structure.
Stromatoporoidal reef - Whiteman's Gap near Cochrane, Alberta
Part of W.O. Kupsch fonds
Stromatoporoidal reef oin Devonian Fairholme limestone at Whiteman's Gap near Cochrane, Alberta.
Stromatoporoidal reef - Whiteman's Gap near Cochrane, Alberta
Part of W.O. Kupsch fonds
Closer view of stromatoporoidal reef oin Devonian Fairholme limestone at Whiteman's Gap near Cochrane, Alberta.
Structural conditions favourable to the accumulation of oil and gas
Part of W.O. Kupsch fonds
Diagrams to illustrate the structural conditions favourable to the accumulation of oil and gas. A, most common occurrence, crest of an antcline, Ranger Field, Texas as an example. B, fault trap; Van Field, Texas. C, reef, porous coral-reef limestone, Scurry County, Texas and some from Alberta fields. D. Stratigraphic trap, difficult to discover, East Texas field (Von Engelin and Caster, 1952, p. 208).
Structural elements of the world
Part of W.O. Kupsch fonds
Structural elements of the world. Colour scheme Pink (Shields), Grey (Carboniferous folding), Black (coal), Brown (younger folding), Yellow (Plateaus), Green (Cenozoic deposits), Orange (Volcanic masses, mainly plateau basalts). Deep sea trenches and /or island arcs indicated by blue lines.
Structural map of North America
Part of W.O. Kupsch fonds
Structural map of North America. King 1959, map at end of book.