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. 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. 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.

Ripple mark cross-bedding in Lenzie silt near Lethbridge, AB. See Horberg, 1952, section 10.

Distorted Saskatchewan gravels under basal till which is overlain by lower till. See Horberg, 1952, section II, near Lethbridge.

Oxidized (yellow orange) and oxidized (blue-grey) till. Near Lethbridge. See Horberg, 1952, section 11. Lower till.

Distorted Saskatchewan gravels overlying Cretaceous shales, upper part of which is oxidized. See Horberg, 1952, section 15.

Gully, 100 ft deep, cut recently by drainage ditch. Lethbridge area.

Vertical and overturned sand and gravels. Gravel pit on west side of highway 9 where it crosses Pipestone Creek, Saskatchewan.

Small horseshoe shaped depression made by spring. Near Dittman farm, Alsask, Saskatchewan.

Spring area issuing from drift. C.N.R. spring near Dittman farm, Alsask, Saskatchewan.

Horse shoe shaped end moraine with outwash area to left, morainal area to the right. West of Glen Kerr, Saskatchewan.

Toographic and bedrock high over Elbow subsurface structure.

Herbert peat project, view of dig.

Abandoned strand line of Lake Bonneville, south of Salt Lake City, Utah.