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Slumping in Eastend-Whitemud strata
Part of W.O. Kupsch fonds
Slumping in Eastend-Whitemud strata overlying Bearpaw Shales in Frenchman River Valley near Ravenscrag.
Slumping along Highway 20, about one mile east of Lumsden
Part of W.O. Kupsch fonds
Slumping along Highway 20, about one mile east of Lumsden. Sliding occurs along till-Bearpaw contact. Friday, November 4, 1960.
Slumping along drainage channel. Swift Current Creek, Sask.
Part of W.O. Kupsch fonds
Slumping along drainage channel. Swift Current Creek, Sask.
Slump structures in ice contact stratified drift - near Kisbey, Sask
Part of W.O. Kupsch fonds
Slump structures in ice contact stratified drift north of Kisbey, Sask.
Slump faults in Pleistocene outwash gravel
Part of W.O. Kupsch fonds
Slump faults in Pleistocene outwash gravel. Soil above is undisturbed; faults older than soil formation. Gravel pit near Wilkie, Sask.
Slump block, east bank of Souris, south of Oxbow, Sask
Part of W.O. Kupsch fonds
Slump block, east bank of Souris, south of Oxbow, Sask.
Slump along open water supply ditch
Part of W.O. Kupsch fonds
Slump along open water supply ditch from South Saskatchewan River to Qu'Appelle Valley and Buffalo Pound, near Elbow. Note contact between grey Bearpaw below till above; lateral spreading of toe.
Sloping dissected terrace remnants on bedrock
Part of W.O. Kupsch fonds
Sloping dissected terrace remnants on bedrock along Red Deer River near Drumheller, AB. November 10, 1962.
Slip-off slope and undercut bank of the Assiniboine River
Part of W.O. Kupsch fonds
Slip-off slope and undercut bank of the Assiniboine River near Treat, Manitoba. October 5, 1962.
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.
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).
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.
Slaty cleavage at angle to bedding
Part of W.O. Kupsch fonds
Slaty cleavage at angle to bedding. ALong Rhine highway near Bingen, Germany.
Part of W.O. Kupsch fonds
Skulls of fossil human types.
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.