Soil polygons. U. of Saskatchewan campus, reflecting pool
- WOK 8-115
- Item
- 1959
Parte de W.O. Kupsch fonds
Soil polygons. University of Saskatchewan campus, reflecting pool.
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Soil polygons. U. of Saskatchewan campus, reflecting pool
Parte de W.O. Kupsch fonds
Soil polygons. University of Saskatchewan campus, reflecting pool.
Pressure ridge in river ice along the South Saskatchewan
Parte de W.O. Kupsch fonds
Pressure ridge in river ice at the convex side of the bend of the South Saskatchewan at Elbow.
Slump along open water supply ditch
Parte de 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.
Aspen "bluff" in winter - east of Saskatoon
Parte de W.O. Kupsch fonds
Aspen "bluff" in winter. Along highway 5, east of Saskatoon. Note convex profile of grove with younger trees in outer part.
Aspen "bluff" in winter - east of Saskatoon
Parte de W.O. Kupsch fonds
Aspen "bluff" in winter. Along highway 5, east of Saskatoon.
Close up of white spruce (Picea Glauca), Forestry Farm, Sutherland
Parte de W.O. Kupsch fonds
Close up of white spruce (Picea Glauca), Forestry Farm, Sutherland.
Cretaceous red Moho shales with grey blocks of Ayavacas limestone
Parte de W.O. Kupsch fonds
Cretaceous red Moho shales with grey blocks of Ayavacas limestone. Looking east from road south of Lake Saracocha.
Picea Glauca, white spruce, Forestry Farm, Sutherland
Parte de W.O. Kupsch fonds
Picea Glauca, white spruce, Forestry Farm, Sutherland.
Saxicava marine sand - Foster's sandpit, Ottawa
Parte de W.O. Kupsch fonds
Saxicava marine sand. Saxicava (a pelecypod) is now known as Hiatella. Thr Saxicava sand is younger than the Leda clay. Whale bones were found in the sand in this locality. Foster's sandpit at airport, Ottawa.
Close-up of unconformity between cross bedded ice contact stratified drift
Parte de W.O. Kupsch fonds
Close-up of unconformity between steeply dipping cross bedded ice contact stratified drift below Mytilus marine gravels above. Boseville pit near Ottawa.
Close-up of marine gravels, showing Mytilus
Parte de W.O. Kupsch fonds
Close-up of marine gravels, showing Mytilus (a pelecypod); Boseville pit near Ottawa.
Unconformity between marine gravels
Parte de W.O. Kupsch fonds
Unconformity between marine gravels wit Mytilus (a pelecypod) over ice contact stratified drift. Boseville pit near Ottawa.
Gravel pit near Gloucester Hunt Club and Metcalfe Road
Parte de W.O. Kupsch fonds
For glacial geology of Ottawa area, see C.S.C. Mem. 101. Marine clays (Leda clay) with reworked boulders over ice contact stratified drift. Leda (a pelecypod) is now known as Yoldia. Nelson Gadd in picture, shovel at contact. Gravel pit near Gloucester Hunt Club and Metcalfe Road, Ottawa, Ontario.
Erratic. Logan boulder in front of National Museum Buliding, Ottawa
Parte de W.O. Kupsch fonds
Erratic. Logan boulder in front of National Museum Buliding, Ottawa. Boulder is of Ottawa gneiss from formation Logan named and which he made classic by his studies. On it is a bronze plaque bearing his likeness and an inscription that reads: SIR WILLIAM LOGAN K.B., L.L.D., FRS/ 1798 - 1873/ The Father of Canadian Geology/ Founder and First Director of the/ Geological Survey of Canada/ 1842 - 1869/ Erected by the Twelfth/ International Geological Congress/ Canada/ MCMXIII.
Uncontrolled disintegration pattern with well-developed "doughtnut"
Parte de W.O. Kupsch fonds
Uncontrolled disintegration pattern with well-developed "doughtnut". East of Saskatoon, flight to Winnipeg.