1974 results directly related Exclude narrower terms
Silt channel in ice-contact gravels
Part of W.O. Kupsch fonds
Silt channel in ice-contact gravels. Gravel pit along highway 11 south of Floral, Saskatchewan. October 7, 1962.
Silt layers in terrace gravels near Eastend, Sask
Part of W.O. Kupsch fonds
Silt layers in terrace gravels near Eastend, Sask (lowest terrace east of town). Notice persistency of layers, sorting, common orientation.
Silt over gravel terrace deposits of Bow River
Part of W.O. Kupsch fonds
Silt over gravel terrace deposits of Bow River at 42nd Ave. McLeod Trail Calgary.
Silty alluvial deposits on east bank of South Saskatchewan River near Beaver Creek
Part of W.O. Kupsch fonds
Silty alluvial deposits on east bank of South Saskatchewan River near Beaver Creek. The alluvium here contains gastropods and other subfossil material as well as some charcoal to which Earl Christiansen is pointing.
Single elliptical drainage deflection of Bear Creek
Part of W.O. Kupsch fonds
Single elliptical drainage deflection of Bear Creek. Vegetational lineament in valley centre. Sec. 8, T. 11, R. 23, W. 3.
Part of W.O. Kupsch fonds
Illustrated portrait of Sir John Richardson. Copied from a book. Pioneer Geologists in Saskatchewan.
Skeidararsandur with vaguely discernible moraines
Part of W.O. Kupsch fonds
Skeidararsandur with vaguely discernible moraines dating from the 15th century to 1930. August 10, 1960.
Skeidararsandur with vaguely discernible moraines
Part of W.O. Kupsch fonds
Skeidararsandur with vaguely discernible moraines dating from the 15th century to 1930. View toward the glacier. August 10, 1960.
Sketch map to show conditions of drainage in karst
Part of W.O. Kupsch fonds
Karst. Sketch map to show conditions of drainage in different stages of karst. Kendall et al., 1951, p. 248.
Sketches of the ocean control theory of glaciation
Part of W.O. Kupsch fonds
Sketches of the ocean control theory of glaciation, as proposed by William Lee Stokes. Stirton, 1959, p. 337.
Part of W.O. Kupsch fonds
Skulls of fossil human types.
Slaty cleavage at angle to bedding
Part of W.O. Kupsch fonds
Slaty cleavage at angle to bedding. ALong Rhine highway near Bingen, Germany.
Slickensided fault plane in basalt
Part of W.O. Kupsch fonds
Slickensided fault plane in basalt. N.Y. State Thruway about eight miles west of Nannet.
Slide in Quebec on the Rimouski River
Part of W.O. Kupsch fonds
Slide in Quebec on the Rimouski River was caused partly by the 14 degree slope (cross section at the top) much steeper than slopes usually associated with quick clay. A layer of soft, silty clay heavily charged with water formed a slip surface. The debris filled river for several thousand feet and created a temporary lake. Hummocky surface is typical of clay slide (Kerr, P.F., 1963, Sci. Amer. Nov., p. 138).
Slip off slope on terrace of Moose Mountain Creek
Part of W.O. Kupsch fonds
Slip off slope on terrace of Moose Mountain Creek cut by post glacial tributary.