Southwestward dipping Ravenscrag sandstone
- WOK 4-3
- Stuk
- 1956
Part of W.O. Kupsch fonds
Southwestward dipping Ravenscrag sandstone along Souris River Valley fault. (Keith Knox)
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Southwestward dipping Ravenscrag sandstone
Part of W.O. Kupsch fonds
Southwestward dipping Ravenscrag sandstone along Souris River Valley fault. (Keith Knox)
Shore line of terraces along Old Wives Lake
Part of W.O. Kupsch fonds
Shore line of terraces along Old Wives Lake.
Thrust end moraines northeast of Clearwater, Sask.
Part of W.O. Kupsch fonds
Thrust end moraines northeast of Clearwater, Sask.
Glacial lake plain around Beechy
Part of W.O. Kupsch fonds
Glacial lake plain around Beechy viewed from preglacial highland covered by moraine. Also preglacial highland covered by moraine in distance.
Fault in Bearpaw; unconformably overlain by till
Part of W.O. Kupsch fonds
Fault in Bearpaw (shale to right against sand to left); unconformably overlain by till. Lacustrine silts on till. Tributary to Snakebite Creek.
Crevasse fillings, crossing - near Wymark, Sask.
Part of W.O. Kupsch fonds
Crevasse fillings, crossing. Near Wymark, Sask.
Tertiary gravels. Cypress Hills formation. West of Wymark, Sask.
Part of W.O. Kupsch fonds
Tertiary gravels. Cypress Hills formation. West of Wymark, Sask.
Elbow upland over Elbow structure
Part of W.O. Kupsch fonds
Elbow upland over Elbow structure.
Dipping gravels, near Eastend, Sask.
Part of W.O. Kupsch fonds
Dipping gravels. Frontal part of Wright's gravel pit, near Eastend, Sask.
Ice wedge in till filled with sand
Part of W.O. Kupsch fonds
Ice wedge in till filled with sand. Trans Canada gas pipeline trench. Sec. 24, T. 18, R. 10, W. 3.
Part of W.O. Kupsch fonds
Formation of esker in ice-age. Sand and gravel sedimentation in meltwater tunnel of crevasse in moraine-choked glacier ice or dead-ice. The shape of the esker formed after the melting of the ice by soil slipping from the ice-contact walls. Source: Atlas of Denmark.
Present stage of outwash plains
Part of W.O. Kupsch fonds
Present stage of outwash plains. 2. Outwash plain. 3. Moraine landscape. a. Highest point of outwash plain. b. The ice-contact slope of the high outwash plain against the moraine landscape. c. Bog, overgrown lake. d. Lake. e. Marginal moraine. f. Boggy area. A. Moraine. C. Meltwater deposits. Source: Atlas of Denmark.
Tunnel-meltwater glacial complex.
Part of W.O. Kupsch fonds
Tunnel-meltwater glacial complex. 1. Moraine plateau. 2. Tunnel valley. a. Mosso basin. b. Saltena valley. 3. Fluvio-glacial valley. 4. Valley terraces, resistant parts of earlier valley bottoms, consisting of metlwater deposits. 5. Dead-ice depressions. c. Salten Langso. d. Bog depression. e. Kettle-holes. 6. Post-glacial erosion valleys, dissecting the moraine plateau. 7. Recent valley bottom. f. Gudena. g. Delta of the River Gudena in the Mosso basin. Source: Atlas of Denmark.
Cliff in dislocated glacial deposits.
Part of W.O. Kupsch fonds
Cliff in dislocated glacial deposits. Surface-forming stages in late- and post-glacial period. III. Ground moraine, deposited discordantly over dislocated meltwater deposits. IV. Deflation-plain, the result of removal of fine-grained moraine components by the alnd surface and inducing the formation of a humification horizon over stones. VI. Blown sand covering other deposits. D2. Stones. E. Humus horizon. F. Blown sand. In this substratum the present cliff was formed by the action of the sea and atmospheric forces. Source: Atlas of Denmark.
Cliff in dislocated glacial deposits.
Part of W.O. Kupsch fonds
Cliff in dislocated glacial deposits. Present stage. 1. Precipice in continuous clay secions. 2. Screes. 3. Gullies between clay walls formed by the slipping sand beds, erosion of running water and wind action. 4. Beach, low tide. 5. Slide plane in screes caused by wave action. 6. Rain gulley. 7. Cone deposited sand. 8. Accumulation of blawn sand above gully. 9. Dune landscape. 10. Ridge formation through intersection of clay with surface. B-G, see slides 60-62. Source: Atlas of Denmark.