Upper Silurian sedimentary rock facies, Arctic islands
- WOK 18-48
- Item
- [1963]
Part of W.O. Kupsch fonds
Upper Silurian sedimentary rock facies, Arctic Islands. Clark and Stearn, 1960, p. 244.
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Upper Silurian sedimentary rock facies, Arctic islands
Part of W.O. Kupsch fonds
Upper Silurian sedimentary rock facies, Arctic Islands. Clark and Stearn, 1960, p. 244.
Upper part of Whitemud with two coal seams, overlain by till
Part of W.O. Kupsch fonds
Upper part of Whitemud with two coal seams, overlain by till. Cactus or Blue Hills, Saskatchewan.
Upper member of Whitemud Formation at base
Part of W.O. Kupsch fonds
Upper member of Whitemud Formation (Upper Cretaceous) at base, overlain unconformably by greenish grey sands and clays of Frenchmen Formation (Upper Cretaceous) and coaly sands of Paleocene Ravenscrag Formation. The coal seam at the base of the Ravenscrag is the Ferris Seam. Type section of Ravenscrag Formation at Ravenscrag Butte quarry, Ravenscrag, Saskatchewan. May, 1964.
Part of W.O. Kupsch fonds
Upper Devonian tectonic map (Raasch et al., 1961, v. 1, p. 447).
Upper Cretaceous to early Tertiary tectonic map
Part of W.O. Kupsch fonds
Upper Cretaceous to early Tertiary tectonic map (Raasch et al., 1961, v. 1, p. 452).
Unglaciated plains area near Bellefourche, S.D.
Part of W.O. Kupsch fonds
Unglaciated plains area near Bellefourche, S.D.
Unglaciated part of Wood Mountains where no erratics found
Part of W.O. Kupsch fonds
Unglaciated part of Wood Mountains where no erratics have been found. Looking west along Highway 2, south of Rock Glen. Sunday, October 2, 1960.
Uncovering a mammoth tusk in preparation of a plaster block
Part of W.O. Kupsch fonds
Uncovering a mammoth tusk in preparation of a plaster block in the field: (a) discovery, (b) outlining the block, (c) application of shellack, (d) first plaster strips over wet newspaper, (e) reinforcing block, (f) plaster strips covering side of block. (Stirton, 1959, p. 35).
Uncontrolled disintegration pattern with well-developed "doughtnut"
Part of W.O. Kupsch fonds
Uncontrolled disintegration pattern with well-developed "doughtnut". East of Saskatoon, flight to Winnipeg.
Uncontrolled disintegration moraine - NW of Saskatoon
Part of W.O. Kupsch fonds
Uncontrolled disintegration moraine (rimmed kettles) from air. Northwest of Saskatoon on flight to Edmonton.
Uncontrolled disintegration moraine
Part of W.O. Kupsch fonds
Uncontrolled disintegration moraine with "doughnuts" emphasized by aspen ring "bluffs". East of Saskatoon, flight to Winnipeg.
Unconformity between marine gravels
Part of W.O. Kupsch fonds
Unconformity between marine gravels wit Mytilus (a pelecypod) over ice contact stratified drift. Boseville pit near Ottawa.
Unconformable contact between Whitemud Formation and Frenchman Formation
Part of W.O. Kupsch fonds
Unconformable contact between lower, sandy member of Whitemud Formation below and Frenchman sands above. Note clay pebbles forming a basal conglomerate in the Fenchmen sands. No quartzite pebbles were found in place as mentioned by Kupsch, 1956, p. 20-21. May, 1964.
Unconformable contact between Whitemud Formation and Frenchman Formation
Part of W.O. Kupsch fonds
Unconformable contact between upper white member of Whitemud Formation below and purplish clays of Frenchman Formation (Battle facies) above. Ravenscrag Butte, Saskatchewan. May 1964.
Unconformable contact - Lake Minnewanka near Banff, Alberta
Part of W.O. Kupsch fonds
Unconformable contact between permo-pennsylvanian Rocky Mountain quartzite at left and Triassic Spray River formation, dark phosphatic shale at right. Lake Minnewanka near Banff, Alberta